S3

Change in extreme droughts in the future

Drought is an extreme which has always drawn attention of the hydrological science community. It has been so more these days as too little water is not an avoidable case anymore with the change in hydrology, which can be either natural or because of human activities. Regardless of the nature of the change, we now face more frequent and more severe droughts for which actions are needed to be taken in advance for the sustainability of water-dependent sectors; irrigation, energy, industry, tourism, ecology, etc. Consequently, the economy is affected by the drought. An awareness is clearly needed to cope with the consequences of drought, and to be able to anticipate major drought spells. For this aim, people could be encouraged to include the concepts of water scarcity, water conservation and drought prevention in their everyday life. Also, it is expected that these concepts are considered in water resources management and planning. Legislative background is needed for the future water scarcity and drought management. Innovative and novel tools, methods and techniques are expected for the future to understand the drought process, make research and practice. They are also needed for promoting water savings, using alternative resources, encouraging the use of renewable sources; and discussing the environmental, economic and social impacts of water scarcity and drought. Studies touching upon all above concepts and issues are welcome to this session. Particularly welcome are studies showing experiences of how research directions can be driven from users and professional needs and requirements.

Convener: Gil Mahé | Co-Conveners: David Hannah, Yonca Cavus, Ebru Eris, MEDDI Mohamed
Orals
| Wed, 01 Jun, 10:30–15:00|Room Auditorium Pasteur
Posters
| Attendance Wed, 01 Jun, 15:00–16:30|Poster area

Orals: Wed, 01 Jun | Room Auditorium Pasteur

Chairpersons: Gil Mahé, Ebru Eris
Drought Characterisation
10:30–10:45
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IAHS2022-372
Christina Anna Orieschnig and Yonca Cavus

Drought is a natural hazard which occurs in all climatic zones and affects different sectors such as irrigation, energy, water supply, and ecology. Monitoring and predicting drought are pressing challenges since drought is becoming more common and severe owing to the impacts of climate change and increased climatic variability. However, in many areas of the globe, the temporal and spatial characterization of droughts and trends in their frequency and severity is hindered by a lack of reliable, long-term locally measured data and unevenly distributed, erratic meteorological stations. In this situation, remote sensing datasets such as Climate Hazards Group InfraRed Precipitation with Station Data (CHIRPS) can offer valuable insights into long-term developments and the spatial characteristics of droughts. Nonetheless, it is often uncertain to which extent data such as CHIRPS succeeds in representing local dynamics and how this varies between geographical regions and climate zones. 

In this analysis, we aim to evaluate spatial drought conditions over the Seyhan River basin in Turkey in the Eastern Mediterranean. Using the Standardized Precipitation Index (SPI) as a drought index, the applicability of CHIRPS as a long-term satellite precipitation product for drought monitoring is investigated. We compare two spatial representations of the SPI: one derived on a per-pixel basis from CHIRPS data since 1981, the other based on data from 19 meteorological stations scattered across the basin which was spatialized using inverse distance weighted interpolation. Our results offer insights into the relative accuracy of CHIRPS data in the Eastern Mediterranean, and avenues towards optimizing the quality of spatial drought characterization approaches. 

How to cite: Orieschnig, C. A. and Cavus, Y.: Spatial characterization of drought through CHIRPS and a station-based dataset in the Eastern Mediterranean , IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-372, 2022.

10:45–11:00
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IAHS2022-77
Future Changes in Drought Characteristics under Extreme Climate Change over Oti Riverbasin in Togo (West-Africa)
(withdrawn)
Lamboni Batablinlè and Lawin Agnidé
11:00–11:15
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IAHS2022-276
Yonca Cavus, Hafzullah Aksoy, and Kerstin Stahl

Seyhan River Basin has great importance for agricultural production, industry, energy and tourism sectors in Turkey. This study investigates temporal characteristics of meteorological droughts in the river basin at station-scale. Six major droughts were identified lasting 2 years at minimum from the average precipitation time series of 19 meteorological stations over the basin. We have adopted a methodology specifically for the river basin where local meteorological data are limited. The river basin was divided into four sub-basins. Each sub-basin was represented by one meteorological station which has a high correlation with the basin-average precipitation and also covers as many of the major droughts as possible. The Standardized Precipitation Index (SPI) was calculated for the meteorological stations at different time scales. The site-specific drought analysis elucidated the probability of mild, moderate, severe, and extreme droughts. The temporal occurrence illustrates that the river basin has experienced severe prolonged droughts every ten years on average. Mild drought dominates at each time scale and their frequencies increase with increasing time scale although severe and extreme events are observed with a higher probability in some major droughts. A significant change of the probabilities of the drought classes was not found in the representative stations, instead, we observed no consistent change. This analysis presented valuable information for the river basin on the temporal variability of the drought, and also shed light on the need for such analyses for regional drought adaptation and mitigation. Given the limitations that emerged on the determination of the representative stations, it would be advisable to consider additional data (such as remote sensing or satellite) in future studies to gain further insights into the temporal characteristics of drought.

How to cite: Cavus, Y., Aksoy, H., and Stahl, K.: Characterizing major droughts in the context of dry period in Seyhan River basin, Turkey, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-276, 2022.

11:15–11:30
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IAHS2022-133
Multivariate analysis of meteorological drought in northern Algeria 
(withdrawn)
Faiza Hallouz and Mohamed Meddi
11:30–11:45
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IAHS2022-176
Pilabina Somiyabalo, Yabi Ibouraïma, and Amoussou Ernest

Drought is an insidious scourge that results from a decline in precipitation from levels considered normal. The data used cover a period of 118 years (1901-2019) which ensures a good coverage of the studied region. Two approaches (SPI and SPEI) were applied to assess drought in the Volta bassin in Togo. The results show that there has been a decrease in rainfall in the Volta bassin in Togo in recent years. In terms of SPI, 36 years have indices lower than -0.5 and 4 years lower than -1 in the Dapaong station. The longest periods of drought are observed between 1958-1990 or 33 years and 2010-2019 or 10 years. The SPEI show 9 years with an index lower than -0.5 and only one year (2001) with an index lower than -1. The longest droughts occurred during the period 2009-2019, or 10 years, as for the IPS. This shows a trend of aridification of the climate in this area.

How to cite: Somiyabalo, P., Ibouraïma, Y., and Ernest, A.: Modelling of meteorological drought using the SPI and SPEI indices in the Volta watershed in Togo, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-176, 2022.

11:45–12:00
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IAHS2022-744
Akinwale Ogunrinde, Phillip G. Oguntunde, Akinola S. Akinwumiju, and Johnson T. Fasinmirin

The impact of climate change on drought phenomenon in Nigeria which is one of the major countries in West Africa cannot be over emphasized since the commencement of decreasing rains in the early 1980s. Hence, this work aims at evaluating some of the drought characteristics over all the agroecological zones in Nigeria, and project the influence of future climate change on drought. Historical observatory and future simulated datasets based on representative concentration pathway (RCP) 8.5 scenario covering from 1981 – 2100 were analysed. Three well accepted drought indices; the standardized precipitation index (SPI), reconnaissance drought index (RDI) and standardized precipitation and evapotranspiration index (SPEI) were utilized in drought characterization. Implications from the study reveal that the historical drought pattern of drought is similar to the earlier studies conducted across agroecological zones in Nigeria. The ensemble of the seven (7) GCMs using RCA-4 captured some pragmatic features of the climatology of Nigeria in the historical period. On a general note, there is a projection of an increase in both the frequency and intensity of drought over all the agroecological zones in Nigeria. Considering the output of drought characteristics as measured by SPI, future climates were predicted to be more wet when compared to historical period in the study period. In contrast, SPEI and RDI forecasted dryer climates. The prediction of SPEI and RDI must have been predicated on the influence of increasing temperature due to global warming as captured by RCP 8.5, which would in turn affect the rate of evapotranspiration. In view of drought analysis using the RCP 8.5 scenario, the frequency of severe/extreme drought will likely become more intense due to increasing temperature levels. The changes in the SPEI drought frequency range from 2.2 (2031–2060) to 3.4 (2071–2100) month/year while RDI ranges from 1.5 (2031–2060) to 2.5 (2081–2100) month/year. Sahel and Sudan savannah agroecological zones are likely to be more impacted in the future than other zones which may not be significantly affected. Implications from this study may assist in developing drought mitigation preparedness plans and strategies for minimizing climate change impacts.

How to cite: Ogunrinde, A., Oguntunde, P. G., Akinwumiju, A. S., and Fasinmirin, J. T.: Evaluation of some Meteorological Drought Indices in Nigeria using RCP 8.5 Climate Scenario, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-744, 2022.

Lunch Break // W4F Hackathon High Schools Final
Chairpersons: David Hannah, MEDDI Mohamed
Drought related issues
13:30–13:45
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IAHS2022-192
Domiho Japhet Kodja, Houteta Djan’na Koubodana, Gandome Mayeul L. D Quenum, Ernest Amoussou, Arsène Sègla Josué Akognongbé, Gil Mahé, Jean-Emmanuel Paturel, Expédit Wilfrid Vissin, and Constant Houndénou

This study aims to investigate drought and flooding area in West Africa during the pre-industrial and projected future periods. The datasets used consist of CHIRPS-2 and CRU for observed reanalysis and CORDEX/CMIP6 for climate model scenarios. The CORDEX/ CMIP6’s potential evapotranspiration (PET) and precipitation correlate well with observation dataset over the study area with respective KGE up to 0.75 and 0.9. The pre-industrial period used in this research covers 1971-2000, while the projection period is defined according to the global warming level and the RCPs. Results showed that, the spatial and temporal repartition of SPEIs was elucidated by applying the Empirical Orthogonal Function (EOF) analysis, which showed that during the pre-industrial period, the wettest areas were located at the eastern and southern part of West Africa. The analyses on projected scenarios reveals that most of the coastal countries in Gulf of Guinea will be globally wetter under all the GWLs studied, with some interleaving as coastal countries (Senegal, Ivory-Coast, Benin, Togo and Nigeria). Some years will experiment extreme drought, whilst Savanna will get positive changes, which will lead them to become less dry compare to period 1971-2000. An investigation on the spatial concentration of precipitation using precipitation concentration index (PCI), have involved this study to highline an uniform spatial distribution of annual and wet season precipitations over gulf of Guinea and Savanna, follow by an increasing of uniform and moderate spatial distribution of precipitation under RCP4.5, and negative changes over eastern and western part of the study area for projection RCP8.5, explaining the high variability of concentration of precipitation over these regions.

Keywords: Drought and flood area, climate model, West Africa, global warming

How to cite: Kodja, D. J., Koubodana, H. D., Quenum, G. M. L. D., Amoussou, E., Akognongbé, A. S. J., Mahé, G., Paturel, J.-E., Vissin, E. W., and Houndénou, C.: Investigation of drought and flooding areas in coastal countries of West Africa in the context of global warming, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-192, 2022.

13:45–14:00
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IAHS2022-67
Fares Al Hasan, Ruud van der Ent, and Andreas Link

The 2018 summer drought in Europe was particularly extreme in terms of intensity and impact due to the combination of low rainfall and high temperatures. However, it remains unclear how this drought developed in time and space in such an extreme way. In this study we aimed to get a better understanding of the role of land-atmosphere interactions. More specifically, we investigated whether there was a change in water vapor originating from land, if that caused a reduction in rainfall, and by this mechanism possibly the propagation and intensification of the drought in Europe. We used a global gridded dataset of the fate of land evaporation (i.e., where it ends up as precipitation) to investigate whether the drought intensification and propagation was impacted by the reduction in water vapor transported from the regions that first experienced the drought. It was found that during the onset phase of the 2018 drought in Europe that the water vapor originating from land played an important role in mitigating the precipitation anomalies as, for example, the share of land evaporation contributing to precipitation increased from 27% (normal years) to 38% (2018) during July in West of Europe. Land evaporation played a minor role in amplifying it during the intensification phase of the drought as the share of land evaporation contribution to precipitation decreased from 23% (normal years) to 21% (2018) during August in West of Europe. These findings are somewhat in contrast to similar studies in other continents that found the land surface to play a strong amplifying role for drought development. These results were recently published here: https://doi.org/10.3390/w13202856. Speculating what this case study means for future extreme droughts in Europe, we can at least conclude that for West of Europe the positive feedback loop between drought, soil moisture, vegetation, evaporation and precipitation is still weak even under extreme circumstances, and that probably quite a severe climate changes scenario would be needed to change this.

How to cite: Al Hasan, F., van der Ent, R., and Link, A.: The Effect of Water Vapor Originating from Land on the 2018 Drought Development in Europe, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-67, 2022.

14:00–14:15
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IAHS2022-280
Climate change will increase the severity and duration of soil water stress in temperate forests of eastern North America
(withdrawn)
Audrey Maheu, Cybèle Cholet, Daniel Houle, Jean-Daniel Sylvain, and Frédérik Doyon
14:15–14:30
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IAHS2022-352
Frederiek Sperna Weiland, Robrecht Visser, Peter Greve, Berny Bisselink, Lukas Brunner, and Albrecht Weerts

Climate change will influence the severity and intensity of floods and droughts throughout Europe. Ensemble projections of future changes in discharge show large variation. Several methods for performance-based weighting exist that have the potential to increase the robustness of the change signal. Here we use future projections of an ensemble of three hydrological models forced with climate datasets from the Coordinated Downscaling Experiment - European Domain (EURO-CORDEX). The experiment is set-up for nine river basins spread over Europe that hold different climate and catchment characteristics. We evaluate the ensemble consistency and apply two weighting approaches; (1) the Climate model Weighting by Independence and Performance (ClimWIP) that focuses on meteorological variables and (2) the Reliability Ensemble Averaging (REA) that is in our study applied to discharge statistics per basin. For droughts we focus on the change in discharge during low flow periods of 7-days.

For basins with a strong climate signal, in Southern and Northern Europe, the consistency in the set of projections is large. For rivers in Central Europe the differences between models become more pronounced. Both weighting methods favor projections from similar GCMs and assign high weights to a single or few best performing GCMs. The ClimWIP method results in ensemble mean weighted changes that differ only slightly from the non-weighted mean. The REA method influences the weighted mean more. The weights assigned to the CORDEX model simulations based on basin specific discharges highly vary from basin to basin.

How to cite: Sperna Weiland, F., Visser, R., Greve, P., Bisselink, B., Brunner, L., and Weerts, A.: Performance-based weighting of CORDEX projections of hydrological climate change impacts over Europe, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-352, 2022.

14:30–14:45
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IAHS2022-674
Lucy Barker, Nathan Rickards, Sunita Sarkar, Jamie Hannaford, Eugene Magee, and Gwyn Rees

Droughts are known to be one of the most damaging and costly natural hazards as a result of their large spatial scale, creeping nature and long duration. They have widespread primary and secondary impacts, and as such, proactive drought management is crucial to mitigate those impacts. In order to do so, it is crucial to understand the drought risk – i.e. the characteristics of the drought hazard, who or what is exposed to the drought hazard, and who (or what) is vulnerable to the effects of drought. Drought mitigation is one of five strategic objectives under the United Nations Convention to Combat Desertification (UNCCD) 2018-2030 Strategic Framework, under which a monitoring framework and a range of indicators was agreed by country Parties to the UNCCD.

Here we present new guidance created to help Parties to the UNCCD report on their progress towards Strategic Objective 3 ‘To mitigate, adapt to, and manage the effects of drought in order to enhance resilience of vulnerable populations and ecosystems’. Progress is monitored using three indicators, capturing the three fundamental components of risk: drought hazard, exposure to drought and vulnerability to drought. The three indicators, as agreed by Parties to the UNCCD, are:

  • Trends in the proportion of land under drought over the total land area,
  • Trends in the proportion of the total population exposed to drought, and
  • Trends in the degree of drought vulnerability.

Acknowledging the need for global applicability, the methods recommended to calculate these three indicators balance state-of-the-art science with relative simplicity, whilst also meeting the requirements set out in official UNCCD Decisions, guidelines of the World Meteorological Organization, and where possible utilising datasets used for other reporting activities (e.g. the Sustainable Development Goals). The methods for each indicator are illustrated using contrasting case studies, highlighting the flexibility of the approaches recommended, as well as opportunities for the future of national reporting on drought risk.

How to cite: Barker, L., Rickards, N., Sarkar, S., Hannaford, J., Magee, E., and Rees, G.: Assessing drought risk to track progress in drought adaptation, mitigation and management at the global scale, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-674, 2022.

14:45–15:00
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IAHS2022-147
Denis Hughes

The city of Grahamstown in the Eastern Cape Province of South Africa has been experiencing an extended period of below average rainfall for more than 7 years. The public perception of this drought is that it could be a consequence of climate change and represents the new ‘normal’ for this area. This study looks at this drought in the context of daily rainfall records extending back to the start of the 20th century. The rainfall data are analysed in several ways to determine if this drought is really exceptional and to try and identify any unique characteristics of the recent drought period. The analyses are all relatively simple non-statistical methods, largely because statistical trend tests are considered by the author to frequently suggest results that are more artifacts of the data analysis methods than real, particularly in data sets that show cyclical trends (frequently shown to be one of the key characteristics of South African rainfall data).  

A relatively simple analysis using the cumulative departure of monthly rainfall totals from the calendar month means shows a systematic downward slope since 2014 (Figure 1). However, there was a similar general downward trend between 1940 and 1960, as well as between 1980 and 1990, suggesting that, from this perspective, the current period is not exceptional. A comparative analysis using a similarly long rainfall record for a farm located in a drier area, but only 20 km from the city, shows a relatively different pattern of historical rainfall variations.

Other types of analysis using different rainfall characteristics show different things. The rainfall data for over 120 years are also used to force a hydrological model to generate simulated streamflow, groundwater recharge and soil moisture storage to further investigate the drought characteristics from a broader perspective than simply the rainfall data themselves. The rainfall data are also used to simulate the performance of a domestic rainwater storage tank to investigate the feasibility of using household level interventions to mitigate against deficiencies in the municipal water supply.    

How to cite: Hughes, D.: Anatomy of an extended drought in part of the Eastern Cape Province, South Africa, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-147, 2022.

Posters: Wed, 1 Jun, 15:00–16:30 | Poster area

Chairpersons: Yonca Cavus, MEDDI Mohamed
P1
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IAHS2022-327
Sabyasachi Swain, Surendra Mishra, and Ashish Pandey

Drought is one of the most precarious phenomena associated with serious repercussions, especially over the agriculture-dominated regions. This study presents an investigation of drought characteristics over the Marathwada Region, Maharashtra, India, which is infamous for a large number of farmer suicides. The monthly rainfall data for 1951-2020 is collected from Indian Meteorological Department (IMD). Two widely used drought indices, viz., Standardized Precipitation Index (SPI) and Effective Drought Index (EDI) are employed to characterize the drought events. Moreover, droughts under future climate i.e., from 2021 to 2090, are investigated using an ensemble of different CMIP5 models for the Representative Concentration Pathways (RCPs) 4.5 and 8.5. The results revealed the Marathwada Region to be prone to droughts due to a remarkable inter-annual variability in rainfall. The droughts are predicted to become more severe, frequent, and persistent in the future. From the comparative assessment of two indices, EDI is found to be superior in capturing the onset of the droughts and hence, can be handy in drought monitoring purposes. Since Marathwada Region has a monsoon-dominated climate with high agricultural importance, the information reported in this study will help devise water management strategies to minimize the repercussions of droughts. Besides, the methodology presented will encourage its replication over different regions of the world that have been affected by climate change and its ramifications, mostly in the form of frequent droughts or lower crop yields.

How to cite: Swain, S., Mishra, S., and Pandey, A.: Evaluation of Meteorological Drought Characteristics under Climate Change over the Agriculture-dominated Marathwada Region, India, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-327, 2022.

P2
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IAHS2022-342
Akif Rahim, Yannis Markonis, and Rajani Kumar Pradhan

Flash drought is a unique natural hazard due to its rapid rate of intensification. The rapid development of flash drought has made it different from the traditional drought. In this study we examined the characteristics (Frequency, Rate of intensification, Severity, and Extent) of flash drought events in the Central Europe between 1970 and 2020. The weekly averaged topsoil moisture (SM) data set of the Global Land Data Assimilation System (GLDAS) has been used as an indicator for identifying flash drought events. The result of the study shows that the relative frequency across the central Europe varies from 0.06 to 0.47 and the western and southeast part of the central Europe received high number of flash drought events since 1970. The total severity of the flash drought varies from 0.15to 1.84 whereas the average rate of intensification varies from 0.05 to 0.12 percentile per week. The severity of the drought was found to increase during the beginning of the growing season, then decreased during the last part of the growing season. The areal extend of flash drought observed increasing after 1988 from 22% to 34% of the Central Europe. Analysis of the study has shown that the decreasing conditions of soil moisture in the region increased the risk of flash drought.

How to cite: Rahim, A., Markonis, Y., and Pradhan, R. K.: Investigation of Flash Drought Characteristics Across The Central Europe, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-342, 2022.

P3
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IAHS2022-350
A time-varying drought identification and frequency analyzation method: A  case study of Jinsha River Basin
(withdrawn)
Xiaopei Ju, Yuankun Wang, Dong Wang, and Pengcheng Xu
P4
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IAHS2022-586
Haifa Feki and Christophe Cudennec

Tunisia is a coastal region of the Mediterranean Sea in North Africa with an area of ​​164,150 km2. The physical geography of the region is very heterogeneous with mountains to the north and the Sahara to the south. It is located in the transition zone between the humid Mediterranean climate and the arid Saharan climate. Precipitation is characterized by a large North-South spatial distribution varying between 1400 mm/year in the North to less than 40 mm/year to the South.

Thanks to the consolidation of a quality, long-term, synoptic database over the whole country, the average monthly rainfall was mapped by comparing the beginning and the end of the 20th century to look for a possible change in the spatial distribution of rain across Tunisia. We found a slight change in the spatial distribution of rainfall by comparing average monthly rainfall in the early to late twentieth century. A slight change in the direction of the rainfall gradient is perceptible during transition seasons with a speed of change in spatial structure that is more important at the end of the twentieth century for the fall season. This change may intensify as a result of the impacts of climate change and subsequently have an effect on socio-economic aspects. On the other hand, the phenomenon of meteorological drought continues to migrate towards the North and it appears that the stations with significant tendencies towards the increase of drought are located mainly in the regions of North / North-West of the country.

How to cite: Feki, H. and Cudennec, C.: Rainfall and drought: Changes in the synoptic distribution over semi-arid Tunisia, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-586, 2022.

P5
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IAHS2022-623
Hajar El Khalfi, Claire Delus, Gilles Drogue, Sébastien Lebaut, Luc Manceau, and Didier François

The aim of this communication is to present the state-of-the-art on low flows trends and modelling in the French part of the Mosel basin (~10800 km²) over the last decades. The state-of-the art is feed by the two following complementary projects that focus on (i) characterization and (ii) forecasting of low flows:

  • MAJORE is a project supported by the Rhine-Meuse Water Agency which studies low flow characteristics in a context of non-stationary flows. The issue focuses on the detection of the reference period for calculating low flow characteristics as well as to understand and explain why some basins are more affected by droughts than others over the two last decades.
  • The CIPRHES[1] project is a French national research project which aims to provide solutions to water resources managers by proposing low flow forecasts. For that purpose we developed a new semi-distributed version of our hydrological model that integrate the main anthropic influences in the basin (drinking water supply, dams, canals ...). Results obtained on the Meurthe basin which benefits from a low water support through the Vieux Pré dam are compared to those obtained from the upstream Mosel basin which is not influenced by a regulating reservoir.

[1] https://www6.inrae.fr/ciprhes/Le-projet/Defis-cles

How to cite: El Khalfi, H., Delus, C., Drogue, G., Lebaut, S., Manceau, L., and François, D.: Low flow characterization and forecasting in a non-stationary context, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-623, 2022.

P6
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IAHS2022-665
Charles Perrin and the CIPRHES Team

There has been a growing interest in extending forecast lead times to facilitate water resources planning and management during droughts and low-flow events. This can be partly achieved by improving integrated hydrometeorological forecasting systems, which offer forecasts of future meteorological and hydrological conditions over continuous space and time scales. Several initiatives have been recently carried out at continental or global scales, in Europe and worldwide, to set up forecasting chains that run with numerical weather and climate model predictions as input to distributed hydrological models. Overall, these systems have been developed in response to a call for seamless forecasts in time (from short to medium and long-ranges) and space (at well-monitored and partially-monitored or ungauged catchments). These systems usually have to deal with limited calibration and evaluation against local data.

In France, the CIPRHES project (2021-2025) aims at building an efficient and integrated methodology and an online operational service for a country-wide hydrological drought and low-flow forecasting system, based on the proof-of-concept PREMHYCE platform. The first step focuses on producing seamless atmospheric forecasts, combining information from climatology, weather predictions and seasonal forecasts. Then forecasts are post-processed and tailored for hydrological purposes of drought and low-flow forecasting.

The first outcomes of the project will be presented, towards providing short- to long-term seamless hydrological forecasts. The outputs of a workshop organized with end-users to improve a forecasting prototype will be discussed.

The CIPRHES project is funded by the French National Research Agency (grant ANR-20-CE04-0009-03).

How to cite: Perrin, C. and the CIPRHES Team: Integrated chain for the hydrometeorological forecasting of low flows and droughts in France. The CIPRHES project, IAHS-AISH Scientific Assembly 2022, Montpellier, France, 29 May–3 Jun 2022, IAHS2022-665, 2022.