EGU23-6897, updated on 10 Apr 2024
https://doi.org/10.5194/egusphere-egu23-6897
EGU General Assembly 2023
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Satellite Remote Sensing and Hydrological Modeling for Estimating Daily Actual Evapotranspiration in a Semi-Arid Mediterranean Ecosystem

Hassan Awada1,5, Mirko Castellini2, Simone Di Prima1, Filippo Giadrossich1, Costantino Sirca1,3,4, Serena Marras1,3,4, Donatella Spano1,3,4, and Mario Pirastru1,4,5
Hassan Awada et al.
  • 1University of SASSARI, Department of Agricultural Sciences, Italy (hawada@uniss.it)
  • 2Council for Agricultural Research and Economics-Agriculture and Environment Research Center (CREA-AA), Via Celso Ulpiani 5, 70125 Bari, Italy
  • 3Euro-Mediterranean Centre on Climate Change (CMCC) Foundation, Via de Nicola 9, 07100, Sassari, Italy.
  • 4National Biodiversity Future Center (NBFC), Palermo 90133, Italy
  • 5Desertification Research Group, NRD, University of Sassari, Viale Italia 57, 07100 Sassari, Italy

Evapotranspiration (ET) is the process by which water is lost from the Earth's surface through the combined mechanisms of evaporation from surfaces and transpiration from plants. It is an important factor in the soil-plant-atmosphere (SPA) system and plays a key role in the functioning of ecosystems. In semi-arid regions such as the Mediterranean, ET is a major contributor to water loss. An accurate understanding of the spatiotemporal dynamics of ET is crucial for effective water resource management and conservation, particularly in the face of increasing water resource pressure and potential climate change. Remote sensing (RS) can provide long-term data with relatively high spatial and temporal resolution, which can be valuable for sustainable ecosystem management. Surface energy balance (SEB) techniques based on satellite RS data have proven useful for quantifying actual evapotranspiration (ETa eb) at various temporal and spatial scales. However, limitations such as the temporal resolution of satellite data and gaps in image acquisition due to cloud cover can limit the usefulness of RS. This study proposes a model-based approach for constructing daily crop actual evapotranspiration (ETc act) between Landsat 8 acquisition days. The modeling approach aims to simulate the dynamics in the SPA system that occur between two Landsat acquisitions in order to estimate the daily time series of ETc act. The model integrates ETa eb estimates by SEBAL model on Landsat-8 acquisition days, RS-derived vegetative biomass dynamics, field measurements of potential evapotranspiration, and a hydrological modeling approach using the transient flow Richards equation to estimate soil moisture in the root zone. The results show that the proposed approach is well suited for modeling the dynamics in the soil-plant-atmosphere system that occurs between two Landsat acquisitions to estimate the daily time series of ETc act. This approach can provide valuable information for water resource management, drought monitoring, and climate change research, moreover accurate ETc act estimates can make significant contributions to near real time irrigation modeling and scheduling.

How to cite: Awada, H., Castellini, M., Di Prima, S., Giadrossich, F., Sirca, C., Marras, S., Spano, D., and Pirastru, M.: Satellite Remote Sensing and Hydrological Modeling for Estimating Daily Actual Evapotranspiration in a Semi-Arid Mediterranean Ecosystem, EGU General Assembly 2023, Vienna, Austria, 23–28 Apr 2023, EGU23-6897, https://doi.org/10.5194/egusphere-egu23-6897, 2023.