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Hydrol. Earth Syst. Sci., 22, 1351-1369, 2018
https://doi.org/10.5194/hess-22-1351-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 3.0 License. 
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Research article
23 Feb 2018
1Hydrological Sciences Lab, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
2Earth Science Office, NASA Marshall Space Flight Center, Huntsville, AL, USA
3Hydrology and Remote Sensing Laboratory, USDA ARS, Beltsville, MD 20705, USA
Received: 19 May 2017 – Discussion started: 06 Jun 2017
Revised: 22 Dec 2017 – Accepted: 08 Jan 2018 – Published: 23 Feb 2018
Abstract. A newly developed microwave (MW) land surface temperature (LST) product is used to substitute thermal infrared (TIR)-based LST in the Atmosphere–Land Exchange Inverse (ALEXI) modeling framework for estimating evapotranspiration (ET) from space. ALEXI implements a two-source energy balance (TSEB) land surface scheme in a time-differential approach, designed to minimize sensitivity to absolute biases in input records of LST through the analysis of the rate of temperature change in the morning. Thermal infrared retrievals of the diurnal LST curve, traditionally from geostationary platforms, are hindered by cloud cover, reducing model coverage on any given day. This study tests the utility of diurnal temperature information retrieved from a constellation of satellites with microwave radiometers that together provide six to eight observations of Ka-band brightness temperature per location per day. This represents the first ever attempt at a global implementation of ALEXI with MW-based LST and is intended as the first step towards providing all-weather capability to the ALEXI framework.
The analysis is based on 9-year-long, global records of ALEXI ET generated using both MW- and TIR-based diurnal LST information as input. In this study, the MW-LST (MW-based LST) sampling is restricted to the same clear-sky days as in the IR-based implementation to be able to analyze the impact of changing the LST dataset separately from the impact of sampling all-sky conditions. The results show that long-term bulk ET estimates from both LST sources agree well, with a spatial correlation of 92 % for total ET in the Europe–Africa domain and agreement in seasonal (3-month) totals of 83–97 % depending on the time of year. Most importantly, the ALEXI-MW (MW-based ALEXI) also matches ALEXI-IR (IR-based ALEXI) very closely in terms of 3-month inter-annual anomalies, demonstrating its ability to capture the development and extent of drought conditions. Weekly ET output from the two parallel ALEXI implementations is further compared to a common ground measured reference provided by the Fluxnet consortium. Overall, the two model implementations generate similar performance metrics (correlation and RMSE) for all but the most challenging sites in terms of spatial heterogeneity and level of aridity. It is concluded that a constellation of MW satellites can effectively be used to provide LST for estimating ET through ALEXI, which is an important step towards all-sky satellite-based retrieval of ET using an energy balance framework.
Citation: Holmes, T. R. H., Hain, C. R., Crow, W. T., Anderson, M. C., and Kustas, W. P.: Microwave implementation of two-source energy balance approach for estimating evapotranspiration, Hydrol. Earth Syst. Sci., 22, 1351-1369, https://doi.org/10.5194/hess-22-1351-2018, 2018.
2Earth Science Office, NASA Marshall Space Flight Center, Huntsville, AL, USA
3Hydrology and Remote Sensing Laboratory, USDA ARS, Beltsville, MD 20705, USA
The analysis is based on 9-year-long, global records of ALEXI ET generated using both MW- and TIR-based diurnal LST information as input. In this study, the MW-LST (MW-based LST) sampling is restricted to the same clear-sky days as in the IR-based implementation to be able to analyze the impact of changing the LST dataset separately from the impact of sampling all-sky conditions. The results show that long-term bulk ET estimates from both LST sources agree well, with a spatial correlation of 92 % for total ET in the Europe–Africa domain and agreement in seasonal (3-month) totals of 83–97 % depending on the time of year. Most importantly, the ALEXI-MW (MW-based ALEXI) also matches ALEXI-IR (IR-based ALEXI) very closely in terms of 3-month inter-annual anomalies, demonstrating its ability to capture the development and extent of drought conditions. Weekly ET output from the two parallel ALEXI implementations is further compared to a common ground measured reference provided by the Fluxnet consortium. Overall, the two model implementations generate similar performance metrics (correlation and RMSE) for all but the most challenging sites in terms of spatial heterogeneity and level of aridity. It is concluded that a constellation of MW satellites can effectively be used to provide LST for estimating ET through ALEXI, which is an important step towards all-sky satellite-based retrieval of ET using an energy balance framework.
Citation: Holmes, T. R. H., Hain, C. R., Crow, W. T., Anderson, M. C., and Kustas, W. P.: Microwave implementation of two-source energy balance approach for estimating evapotranspiration, Hydrol. Earth Syst. Sci., 22, 1351-1369, https://doi.org/10.5194/hess-22-1351-2018, 2018.
