OS2.3 | Advances in understanding the multi-scale and multi-disciplinary dynamics of the Southern European Seas (Mediterranean and Black Sea)
Advances in understanding the multi-scale and multi-disciplinary dynamics of the Southern European Seas (Mediterranean and Black Sea)
Convener: Vanessa Cardin | Co-conveners: Arthur Capet, Alejandro Orfila, Katrin Schroeder
Orals
| Fri, 28 Apr, 08:30–12:30 (CEST)
 
Room E2
Posters on site
| Attendance Fri, 28 Apr, 14:00–15:45 (CEST)
 
Hall X5
Posters virtual
| Attendance Fri, 28 Apr, 14:00–15:45 (CEST)
 
vHall CR/OS
Orals |
Fri, 08:30
Fri, 14:00
Fri, 14:00
Among other stressors, the Mediterranean and Black Seas have recently shown clear signs of climate change, including an increase in sea surface temperature in both basins, salinization of the intermediate and deep waters, a rise in sea level over the last century, and deoxygenation trends. These trends stress the vulnerability of these semi-enclosed and densely populated basins.

The urgent social and economic drivers require targeted improvements in weather, climate, water, oceans, and relevant environmental information and services. The risks associated with climate variability and extreme environmental events can lead to social and economic stresses that require new meteorological, hydrological, oceanographic, and climate services to ensure the safety and security of populations and the development of adaptive economic strategies.

This session is devoted to multidisciplinary scientific advances highlighting environmental trends at different spatial and temporal scales in the Mediterranean and Black Seas. We call for studies that address those threats in the Mediterranean and Black Seas including new approaches in physical and biogeochemical monitoring, ocean modeling, operational oceanography, and downstream product development.

Orals: Fri, 28 Apr | Room E2

Chairpersons: Katrin Schroeder, Arthur Capet
08:30–08:35
08:35–08:40
08:40–08:50
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EGU23-5381
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ECS
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On-site presentation
A exhaustive dataset of Sentinel-1 observations and derived information on the Mediterranean Sea
(withdrawn)
Aurélien Colin, Ronan Fablet, Romain Husson, Charles Peureux, and Pierre Tandeo
08:50–09:00
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EGU23-14117
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ECS
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On-site presentation
Bethany McDonagh, Emanuela Clementi, and Nadia Pinardi

Tidal forcing was not included in a large proportion of numerical models of the ocean from the past but is known to be necessary to forecast the ocean accurately, since tides dissipate around 3.5TW of energy in the global ocean, and are an important driver of mixing. The inclusion of tides in models affects not only the near-field dynamics such as local temperature and salinity, but also large-scale circulations that influence the entire global ocean. In the Mediterranean Sea, amplitudes of tides are typically low, but are known to have effects both at local scales where tidal amplitude is larger, and across the entire basin. However, their impact on processes such as circulation, vertical mixing, and internal tides at the basin scale are not well known. 

In this work, the characteristics of tides in the Mediterranean Sea were investigated using the hydrodynamic model NEMO (Nucleus for European Modelling of the Ocean) version 3.6, corresponding to the Copernicus Monitoring Environment Marine Service (CMEMS) system, a baroclinic forecasting model for the Mediterranean Sea, integrated over five years. 

Analysis of potential and kinetic energy due to tides showed that tides have impacts across a wide variety of spatial and temporal scales in the basin, both at the surface and at deeper levels. Increased kinetic energy at depth in the basin led to an exploration of internal tides, which have not been previously studied at the scale of the Mediterranean Sea using a numerical approach. Additionally, the effects of tides on salt transport through the Gibraltar Strait were analysed, and numerical results were compared to a two-layer box model of the Gibraltar Strait and Mediterranean Sea. This demonstrated the utility of simple theoretical frameworks to understand dynamics in the region, while highlighting the impact of increased vertical mixing in the Gibraltar Strait due to internal tides.

Our improved understanding of the impacts of tides across temporal and spatial scales lays out an argument for the inclusion of tides in ocean models ranging from local to global, and from short timescales to long term climate modelling. Our analysis also provides a novel understanding of dynamics such as internal tides and transport of salinity in the Mediterranean region.

How to cite: McDonagh, B., Clementi, E., and Pinardi, N.: The characteristics and effects of tides on the general circulation of the Mediterranean Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-14117, https://doi.org/10.5194/egusphere-egu23-14117, 2023.

09:00–09:10
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EGU23-4429
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Highlight
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On-site presentation
Salvatore Marullo, Vincenzo De Toma, Alcide di Sarra, Roberto Iacono, Angela Landolfi, Francesca Leonelli, Ernesto Napolitano, Daniela Meloni, Emanuele Organelli, Andrea Pisano, Rosalia Santoleri, and Damiano Sferlazzo

Marine Heat Waves (MHWs) are events of prolonged anomalously warm water, in portions of the oceans, which may have severe impacts on the local marine ecosystems.  In a climate change scenario, with increasing temperatures and more frequent atmospheric extreme events, the frequency and intensity of the MHWs are expected to increase. However, in a warming ocean, the choice of the long-term baseline used to compute SST anomalies becomes a critical issue, since it can significantly affect the frequency and intensity of the events. It may be argued that this climate change signal should be removed, in some way, to allow for a correct detection of MHWs.

Here, we critically address the problem of how to characterize and define MHWs in the present warming climate scenario by evaluating the impact of different SST climatic baselines, and the effects of removing climate trends from the original SST time series. We focus on the Mediterranean Sea, a hot spot region for climate change, where a strong mean SST increasing trend (about 0.045 °C/year) has been observed in the last 40 years.  Specifically, we use the Mediterranean SSTs, a satellite-based daily gap-free (level-4) SST provided in near real time at 1 km grid resolution and distributed through the Copernicus Marine Service (https://doi.org/10.48670/moi-00172 ).

We then examine the strong Mediterranean MHW of 2022, which started in May and is not yet extinguished at the time of this writing (December 2022). The MHW extended its presence through the summer and autumn seasons, with a sequence of intense events that interested between 30% to 60% of the Mediterranean area. The intensity of the 2022 MHW was comparable to that of the famous 2003 event, but the durations of the two MHWs have been quite different: in 2003 the areal threshold of 30% was exceeded from May to August (4 months) while in 2022 that threshold was exceeded from May to December and continues in January 2023. The evolution of the 2022 MHW is also discussed in relation to the corresponding atmospheric events occurred over the western portion of Europe and of the Mediterranean Sea and complemented with in situ data acquired at the ENEA station for climate observation of Lampedusa.

This work is funded in the framework of project “Detection and threats of marine heat waves -CAREHeat” of the European Space Agency - ESA – OCEAN HEALTH  program.

How to cite: Marullo, S., De Toma, V., di Sarra, A., Iacono, R., Landolfi, A., Leonelli, F., Napolitano, E., Meloni, D., Organelli, E., Pisano, A., Santoleri, R., and Sferlazzo, D.: Has the frequency of Mediterranean Marine Heatwaves really increased in the last decades?, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-4429, https://doi.org/10.5194/egusphere-egu23-4429, 2023.

09:10–09:20
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EGU23-5884
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On-site presentation
Simon Josey and Katrin Schroeder

Over the past 70 years, a major change in winter air-sea heat loss between the North-west Mediterranean (NWMed) and the Aegean Sea,  is revealed using the ERA5 amd 20CRv3 atmospheric reanalyses. The NWMed heat loss weakens from -154 Wm-2 in 1951-1985 to -137 Wm-2 in 1986-2020 as a results of weaker latent heat loss. This long-term weakening threatens continued dense water formation, and we show by evaluation of historical observations that winter-time ocean convection in the NWMed has declined by 40% from 1969 to 2018. Extension of the heat flux analysis reveals changes at other key dense water formation sites that favour an eastward shift in the locus of Mediterranean convection towards the Aegean Sea (where heat loss has remained unchanged at -172 Wm-2). The contrasting behaviour is due to differing time evolution of sea-air humidity and temperature gradients. These gradients have weakened in the NWMed due to more rapid warming of the air than the sea surface but remain near-constant in the Aegean. The different time evolution reflects the combined effects of global heating and atmospheric circulation changes which tend to offset heating in the Aegean but not the NWMed. The shift in heat loss has potentially significant consequences for dense water formation at these two sites and outflow to the Atlantic. The process of differential heat loss change in the Mediterranean Sea has implications for temporal variations in the balance of convection elsewhere e.g., the  high latitude Atlantic/Arctic margin dense water formation sites (Labrador-Irminger-Nordic Seas).

How to cite: Josey, S. and Schroeder, K.: Reduction in Winter Surface Heat Loss over the Past 70 Years Threatens North-West Mediterranean Convection, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5884, https://doi.org/10.5194/egusphere-egu23-5884, 2023.

09:20–09:30
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EGU23-6923
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ECS
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Highlight
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On-site presentation
Dimitra Denaxa, Emmanouil Flaounas, Maria Hatzaki, and Gerasimos Korres

The Mediterranean Sea (MS) has been experiencing significant surface warming over the past decades, greater than the global ocean and particularly higher during summers. The present study proposes the concept of Extreme Marine Summers (EMS) and investigates their characteristics in the MS in a climatological framework, based on ECMWF ERA5 daily sea surface temperature (SST) data for the period 1950-2020. Main objectives are to explore the SST substructures within EMSs, the contribution of Marine Heatwaves (MHW) during EMSs and the driving role of air-sea heat fluxes in the EMS formation.

EMSs are defined as the summers (July-August-September) exhibiting a mean SST greater than the 95th percentile of the mean summer SST values within the study period. A marine summer may evolve as extreme under different SST substructures within the season, e.g., due to uniformly increased SST values throughout the summer or due to higher than usual SSTs of a specific part of the SST distribution during the season. Results suggest that EMSs identified in the greatest part of the basin are formed due to the warmest part of the ranked daily SST distribution being warmer than normal. SSTs within EMSs are organised under high dependency on the climatological SST variability: locations where the warmest (coldest) part of the ranked daily SST distribution is more variable climatologically, experience EMSs primarily due to the contribution of the warmest (coldest) part of the SST distribution.

MHWs in EMSs present greater intensity, duration and occurrence frequency with respect to mean MHW conditions, in the northern flanks of the Mediterranean basin and particularly in the Aegean and Adriatic Seas. Although the north-western part of the basin experiences the most intense EMSs and summer MHWs, the role of MHWs in the formation of EMSs appears more pronounced in the central and eastern MS. In the rest of the basin, and particularly in southern MS regions, MHWs in EMSs are less intense but longer lasting and more frequent than usual.

To quantify the driving role of the net surface heat flux (Qnet) in the EMS formation, a metric is proposed based on the surface heat budget equation. The proposed metric represents the mean contribution of Qnet during summer sub-periods within which SST is kept above climatology via a) faster warming or b) slower cooling compared to the corresponding climatological period. Results show that EMSs are largely driven by Qnet in the northern MS regions: a latitudinal gradient is generally observed in the basin with increasing contribution percentages while moving northerly. In areas where the observed SST anomalies are not entirely explained by surface heat fluxes, negative wind speed and mixed layer depth seasonal anomalies relative to climatology are commonly observed, suggesting that wind-induced mixed layer shoaling is a complementary EMS contributing mechanism. Moreover, results reveal a strong link between MHW properties and surface heat fluxes during EMSs, suggesting that Qnet modulates particularly the intensity of MHWs.

How to cite: Denaxa, D., Flaounas, E., Hatzaki, M., and Korres, G.: Extreme marine summers in the Mediterranean Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-6923, https://doi.org/10.5194/egusphere-egu23-6923, 2023.

09:30–09:40
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EGU23-16588
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On-site presentation
Giovanni Liguori, Pinardi Nadia, and Mahmud Hasan Ghani

Using a suite of initial-condition (IC) ensemble forecasting experiments for the Mediterranean Sea, we assess the relative contribution of initial conditions versus atmospheric forcing in 10-day forecasts. Each ensemble member is forced at the surface by ECMWF fields and forecasts the same 10-day period starting from a different initial condition, which is taken from an ocean analysis estimate of the preceding 10-day period. This IC-time-shifted ensemble scheme allows us to explore the forecast dependency from both the IC and the atmospheric forcing (i.e., ECMWF).  Generally, the surface forcing dominates the forecast trajectory at the surface, leading to an inter-member spread that decreases with time. There are also cases in which the initial spread at the surface increases with time, indicating the dominant role of the uncertainty in the IC. While much less common, there are specific times and regions in which the initial condition determines the forecast trajectory during multiple days, indicating that certain oceanic structures are intrinsically more predictable. The identification of these highly-predictable oceanic states might prove extremely valuable in predicting the uncertainty in the forecast.

How to cite: Liguori, G., Nadia, P., and Hasan Ghani, M.: The relative contribution of initial condition versus atmospheric forcing in 10-day forecasts of the Mediterranean Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-16588, https://doi.org/10.5194/egusphere-egu23-16588, 2023.

09:40–09:50
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EGU23-16776
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On-site presentation
Mahmud Hasan Ghani and Giovanni Ligouri

In a semi-enclosed sea basin, like in the Mediterranean, determining the heat flux components of the heat budget is crucial for better understanding of the water budget and the regional climate. Due to its relatively small sea basin and existence of many islands, it’s always a complex and uncertain to settle with an accurate net heat balance. The variation in the net heat budget is referred as a heat budget “closure” problem, which has referred by many authors for the Mediterranean Sea. The value of net heat flux under this closure hypothesis should be negative, but there is a considerable range of variation for net heat budget in published literatures. In that context, we have computed the heat fluxes for in the Mediterranean Sea using a higher resolution atmospheric model analysis dataset (ECMWF) along with heat fluxes using a lower resolution dataset (ERA5) to compare. The computation of heat fluxes using high resolution ECMWF analysis dataset is a newer one for the Mediterranean Sea. The resulted long-term climatology of heat flux components (between ECMWF & ERA5) has shown a close agreement except a variation is observed in the Long Wave (LW) flux which matches a similar finding from Marullo et al. (2020). In addition to the net heat budget, this study aims to provide a newer aspect with the analysis of probability distributions of air-sea fluxes and uncertainty in those distributions. We have investigated the probability distributions of heat fluxes on the base of computed air-sea fluxes time series. We have analysed the probability distributions of air-sea fluxes using atmospheric analysis and reanalysis datasets and fitted with three parameters Probability Density Function (PDF). Then, we have evaluated the applied theoretical PDF fits with observed heat fluxes that have indicated areas with uncertainty through our statistical modelling approach for the turbulent heat flux distributions. The statistical analysis of air-sea fluxes is not a usual one for the Mediterranean Sea but an important one to obtain the statistical inference of air-sea flux distributions in relation to the probable uncertainty arises in the ocean forecasts. 

How to cite: Ghani, M. H. and Ligouri, G.: Reassessment of heat budget in the Mediterranean Seaand uncertainty in the probability distributions of heat fluxes, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-16776, https://doi.org/10.5194/egusphere-egu23-16776, 2023.

09:50–10:00
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EGU23-2073
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ECS
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On-site presentation
Leidy Maricela Castro Rosero, Ivan Hernandez, Manuel Espino Infantes, and Jose Maria Alsina Torrent

Floating marine litter (FML) is a global problem because of the risk it poses to marine life and human health. In a semi-enclosed basin such as the Black Sea, the slow replenishment of water and the strong input from European rivers potentially favoured the increasing accumulation of FML. In this sense, it is absolutely necessary to generate strategies in the Black Sea to mitigate the impacts on the marine ecosystem and human populations. This is one focus of the DOORS European Union Project (Developing Optimal and Open Research Support for the Black Sea) within which this work is framed.

In recent years, scientific studies on marine litter in the Black Sea have increased at regional and coastal scales. Such works include counting, analysis of distribution, estimation of riverine input and the use of numerical models to identify circulation and accumulation patterns (Bouzaiene et al., 2021; González-Fernández et al., 2022). Using Lagrangian models has opened the door to the discussion of how such models should be configured and the importance of whether to include phenomena such as stokes drift. In addition, some areas have been suggested as high accumulation areas but these results diverge between authors and available data. 

LOCATE is a tool built with the Lagrangian solver OceanParcels and developed for the prediction of areas of high FML accumulation, which has been adapted and validated for the Black Sea. The experiments were performed using surface current velocity and Stokes drift data taken from the Copernicus Marine Service with items of FML represented by Lagrangian particles in the model. Two simulations were run with a homogeneous particle release over the whole basin, every month during one year. The first one with only the surface currents and the second one adding Stokes drift, in order to evaluate the contribution of including the Stokes drift taken from the wave data. A third simulation was carried out with both drivers and releasing particles daily during one year according to the estimated amount of waste transported at the mouths of the nine main contributing rivers, to identify the trends of particle movement from these discharge points.

The results indicate the south-western area as an area of high coastal accumulation in all three simulated cases. The mainly cyclonic circulation, the large input of FML from the Danube River and other northern rivers including a relevant fraction of the outflow from the Kerch Strait probably explained this. In addition, the percentage of particles beached on shore and the residence time in offshore waters were strongly influenced by including Stokes drift, moving from a percentage of 45.5% to 75.5% and from an average residence time of 99 to 63 days. These values are in agreement with recent literature supporting an overestimation of residence times by omitting Stokes drift. Finally, this is only the beginning of a forecasting tool for FML in the Black Sea that is expected to be further improved by using coupled hydrodynamic models, extending the resolution with nested areas and incorporating higher accuracy in coastal processes including beaching.

How to cite: Castro Rosero, L. M., Hernandez, I., Espino Infantes, M., and Alsina Torrent, J. M.: Numerical analysis of transport and accumulation of floating marine litter in the Black Sea., EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-2073, https://doi.org/10.5194/egusphere-egu23-2073, 2023.

10:00–10:10
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EGU23-15206
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ECS
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Highlight
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Virtual presentation
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Matvey Novikov, Anfisa Berezina, Svetlana Pakhomova, and Evgeniy Yakushev

The Black Sea contains the largest volume of sulphidic water in the world. The position of the upper boundary of hydrogen sulfide is associated with the supply of oxygen, which is used for the oxidation of organic matter and reduced compounds of several chemical elements, such as sulfur, manganese, iron, nitrogen, etc. Climate change and anthropogenic impact dramatically affect the biogeochemical regime of the Black Sea. The depth of the oxygen layer of the sea depends on vertical mixing, which transfers dissolved oxygen from the upper euphotic layer to deeper layers, and the consumption of dissolved oxygen for the oxidation of autochthonous organic matter (OM) produced in the sea and allochthonous OM delivered with coastal runoff, and for the reduced forms of the listed elements.
The study uses the BROM biogeochemical model, which describes biogeochemical processes in the water column. The BROM benthic-pelagic biogeochemical model combines a relatively simple ecosystem model with a detailed biogeochemical model for the water column, bottom boundary layer, and upper sediment, with a focus on changes in oxygen regime and redox conditions. BROM considers the interrelated transformations of chemical elements (N, P, Si, C, O, S, Mn, Fe) and organic matter (OM) in terms of nitrogen according to the Redfield ratio between the main nutrients.
In this work, we used the previously combined BROM-2DBP model within the FABM framework. In order to more accurately reproduce the fine structure of the redox layer by the model, the parameterization of the change in the vertical velocity of the suspended matter due to aggregation with Mn(IV) oxide was introduced:
WCi=WCi0+WMe∗Mn(IV)/(Mn(IV)+0.1) ,
where WCi is the total vertical velocity, WCi0 is the own vertical velocity of the suspended matter, Mn(IV) is the concentration of Mn(IV) oxide.
The hydrophysical forcing was hourly temperature, salinity, and orthogonal components of currents data for 2010 on a point with coordinates 43.5 °N. 37.75 °E from “Copernicus” portal. 
To take into account stationary recovery conditions, the upper 350 m were used in the calculations. The obtained data were compared with the field observations of the expedition aboard the R/V Knorr in March 2003. The obtained vertical distributions of hydrochemical parameters (a) are consistent with the existing hydrochemical structure of the Black Sea. Dissolved oxygen has a similar distribution in the model and observations, occupying the upper 70 m layer, its origin was located higher than the appearance of hydrogen sulfide at about 150 m. Within the redox layer, nitrate, Mn(IV), Mn(III ), Fe(III), elemental sulfur and a minimum of phosphate. Below the redox layer, the model reproduced the maxima of Mn(II) and Fe(II). Hydrogen sulfide appears at a horizon of about 80 m.
The introduced parametrization of the additional vertical velocity of suspended matter makes it possible to more accurately reproduce the processes of a relatively thin redox layer by taking into account its aggregation with Mn(IV) oxide, which, in turn, can shift the redox layer lower or higher, depending on the availability of Mn(IV) oxide.

How to cite: Novikov, M., Berezina, A., Pakhomova, S., and Yakushev, E.: The oxygen balance analysis in the water column of the Black Sea based on a mathematical model, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-15206, https://doi.org/10.5194/egusphere-egu23-15206, 2023.

Coffee break
Chairpersons: Vanessa Cardin, Katrin Schroeder, Alejandro Orfila
10:45–10:50
10:50–11:00
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EGU23-5442
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On-site presentation
Anna Teruzzi, Ali Aydogdu, Carolina Amadio, Gianpiero Cossarini, Laura Feudale, Alessandro Grandi, Pietro Miraglio, Jenny Pistoia, and Stefano Salon

Biogeochemical seasonal cycle in the Mediterranean Sea is characterized by late-winter early-
spring phytoplankton blooms driven by vertical mixing events that bring nutrients to surface
layers. Relatively intense bloom events are usually observed in areas where mixing is strong and
persistent enough to significantly impact concentration of nutrients in surface layers.
A markerlymarkedly intense bloom was forecasted in spring 2022 by the Med-MFC system, the
production center of the Copernicus Marine Service for the Mediterranean Sea, in the
southeastern basin (in the Cretan area). Thanks to the three-dimensional description of ocean
physical and biogeochemical dynamics at relatively high resolution (1/24°) provided by the
Med-MFC system, it has been possible to investigate various elements of the spring 2022 events.
In particular chlorophyll was 50% higher than usual, and patches of high chlorophyll
concentration lasted for 3/4 weeks. Comparison with satellite observations confirmed the notable
event and its anomaly with respect to past bloom events in the area. In this work, we investigate
the processes occurring in the area in spring 2022 using physical and biogeochemical Med-MFC
products as well as available observations. Results show that the spring 2022 event is particularly
strong with respect to climatology of the area and provide indications on the relationship
between the bloom and the forcing physical processes, e.g., water mass formation and mixing.
Moreover, it has been demonstrated the Med-MFC system capability to monitor in a real time
framework ocean health conditions and extreme marine events in the southeastern
Mediterranean.

How to cite: Teruzzi, A., Aydogdu, A., Amadio, C., Cossarini, G., Feudale, L., Grandi, A., Miraglio, P., Pistoia, J., and Salon, S.: Anomalous 2022 deep water formation and intense bloom event in the southeastern Mediterranean Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5442, https://doi.org/10.5194/egusphere-egu23-5442, 2023.

11:00–11:10
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EGU23-6475
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On-site presentation
Milena Menna, Riccardo Martellucci, Miroslav Gačić, Annunziata Pirro, Giuseppe Civitarese, Elena Mauri, and Vanessa Cardin

Long-term variability of the multiannual circulation inversions of the North Ionian Gyre (Bimodal Oscillating System - BiOS) was analyzed using the surface geostrophic vorticity time-series. The vorticity evolution within the period 1992-2021 in the South Adriatic Pit (SAP) area was compared to the North Ionian one to look for their possible relationship. In parallel, variations in the thermohaline properties from Argo float data in the SAP were analyzed to search for the role of baroclinic forcing in generating the vorticity variability. The long-term variations of the North Ionian vorticity show a clear BiOS signal with prevalently constant amplitude of the cyclonic mode. On the other hand, the anticyclonic mode displays a maximum in the early 1990s and then it decreases in amplitude. The maximum anticyclonic amplitude during this period is associated with the Eastern Mediterranean Transient. The vorticity curve of the SAP shows positive values (cyclonic curl) over the entire period with amplitude which changes rather weakly in the first part of the record up to 2006, while after 2006 it displays large multiannual oscillations showing also a higher long-term average value.  A comparison between the vorticity time-series and the salinity in the SAP shows that large amplitude variations in the second part of the vorticity record are in counterphase with respect to the average 0-150m salinity. This suggests that these large amplitude vorticity variations after the end of the EMT are driven by the horizontal density gradient, which is largely associated with the salinity variations, i.e., baroclinic in origin. As for the long-term trend in salinity over the 30-year time-series, the increase is quite significant.

How to cite: Menna, M., Martellucci, R., Gačić, M., Pirro, A., Civitarese, G., Mauri, E., and Cardin, V.: Long-term variability of the North Ionian Gyre (BiOS); characteristics and causes, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-6475, https://doi.org/10.5194/egusphere-egu23-6475, 2023.

11:10–11:20
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EGU23-12054
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ECS
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On-site presentation
Annunziata Pirro, Elena Mauri, Riccardo Gerin, Riccardo Martellucci, Piero Zuppelli, and Pierre Marie Poulain

The deepwater formation in the northern part of the South Adriatic Pit (Mediterranean Sea) during winter 2018 is investigated using in-situ glider data. After a period of about 2 weeks from the beginning of the mixing phase, a homogeneous convective area ∼110-km-wide and ∼300-m deep, breaks up due to the baroclinic instability process in cyclonic cones made of geostrophically adjusted fluid. The base of these cones is located at the bottom of the mixed layer, and they extend up to the theoretical critical depth Zc. These cones, with a diameter on the order of internal Rossby radius of deformation (∼6 km), populate the convective site, develop beneath it, and have a short lifetime of weeks. Later on, they extend deeper and intrusion from deep layers makes their inner core denser and colder. The breaking mechanism of these cyclonic spinning features occurring during the spreading phase and some bio-geochemical aspects associated to their evolution are also addressed. The observed cones differ from the long-lived cyclonic eddies sampled in other ocean sites and formed at the periphery of the convective area in a postconvection period. In-situ data are also corroborated by theoretical studies, laboratory experiments and model simulations.

How to cite: Pirro, A., Mauri, E., Gerin, R., Martellucci, R., Zuppelli, P., and Marie Poulain, P.: New Insights on the Formation and Breaking Mechanism of Convective Cyclonic Cones in the South Adriatic Pit during Winter 2018, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-12054, https://doi.org/10.5194/egusphere-egu23-12054, 2023.

11:20–11:30
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EGU23-13187
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ECS
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On-site presentation
Iván Manuel Parras Berrocal, Rubén Vázquez, William Cabos, Dmitry V. Sein, Oscar Álvarez, Miguel Bruno, and Alfredo Izquierdo

Dense water formation in the Eastern Mediterranean (EMed) is essential in sustaining the Mediterranean overturning circulation. Changes in the sources of dense water in the EMed point to changes in the circulation and the water properties of the Mediterranean Sea. Here we examine with a regional climate system model the changes in the dense water formation in the EMed through the twenty-first century under the RCP8.5 emission scenario. Our results show a shift in the dominant source of Eastern Mediterranean Deep Water (EMDW) from the Adriatic Sea to the Aegean Sea at the first half of twenty-first century. The projected dense water formation reduces by 75% for the Adriatic Sea, 84% for the Aegean Sea and 83% for the Levantine Sea by the end of the century. The reduction in the intensity of deep water formation is related to hydrographic changes of surface and intermediate water, that strengthen the vertical stratification hampering the vertical mixing and thus the convection. Those changes have an impact on the water that flows through the Sicilian Strait to the Western Mediterranean and therefore on the whole Mediterranean system.

How to cite: Parras Berrocal, I. M., Vázquez, R., Cabos, W., Sein, D. V., Álvarez, O., Bruno, M., and Izquierdo, A.: Dense water formation in the Eastern Mediterranean under global warming scenario, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-13187, https://doi.org/10.5194/egusphere-egu23-13187, 2023.

11:30–11:40
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EGU23-13857
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ECS
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On-site presentation
Beatrice Giambenedetti, Nadia Lo Bue, Vincenzo Artale, and Federico Falcini

The Mediterranean is a climate change hot spot: it is warming 20% faster than the rest of the globe's oceans. Despite the importance of monitoring such dramatic changes and their consequences, the processes and the mechanisms involved in deep-sea variability are still unclear, due to a lack of long-term observations above 2000 m of depth. The availability of seafloor time series data and full-depth CTD profiles collected in the Ionian Sea allowed studying processes connecting the deep variability with the whole water column. The analysis of the in-situ seafloor time series showed a near-inertial peak in the current kinetic energy spectrum in the bottom layer, which hints at the presence of local vorticity. Moreover, the analysis of the CTD profiles revealed for the first time in this area the presence of variability at tidal periodicity in the deep layers (below 2000m), suggesting a connection with what was observed in the surface and subsurface layers. A unique opportunity to study and validate this mechanism was offered by the adjustment of the water stratification before and after the Eastern Mediterranean Transient, the major climate event occurred at the beginning of the 90s when warmer and saltier Aegean waters replaced colder and fresher Adriatic deep waters in the bottom layers of the Ionian basin. Data collected between 1999 and 2003 depict a stable water mass in the Ionian deep layers, identified as the Ionian Abyssal Water (IAW). The presence of the IAW layer could be a key condition for catching such variability in the deep. This allows studying the role that the stratification can have on the rapid propagation of the perturbation in depth, and also how the relative layer thicknesses and different densities can trigger the instability transport throughout the water column. The observed mean structure of the Ionian Sea stratification suggests that a 4-layer scheme should be enough to have a realistic yet straightforward theoretical representation. To study how much and under which conditions a potential vorticity input can propagate, a quasi-geostrophic equation has been considered, with 4 coupled layers of arbitrary thickness and density, simulated with a custom-designed algorithm. The relative stability of the coupled layers, and their response to external forcing, is crucial to understand how vorticity can propagate through the water column down/up and to/from the deepest layers. This case study aims to give more insight into how energy stored by the deep-sea layers can be released along the entire water column. This will enable a better parametrization of the deep processes also contributing to future Mediterranean climate numerical models.

How to cite: Giambenedetti, B., Lo Bue, N., Artale, V., and Falcini, F.: Role of stratification in vorticity propagation throughout the entire water column: a Mediterranean example (Ionian Sea), EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-13857, https://doi.org/10.5194/egusphere-egu23-13857, 2023.

11:40–11:50
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EGU23-14768
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Virtual presentation
Steve Brenner, Isaac Gertman, Tal Ozer, Simona Simoncelli, and George Zodiatis

An analysis of in-situ data gathered over the two decade post POEM period in the South-Eastern Levantine Basin from extensive hydrographic (CTD) campaigns and VOS XBT transects, along with data provided by the latest SeaDataCloud Mediterranean Sea Temperature and Salinity climatology (http://dx.doi.org/10.12770/3f8eaace-9f9b-4b1b-a7a4-9c55270e205a) and the Mediterranean Sea Physics Reanalysis from the Copernicus Marine Service (CMS; https://data.marine.copernicus.eu/product/MEDSEA_MULTIYEAR_PHY_006_004), have all provided insight on the dominant, coherent, meso-scale, circulation features as well as the evolution and variability of the thermohaline properties of the main water masses in this sub-basin. The most pronounced feature, the warm core Cyprus Eddy, migrates over the broad region of the Eratosthenes seamount and exhibits significant seasonal and inter-annual spatio-temporal variability. Another prominent structure is the anticyclonic Shikmona Eddy generated periodically due to instabilities of the strong northward flowing jet along the south-easternmost shelf and slope of the Levantine basin. Its evolution and co-existence with the Cyprus Eddy for periods of a few months, affects the temporal re-establishment of the Shikmona Gyre, which was first observed during the POEM cruises in the mid 1980s. The eastward flowing Mid Mediterranean Jet (MMJ) defines the northern flanks of these sub-basin scale eddies and transports the lower salinity Modified Atlantic Water (MAW) through the warmest and most saline region of the Mediterranean. Periodically the MMJ bifurcates and/or is diverted northward, along the western coast of Cyprus due to spatial fluctuations of the Cyprus Eddy. Four active periods were identified with either a dominant Cyprus Eddy only or coexisting Cyprus and Shikmona Eddies. This long term in-situ monitoring also provides an overview of the extent of the main water masses and characterizes their variability throughout the period considered. The temperature and salinity of the Levantine Surface Water (LSW) and of the subsurface MAW have increased. The Eastern Mediterranean Transient Water (EMTW) is shown to occupy the deep cavities, below the Eastern Mediterranean Deep Water (EMDW), in the vicinity of the Eratosthenes seamount while its upper boundary was lifted to shallower depths over the same period.

How to cite: Brenner, S., Gertman, I., Ozer, T., Simoncelli, S., and Zodiatis, G.: Dominant features and variability of the mesoscale circulation and thermohaline structure of the eastern Levantine during the post POEM period 1995-2015, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-14768, https://doi.org/10.5194/egusphere-egu23-14768, 2023.

11:50–12:00
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EGU23-5490
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ECS
|
On-site presentation
Lénaïg Brun, Ivane Pairaud, Ricardo Silva Jacinto, Pierre Garreau, and Bernard Dennielou

The more than 6000 submarine canyons worldwide constitute key oceanic morphologies incising continental slopes. They favor exchanges of organic matter, water masses, carbon, heat or pollutants between shallow and deep waters, driving ecosystems. They interact with the shelf and slope circulation generating local dynamics that have rarely been surveyed and observed.

Observations of currents, temperature and turbidity along the Cassidaigne canyon, in the Gulf of Lions, northwestern Mediterranean Sea, were carried out to understand the specific circulation patterns in submarine canyons and their transitions. Two oceanographic cruises led in 2017 and 2019 gathered data from the outer shelf and canyon head at 100-400 m to the base of the continental slope at 1900 m depth.

The Cassidaigne canyon is characterized by a steep and narrow morphology and is located in an active circulation area. Near the canyon head and on the shelf, the current is modulated by the stratification, the bottom morphology, the general circulation and the wind. Intermittent upwellings and consecutive relaxations lead to strong transient dynamics characterized by near inertial oscillations inside the canyon. The succession of upwellings induce a quasi-permanent residual up-canyon flow as observed in the narrow gorge area at 1700 m depth. Along-slope currents crossing the canyon during Northern Current intrusion events in the Gulf of Lions favor a temporary down-canyon circulation. Finally, turbidity currents were observed for the first time in connection with upwelling events, suggesting the triggering role of canyons’ internal hydrodynamics on shelf sedimentary processes.

How to cite: Brun, L., Pairaud, I., Silva Jacinto, R., Garreau, P., and Dennielou, B.: Hydrodynamics of the Mediterranean Cassidaigne submarine canyon from observations, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-5490, https://doi.org/10.5194/egusphere-egu23-5490, 2023.

12:00–12:10
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EGU23-6743
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On-site presentation
|
Giuseppe Aulicino, Yuri Cotroneo, Paolo Celentano, Angelo Perilli, Federica Pessini, Antonio Olita, Pierpaolo Falco, Roberto Sorgente, Alberto Ribotti, Giannetta Fusco, and Giorgio Budillon

The Western Mediterranean basin (WMED) is characterized by the presence of energetic and dynamic mesoscale cyclonic and anticyclonic eddies. They mainly originate along the Algerian and the Northern currents and have a large influence on the basin circulation. Eddies can last for months, with longer lifetimes associated with the anticyclones, which can move far from their areas of origin. As they partially isolate and transfer water masses, they also have an impact on water properties (physical, chemical and biological), pollutant’s dispersion and transport of eggs, larvae and planktonic organisms. In this study, a connectivity analysis method is applied to the anticyclonic eddies (AEs) identified by an automated hybrid detection and tracking algorithm south of 42° N in the WMED. The same methodology is also applied to the trajectories of Lagrangian surface drifters available in the study area. The purpose is to highlight the connections between different areas of the basin linked to eddy activities in addition to the connectivity due to the mean surface circulation. Drifter data analysis showed that all the WMED sub-basins are strongly interconnected, with the mean surface circulation allowing a shortcut connection among many areas of the basin. The connectivity analysis of the AEs tracks shows that although AEs are ubiquitous in the WMED, their connectivity is limited to well-defined regions, depending on their origin location. Three main regions: the south-western, the south-eastern and the northern parts of the basin are characterized by AEs recirculation, with sporadic export of eddies to the other WMED zones.

How to cite: Aulicino, G., Cotroneo, Y., Celentano, P., Perilli, A., Pessini, F., Olita, A., Falco, P., Sorgente, R., Ribotti, A., Fusco, G., and Budillon, G.: Connectivity analysis applied to mesoscale eddies in the Western Mediterranean basin, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-6743, https://doi.org/10.5194/egusphere-egu23-6743, 2023.

12:10–12:20
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EGU23-6024
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On-site presentation
|
Yuri Cotroneo, Giuseppe Aulicino, Giannetta Fusco, Simon Ruiz, Ananda Pascual, Pierre Testor, Pierre Cauchy, Nikolaos Zarokanellos, Albert Miralles, Mohamed Zerrouki, Joaquin Tintoré, and Giorgio Budillon

Algerian Basin Circulation Unmanned Survey – ABACUS - has been carried on since 2014 across the Algerian Basin to investigate high resolution variability of the first 1000 m of the ocean and to fill the gap in data collection in this area of the Western Mediterranean Sea.

Five deep SLOCUM G2 glider missions were carried out in the AB between 2014 and 2022 by Università degli Studi di Napoli Parthenope, in collaboration with Balearic Islands Coastal Observing and Forecasting System (SOCIB) and the Mediterranean Institute for Advanced Studies (IMEDEA CSIC-UIB), with the participation of scientists from Algeria, France and Canada. A sixth mission (ABACUS 2023) is indeed in progress. ABACUS projects were supported since 2014 through the Trans National Access (TNA) calls of JERICO, JERICO-NEXT and JERICO S3 programmes and through the SOCIB glider facility open access programme.

Recently, ABACUS line was also added to the Boundary Ocean Observing Network (BOON) of the OceanGliders programme that proposes the long term and sustained observation of oceanographic features using the unique capabilities of the gliders.

To date, a total of 22 deep glider ABACUS transects were realized between the island of Mallorca and the Algerian coast. Each mission had an average duration of about 40 days and was mainly carried out during fall and/or early winter (2014–2018, 2021-2022) or spring (2018, 2022). All the glider surveys were conducted along neighboring SARAL/AltiKa (2014-2016) and Sentinel-3A (2018, 2021-2022) satellite groundtracks. The timing of the glider missions were accurately planned to optimize the synopticity between in situ and remote sensed observations.

All the ABACUS gliders were equipped with a glider-customized CTD measuring temperature, conductivity/salinity and pressure/depth; a two-channel combo fluorometer sensor by WetLabs (for Chl-a concentration and turbidity measurement); and an oxygen optode by AADI to measure absolute oxygen concentration and saturation. During the last two missions, the glider was also equipped with a passive acoustic probe to study wind and rain events during the mission, as well as the presence of marine mammals in the monitored area.

ABACUS data are freely available through a dedicated webpage and cooperation with new scientists is strongly encouraged. This presentation aims at making the scientific community aware of the importance and possibilities offered by ABACUS and similar glider monitoring lines, as well as at enlarging the ABACUS science team to fully exploit the collected ocean observations.

How to cite: Cotroneo, Y., Aulicino, G., Fusco, G., Ruiz, S., Pascual, A., Testor, P., Cauchy, P., Zarokanellos, N., Miralles, A., Zerrouki, M., Tintoré, J., and Budillon, G.: ABACUS – a repeated glider monitoring line across the western Mediterranean Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-6024, https://doi.org/10.5194/egusphere-egu23-6024, 2023.

12:20–12:30
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EGU23-13547
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On-site presentation
Pierre-Marie Poulain, Luca Centurioni, Tamay Ozgokmen, Irina Rypina, Amala Mahadevan, Leo Middelton, Shaun Johnston, and Eric D'Asaro

A submesoscale cyclonic eddy, less than 10 km in diameter, was observed in the Balearic Sea from inception to dissipation for more than a month in winter 2022 The feature was heavily sampled by freely-drifting (Lagrangian) instruments to study its kinematics, spatial structure and temporal evolution.  The Lagrangian sensors included drifters, wirewalkers and profiling floats. Additional shipboard data (underway CTD, ADCP) and remote sensing images revealed that the eddy was formed by doming isopycnals, extending more than 200 m in depth, with dense salty water at the center. The near-surface chlorophyll concentration was maximum in the eddy center, as clearly seen in ocean color satellite images.

The eddy formed in late February by pinching off from a larger cyclonic feature via the collapse of a sharp submesoscale ridge that connected it to a larger cyclone. Wavelet analysis of the drifter trajectories revealed that the submesoscale eddy had a maximum orbital speed of ~ 30 cm/s, at a radius of ~3 km. In its inner core, vorticity was as large as twice the local inertial frequency (Rossby number ~ 2). The surface drifters made looping tracks that were slightly elliptical. Tracked by the swarm of drifters until mid-March, the eddy remained surprisingly coherent as it moved to the South and then East with a drift speed between 2 and 5 cm/s. After a strong wind event, just a few drifters remained in the eddy until it weakened and dissipated in early April.

These observations were a part of the CALYPSO program, an ONR Departmental Research Initiative that addresses the challenge of observing, understanding and predicting the three-dimensional pathways by which water from the surface ocean makes its way into the deeper ocean. Vertical transports by submesoscale fronts and eddies can play an important role in ocean and climate dynamics.

How to cite: Poulain, P.-M., Centurioni, L., Ozgokmen, T., Rypina, I., Mahadevan, A., Middelton, L., Johnston, S., and D'Asaro, E.: Evolution of a submesoscale cyclone in the Balearic Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-13547, https://doi.org/10.5194/egusphere-egu23-13547, 2023.

Posters on site: Fri, 28 Apr, 14:00–15:45 | Hall X5

Chairpersons: Vanessa Cardin, Arthur Capet, Katrin Schroeder
X5.324
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EGU23-2871
Vanessa Cardin, Felipe de Luca Lopes de Amorim, Laura Ursella, and Achim Wirth

The EMSO-E2M3A South Adriatic Regional Facility provides high-frequency (every hour) temperature and salinity data from 2006 to 2019 along the water column from 150 dbar to the seafloor. Their study reveals processes on different temporal scales, i.e. daily, seasonal, intra-annual and inter-annual, as well as their recurrence (seasonal or not) and climatic trends. The area is characterized by cyclonic circulation, which preconditions deep convection processes that involve both atmospheric and ocean dynamics, forming new, dense and oxygen-rich waters. There are intermittent influxes of high salinity water from the Ionian Sea, that favor salt fingering, and dense overflows from the northern Adriatic. The region is also subject to strong surface cooling. Data collected by the E2M3A observatory allows monitoring of variability on short scales related to convection and submesoscale processes. On an intermediate time scale, changes in basin circulation are monitored, and on a larger time scale, climate variability in the area is monitored. The various processes interact in a nonlinear manner, highlighting the importance of high-frequency measurements of rapid processes and their interaction with and correction of slowly varying properties on a longer time scale.

From ADCP data, the signature of zooplankton migration at the surface/intermediate layer is determined to be enhanced by convection-induced mixing. On the monthly scale, thermohaline variability increases substantially due to oscillations triggered by a combination of factors that include salinity intrusion into the intermediate layer, strong heat loss at the surface, and variability in vorticity during the winter months. The lower layer of the pit has been characterized by a slightly positive trend in temperature and salinity over the last decade, interrupted only by the inflow of dense water from the northern Adriatic Sea cascading through the Canyon of Bari.

How to cite: Cardin, V., de Luca Lopes de Amorim, F., Ursella, L., and Wirth, A.: The EMSO-E2M3A Southern Adriatic Regional Facility: Interconnectedness of a variety ofprocesses at different spatial and temporal scales, their interaction and recurrence., EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-2871, https://doi.org/10.5194/egusphere-egu23-2871, 2023.

X5.325
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EGU23-3265
Angelo Rubino, Sara Rubinetti, and Davide Zanchettin

Sea surface temperature (SST) is of paramount importance for comprehending ocean

dynamics and hence the Earth’s climate system. Accordingly, it is also the most measured

oceanographic parameter. However, until the end of the XIX century, no continuous time series of

SST seem to exist, with most of the available data deriving from measurements on ships. Here,

we present a continuous record of surface water measurements retrieved thrice daily in the Venice lagoon,

in the northeastern part of the Italian peninsula, from June to August 1851 and 1852. To the best of our

knowledge, these data represent the oldest SST time series of the entire world ocean. The

measurements were performed by immersing a Réaumur thermometer a few meters deep in the

lagoon water at 8 a.m., 12 p.m., and 8 p.m. Despite several limitations affecting these data (e.g.,

lacking information regarding the exact water depth where measurements were performed and

instrumental metadata), they are of utmost significance, as they put many decades backward the

date of the development of a fundamental aspect of oceanographic observations. Moreover, the

data were collected close to the Punta della Salute site, where actual sea water temperature

measurements have been performed since 2002. Therefore, a unique comparison between

surface water temperatures within the Lagoon of Venice across three centuries is possible.

How to cite: Rubino, A., Rubinetti, S., and Zanchettin, D.: Mid-XIX Century Estuary SST Time Series Recorded in the Venice Lagoon, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-3265, https://doi.org/10.5194/egusphere-egu23-3265, 2023.

X5.326
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EGU23-3520
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ECS
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John Karagiorgos, Vassilios Vervatis, and Sarantis Sofianos

Marine chlorophyll concentration has an impact on turbidity affecting the upper-ocean properties and regulating the air-sea fluxes. This work aims at assessing the effect of turbidity, as estimated via surface chlorophyll, on the heat content and dynamics of the Mediterranean and Black Seas. We performed twin-simulation experiments using a regional configuration of the NEMO v4.2 ocean model comparing: 1) a run with climatological chlorophyll satellite data to estimate turbidity and shortwave penetration in the water column, with 2) a reference run of fixed turbidity (i.e., chlorophyll concentration fixed at 0.05 mg/m3) corresponding to Yerlov type I clear waters. Interim results for long-term simulations (2008-2018) show that considering the effects of turbidity, as estimated from realistic surface chlorophyll concentrations, increases sea surface temperature, amplifies the seasonal cycle of temperature in the surface layer (0-20 m), and increases the annual heat loss in the Mediterranean Sea by about 1.5 W/m2. The latter is explained because the surface warming during summer is more intense than the cooling observed during winter, with differences between the two experiments reaching up to 2 °C in some regions. The increasing turbidity also affects the subsurface layers (20-200 m), with cooler temperatures throughout the year due to less solar radiation penetrating the water column. Ongoing work is currently being undertaken to estimate the indirect atmospheric feedback due to turbidity changes, using a fully-coupled ocean-atmosphere system (NEMO-WRF).

How to cite: Karagiorgos, J., Vervatis, V., and Sofianos, S.: The effect of water turbidity on the upper-ocean properties and dynamics in the Mediterranean and Black Seas, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-3520, https://doi.org/10.5194/egusphere-egu23-3520, 2023.

X5.327
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EGU23-13320
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ECS
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Eleonora Cusinato, Angelo Rubino, Silvio Gualdi, and Davide Zanchettin

The Mediterranean Sea is one of the few regions in the world where ocean deep convection events occur, contributing to trigger the local thermohaline circulation. The variability of this circulation is typically affected by large-scale atmospheric modes of variability of Atlantic and Eurasian origin, like, e.g., the North Atlantic Oscillation (NAO), the Eastern Atlantic pattern (EA), the Eastern Atlantic Western Russian pattern (EAWR) and the Scandinavian pattern (SCA). 

Whereas previous studies assessed the impacts of these modes on air-sea heat and freshwater fluxes over the Mediterranean Sea, few studies explored the propagation of these signals from the surface towards the interior of the Mediterranean Sea and mostly they relied on the use of single model simulations.

In this contribution we investigate the Mediterranean thermohaline response to winter forcing from NAO, EA, EAWR and SCA using a multi-model analysis of evaluation simulations belonging to the Med-Cordex initiative. We present results from a composite analysis around strong positive and negative phases of these modes to track the propagation of the associated signals from the sea surface towards the Mediterranean interior in key regions such as the South Adriatic, the Aegean and Levantine Seas and the Gulf of Lion. 

Different simulations show only a partial agreement as far as the identification of the modes mostly contributing to deep water formation is concerned.

How to cite: Cusinato, E., Rubino, A., Gualdi, S., and Zanchettin, D.: Mediterranean sea-surface and deep responses to large-scale atmospheric forcing in evaluation Med-Cordex simulations, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-13320, https://doi.org/10.5194/egusphere-egu23-13320, 2023.

X5.328
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EGU23-16141
Maximo Garcia-Jove, Baptiste Mourre, Alex Santana, Nikolaos D. Zarokanellos, Pierre F. J. Lermusiaux, Daniel L. Rudnick, and Joaquín Tintoré

The CALYPSO research program, funded by the Office of Naval Research, aims to understand the coherent pathways from the surface ocean to the interior. In February and March 2022, the CALYPSO campaign surveyed the upper layers of the Balearic Sea (Western Mediterranean), providing high-resolution observations of mesoscale and submesoscale structures. This included submesoscale density fronts, stretching regions and small coherent eddies. In this work, we analyze the formation, evolution, and impact of these submesoscale structures in the development of vertical velocities and in the determination of three-dimensional pathways from the surface to the ocean interior. We combine multi-platform in-situ observations with high-resolution numerical simulations both in free-run and data-assimilative modes. In particular, the WMOP reanalysis  assimilates remote sensing observations of temperature and sea level anomaly as well as vertical profiles of temperature and salinity from floats, underway CTD and gliders obtained during the CALYPSO campaign. The simulations are shown to realistically reproduce the main characteristics of the Balearic front and some of the associated submesoscale patterns, providing an appropriate tool to analyze the processes responsible for vertical velocities development. Particle tracking analyses indicate pathways for vertical exchange of water between the surface and the ocean interior in the frontal region. Finally, the process of frontogenesis and the submesoscale structures play an important role in the development of the vertical velocities and the energy transfers.

How to cite: Garcia-Jove, M., Mourre, B., Santana, A., Zarokanellos, N. D., Lermusiaux, P. F. J., Rudnick, D. L., and Tintoré, J.: Vertical pathways associated with a submesoscale density front in the Balearic Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-16141, https://doi.org/10.5194/egusphere-egu23-16141, 2023.

X5.329
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EGU23-17193
Vincenzo Artale, Tiziana Ciuffardi, Nadia LoBue, Giancarlo Raiteri, and Franco Reseghetti

The warming trend is already well known for the Mediterranean region, which is considered a climate hotspot warming 20 % faster than the global average. Every year, the Mediterranean Sea reaches new records for seawater warming, and year after year, this heat is penetrating deeper and deeper into the sea. New temporal and spatial evidence of this thermal penetration were depicted in the Tyrrhenian Sea thanks to a twenty-year continuous XBT monitoring. This work aims at dealing with the Tyrrhenian Sea sub-basin dynamics and processes. In particular, the mechanisms responsible for penetration of warming signal down to the deep layers (1800 m). What can hinder or exacerbate this spread and what areas are mostly affected by mechanisms of propagation and why?

It’s well known that the seafloor's uneven topography and bottom roughness influences ocean circulation in two basic ways: first, it steers local vorticity flows; second, it provides barriers that prevent deep waters from mixing, except within deep passageways and straits that connect ocean basins or in hydraulically controlled overflow regions. The ways in which the warm signal entering from the south spreads rapidly northward affecting the entire Tyrrhenian Sea basin will be depicted, also considering its sub-basin peculiarities, such as features of the wind-driven surface circulation, strong stratification, and related mixing processes along the entire water column as well as its variability.

How to cite: Artale, V., Ciuffardi, T., LoBue, N., Raiteri, G., and Reseghetti, F.: Thermal penetration evidence recorded since 1999 in the deep Tyrrhenian Sea (Mediterranean Sea), EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-17193, https://doi.org/10.5194/egusphere-egu23-17193, 2023.

X5.330
|
EGU23-17543
Arthur Capet, Evan Mason, Luc Vandenbulcke, and Marilaure Gregoire

The Black Sea is a largely enclosed basin that experiences minimal exchange with the Mediterranean through the 0.7 km wide Bosphorus Strait. It receives significant freshwater discharge from several large rivers. Mesoscale eddies are numerous in the Black Sea. They have been observed, tracked,  and sampled over several decades. Previous eddy identification efforts have focused on surface circulation, aided by sea surface height maps compiled  from space-borne altimeters. We use a 3d high-resolution model solution that solves both physical and biogeochemical variables that enable us to  provide a comprehensive evaluation of the oxygen dynamics within the near-shore Black Sea eddy field. By this, we confirm and explain the strong subsurface oxygen anomalies formerly revealed underneath anticyclones on the basis of Argo floats and detail the transport and the biogeochemical processes involved.

How to cite: Capet, A., Mason, E., Vandenbulcke, L., and Gregoire, M.: Contribution of coastal anticyclones to Black Sea oxygen dynamics, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-17543, https://doi.org/10.5194/egusphere-egu23-17543, 2023.

Posters virtual: Fri, 28 Apr, 14:00–15:45 | vHall CR/OS

Chairpersons: Vanessa Cardin, Arthur Capet, Katrin Schroeder
vCO.7
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EGU23-588
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ECS
Xiaoqin Yan and Youmin Tang

The multidecadal variability in Mediterranean Sea surface temperature (MSMV) exerts important climate impacts on both the Mediterranean region and remote areas at hemispheric scales and has long been identified in previous studies. However, its key region and source are still unclear. For the first time, we show that the key region of the MSMV is in the eastern Mediterranean, where the MSMV can persist throughout the year. The MSMV in the central and western Mediterranean occurs mainly in summer. Comparison of the North Atlantic Oscillation (NAO) and Atlantic Multidecadal Variability (AMV) indices shows that the cumulative NAO index has a better consistency with the MSMV, suggesting that the MSMV most likely results from the cumulative effect of NAO atmospheric forcing on ocean circulation in the Mediterranean Sea. The stable lag relationship between the cumulative NAO index and the MSMV provides a natural indicator for the decadal prediction of the MSMV.

How to cite: Yan, X. and Tang, Y.: Multidecadal Variability in Mediterranean Sea Surface Temperature and Its Sources, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-588, https://doi.org/10.5194/egusphere-egu23-588, 2023.

vCO.8
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EGU23-3361
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ECS
Anıl Akpınar and Bettina Fach

Fronts are ubiquitous features in the ocean, having significant implications for oceanic and atmospheric environments, including; water masses, currents, ocean-atmosphere interactions, and ecosystems, particularly through cross-front exchanges of water masses, materials and biota. In this work, we investigate thermal fronts in the Levantine Basin of the Mediterranean Sea, using remotely sensed sea surface temperature data. First, a frontal detection algorithm is used to determine the fronts. Then the spatial and temporal variability of the fronts are presented. A specific focus lies on the fronts associated with the Asia Minor boundary current, due to its frontal instabilities and associated eddy activity. Detected fronts are used as a basis to investigate these features and their contribution to cross-frontal exchanges. Further work includes identification of in-situ data gaps in existing observatories around fronts to provide an effective monitoring strategy of fronts in the region.

 

This work has been produced benefiting from the 2236 Co-Funded Brain Circulation Scheme2 (CoCirculation2) of TÜBITAK (Project No: 121C411). However, the entire responsibility of the publication belongs to the owner of the publication. The financial support received from TÜBITAK does not mean that the content of the publication is approved in a scientific sense by TÜBITAK.

How to cite: Akpınar, A. and Fach, B.: Sea surface temperature fronts in the Levantine Basin of the Mediterranean Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-3361, https://doi.org/10.5194/egusphere-egu23-3361, 2023.

vCO.9
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EGU23-6977
Kristofer Döös, Jihene Abdennadher, and Moncef Boukthir
The water mass transformation in the Gulf of Gabès and its associated overturning circulation is investigated. The strong all year evaporation in the Gulf leads to a salinification of the entering water masses, which hence return with a strong salinity increase.  The heat transports in and out have a strong seasonal cycle, with approximately as much entering as exiting the Gulf in the yearly mean.
The overturning circulation is calculated from Lagrangian trajectories, which makes it possible to follow in detail the water mass transformation from where the water enters in the north, following an anticlockwise circuit along the coast in the Gulf until it exits in the southeast. The densest and most saline water exits, however, in the deepest middle part of the Gulf, where it tends to mix with the slightly fresher Mediterranean Waters. The trajectories are computed with the velocity and mass transport fields from a high-resolution (1/96°) hydrodynamic model, which includes the strong tides in this part of the Mediterranean.
 
Figure: Examples of trajectories entering and exiting the Gulf of Gabès. Colour for individual trajectories as a function of salinity. 

How to cite: Döös, K., Abdennadher, J., and Boukthir, M.: The residence time and overturning circulation of the Gulf of Gabès in the Eastern Mediterranean Sea, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-6977, https://doi.org/10.5194/egusphere-egu23-6977, 2023.

vCO.10
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EGU23-8252
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ECS
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Ioannis Mamoutos, Vassilis Zervakis, and Elina Tragou

The North Aegean Sea is one of the most interesting seas of the Mediterranean, being under the dominant impact of the Black Sea waters though the so-called Turkish Strait System (TSS – including the Dardanelles and Bosphorus Straits and the Marmara Sea). Moreover, it constitutes a potentially deep water formation site of the Eastern Mediterranean Sea along with the Adriatic Sea. Previous studies for the region focused – rightly – on the crucial role of low salinity Black Sea waters in controlling the overall thermohaline function and dynamics of the North Aegean. None of the previous modeling approaches studied the impact of tides in the mixing processes and the production of extremely dense water, especially during 1987, 1992 and 1993 when major deep water formation events took place in the region. In this work we examine the tidal impact via several long term simulations using a high resolution (1.0 km) ocean model covering the period from 1985 to 2013.

The Regional Ocean Model System (ROMS) was used for two 28-year-long hindcasts. A computational grid of approximately 1.0 km horizontal resolution in both directions and 31 vertical sigma (σ) levels was develop to cover the region of interest that extends from 22.5ºE to 27.25º E in longitude and 38.35º N to 41.2º N in latitude. Atmospheric forcing fields from ECMWF ERA5 reanalysis dataset with a spatial resolution of 0.25 degrees and hourly time step were used. The inflow from the Black sea to the North Aegean was treated as an open (east) boundary condition and data from Vladimir Maderich work was used as input. The tidal forcing, in total eight (8) harmonics – four diurnal and four semidiurnal – came from Oregon State University (OSU) inverse global tidal model. Two identical simulation – in terms of model setup and input – were conducted: the first without and the second with tidal forcing.

After extensive validation of the model’s results, using all available in situ data from different platforms, a comprehensive analysis was conducted and our findings reveal that model results employing tidal forcing exhibit a closer proximity to observations than non-tidal results, thus validating the necessity to incorporate tidal forcing. Furthermore, the use of barotropic tidal forcing enchanced meridional exchanges of heat, salt and buoyancy between the North and South Aegean, thus increasing the stratification and buoyancy content of the upper water column prior to winter mixing. The most significant and surprising result however is that the dense-water volumes produced using tidal forcing were much higher than the ones without tides, a fact signifying the complexity of processes involved prior to and during dense-water formation.

This work was partly covered by the project “Coastal Environment Observatory and Risk Management in Island Regions AEGIS+” (MIS 5047038), implemented within the Operational Program “Competitiveness, Entrepreneurship and Innovation” (NSRF 2014-2020), co-financed by the Hellenic Government (Ministry of Development and Investments) and the European Union (European Regional Development Fund).

How to cite: Mamoutos, I., Zervakis, V., and Tragou, E.: Investigating the impact of tides in the North Aegean on the deep water formation events (DWFe) during Eastern Mediterranean Transient (EMT)., EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-8252, https://doi.org/10.5194/egusphere-egu23-8252, 2023.

vCO.11
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EGU23-13363
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ECS
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Manos Potiris, Ioannis G. Mamoutos, Vassilis Zervakis, Elina Tragou, Dimitris Kassis, and Dionysios Ballas

The observed warming and salinification of the eastern Mediterranean Sea (EMed) during the last decades could impact the dense water formation (DWF) and consequently the thermohaline circulation of the basin. The main drivers of interannual DWF variability in the EMed are the atmospheric heat fluxes, the internal redistribution of salt, and the exchange of heat and salt at its straits. Extremely high salinity has been observed recently in the Levantine and Adriatic Seas due to the superposition of the basin’s decadal variability and long-term trend.

In the Aegean Sea, a major DWF site of the EMed, record-high salinity is recorded in the upper and intermediate layers since 2018. Argo floats observations also show that the Aegean Sea is in the most prolonged state of increased DWF after the Eastern Mediterranean Transient (EMT) period.

The causes of increased salinity and DWF in the Aegean Sea were investigated using: 1) in situ hydrographic observations, 2) satellite observations of sea surface height (SSH), 3) in situ- and model-based gridded hydrography reanalysis products, 4) atmospheric forcing from model reanalysis, and 5) information of Black Sea Water (BSW) inflow in the Aegean Sea from a box model, literature, and an SSH-based index coined in this study.

The long-term increase of salinity in the Aegean Sea follows that of the EMed, and its interannual/decadal variability is dictated by the reversals of the North Ionian circulation and the inflow of BSW. The BSW inflow has a negative trend which results in the decreased dilution of the Aegean Sea and the reduced salinity difference between the Levantine and Aegean Seas, especially after 2012. Surface buoyancy loss also presents significant decadal variability, with peaks in 1993/2003/2012/2022 and anomalously high winter-mean heat loss from 2017 onwards, which coincides with the known post-EMT DWF events in the Aegean Sea. The record-high salinity observed in the Aegean Sea is attributed to the decreased BSW inflow and the anticyclonic reversal of the North Ionian circulation. The decreased BSW inflow and increased surface heat loss can explain the persistence of high salinity and increased DWF in the Aegean Sea from 2020 onwards, despite the cyclonic circulation of North Ionian Sea and the drop of salinity in the Levantine Sea since 2019. In particular, analysis from Argo observations and output of a data assimilating hydrodynamic model developed in the context of the project “Coastal Environment Observatory and Risk Management in Island Regions AEGIS+” revealed widespread formation of water with σ0 > 29.35 kg/m-3.

Post-EMT periods of minor DWF in the Aegean Sea coincide either with the anticyclonic circulation of the North Ionian Sea or with the increased surface buoyancy loss over the Aegean Sea, as a synchronous DWF-favoring phase of both drivers has not occurred yet. However, the common denominator of all major post-EMT DWF events in the Aegean -also true for the EMT period- is the reduced inflow of BSW, which seems to be controlled by the freshwater budget of the Black Sea rather than the temperature-driven increase of SSH in the Mediterranean Sea.

How to cite: Potiris, M., Mamoutos, I. G., Zervakis, V., Tragou, E., Kassis, D., and Ballas, D.: Record-high salinity and interannual dense water formation variability in the Aegean Sea coincide with reduced inflow of Black Sea Water, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-13363, https://doi.org/10.5194/egusphere-egu23-13363, 2023.

vCO.12
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EGU23-15096
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Erdal Tokat and Şükrü Beşiktepe

This study focuses on spatio-temporal climatology and long-term variability of sea surface temperature (SST) in the region of Turkish Straits System for the period 1980-2021. For this purpose, daily SST data from the Advanced Very High-Resolution Radiometer (AVHRR) version 5.3 were used. From this dataset, 40 years of monthly, seasonal, and yearly mean SST time series and spatial fields and their descriptive statistics were calculated. In addition, daily air temperature and sea temperature data that obtained from the Turkish State Meteorological Service (TSMS) for the period 1980-2021 were analysed and compared with AVHRR SST data. Interannual and interdecadal variability of the SST was investigated by using linear trend analysis. The results of this study showed that all regions are experiencing a steady warming trend. In comparison to the north Aegean Sea (0.050 °C.yr-1) and the western Black Sea (0.060 °C.yr-1), the Sea of Marmara shows the largest positive SST annual mean trend (0.064 °C.yr-1). The basin-averaged yearly mean SST anomalies exhibits a similar variability and pattern across all regions: From 1982 to 1998, negative anomalies dominant, from 1999 to 2006, anomalies generally fluctuate around normal, and from 2007 onward, positive anomalies predominant. The seasonal cycle is strong for all regions, with lower SST values in the winter months (January, February, and March) and higher SST values in the summer (July, August and September). From one decade to the next, the SST values in the seasonal cycle gradually increasing. According to the monthly mean climatic SST fields, due to the seasonal upwelling, the eastern Aegean Sea coast experiences lower SST values in the summer compared to all other regions. These findings imply that, over the 40-year study period, the SST values have consistently increased for all regions.

How to cite: Tokat, E. and Beşiktepe, Ş.: Climatology and Variability of Sea Surface Temperature in the Region of Turkish Straits System, 1982-2021, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-15096, https://doi.org/10.5194/egusphere-egu23-15096, 2023.

vCO.13
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EGU23-15714
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ECS
Nikolaos Zarokanellos, Daniel Rudnick, Baptiste Mourre, Maximo Garcia-Jove, Pierre Lermusiaux, and Joaquín Tintoré

Mesoscale features and their corresponding submesoscale structures may generate a substantial vertical transport of carbon and biogeochemical tracers from the surface to the interior. The baroclinic instabilities formed from the Northern and Balearic Currents are associated with vigorous mesoscale eddy activity in the Balearic Sea. In the CALYPSO 2022 experiment, eight gliders were programmed to dive as deep as 700 m from 25 March until 21 June 2022. The glider fleet measured temperature, salinity, velocity, chlorophyll fluorescence, oxygen, and acoustic backscatter. The glider data was mapped utilizing objective mapping of the across-front, along-front, and time on 10 m vertical levels. The geostrophic velocity was inferred using a variational approach. We estimate the vertical and ageostrophic horizontal velocities using the omega equation. The glider observations provide a complete description of the evolution of the eddy field. The analysis of the uplifted isopycnal surface as the eddy formed showed consistency between the movement of the dynamic and biogeochemical tracers. Glider data show the evolution of a cyclonic eddy (20-30 km) in the area, where vertical velocities tend to be downward. As the eddy developed, its axis shifted westward. The isopycnal uplift inside the pycnocline can provide nutrients to the euphotic zone. While the initial cyclonic feature has dissipated, a second shoaling of the 28.9 isopycnal occurred in the east toward the end of April 2022, where the biggest relative vorticity (~0.5 ζ/f) was observed in the region. The eddy extended during its growing phase, showing a westward shift of the eddy axis. The observed peak downward vertical velocities were near 30 m day-1 during the eddy intensification, with the size of the cyclonic eddy varying between 20-30 km. The new cyclonic feature has been spreading in the area for a few days before dividing into two separate cyclonic eddies (15km) around the beginning of May. The two smaller cyclonic eddies moved north and west until they vanished from our study area. However, an anticyclonic structure (20km) was developed within their separation. The vertical velocity tended to be downward on the dense side of the front and upward on the light side, flattening the eddy characteristic. The glider observations reveal horizontal density gradients up to 0.5 kg m-3 over ~10 km. The obtained maximum velocities were up to 30 cm/s in the region. Upwelling and downwelling were also detected by chlorophyll fluorescence, oxygen, and acoustic backscatter near the frontal interface. Glider observations were integrated with remote sensing and modeling simulations to evaluate mesoscale and submesoscale variability in developing vertical velocities in the Balearic Sea and their impact on biological carbon storage.

 

How to cite: Zarokanellos, N., Rudnick, D., Mourre, B., Garcia-Jove, M., Lermusiaux, P., and Tintoré, J.: Glider Survey reveals the evolution of the mesoscale and submesoscale structures in the Balearic Sea: Formation, Intensification, and Decay., EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-15714, https://doi.org/10.5194/egusphere-egu23-15714, 2023.

vCO.14
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EGU23-15973
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ECS
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Stamatios Petalas, Elina Tragou, Ioannis Mamoutos, and Vassilis Zervakis

Understanding the processes that control the buoyancy fluxes of the Aegean Sea is important for various reasons. First, the Aegean is directly connected with the Black Sea and acts as a buffer between two opposite thermohaline systems, a concentration and a dilution basin (the Mediterranean vs the Black Sea), receiving and filtering the variability and changes of a much broader geographical area. Second, the Aegean is capable to produce large amounts of very dense water, having temporarily been the major originator of Eastern Mediterranean Bottom Water. These processes are controlled by the buoyancy fluxes, both through oceanic advection and atmospheric exchanges. In this work we examine the characteristics and variability of heat, freshwater and the overall buoyancy air-sea fluxes, focusing on the potential role of the interaction with the Black Sea. A thirty-year-long simulation (1985-2015) of the whole Eastern Mediterranean/Black Sea system, forced by ERA-Interim data, was used to estimate and analyze the seasonal and interannual variability of the buoyancy fluxes in the North Aegean. The climatological mean buoyancy flux over the North Aegean has been estimated to be about –10×10–6 kg m–1 s–3 (loss to the atmosphere). However, in the absence of Black Sea Water (BSW) inflow, the buoyancy loss would correspond to the high values observed over the Eastern Aegean, an area not directly affected by the presence of the BSW, i.e. about –30 ×10–6 kg m–1 s–3. It should be noted that the heat loss of the Aegean Sea to the atmosphere is much higher than all neighboring seas, including the Adriatic, the dominant dense-water formation site for the Eastern Mediterranean. Our analysis reveals that the thin surface layer of modified BSW acts as a moderator of the buoyancy loss from the upper water column. This layer not only absorbs the air-sea fluxes (acting as an effective insulator regarding dense-water formation processes), but also moderates or even reverses the buoyancy fluxes over its path. Thus, in addition to the significant lateral buoyancy input to the basin by the Black Sea inflow, an additional mechanism of reduction of winter heat losses to the atmosphere contributes to the control of dense water formation processes.

How to cite: Petalas, S., Tragou, E., Mamoutos, I., and Zervakis, V.: On the role of Black Sea Waters in controlling the North Aegean buoyancy fluxes, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-15973, https://doi.org/10.5194/egusphere-egu23-15973, 2023.