Abstract
Evapotranspiration (ET) is the major component of the terrestrial water cycle. Information on ET will help monitor crop water requirement, crop phenology & production, and better irrigation water management. Despite its importance, ET’s near-real-time estimation at a varied spatial and temporal scale is not available. Different types of instruments are used to measure ET, which includes simple Lysimeter to more complex eddy covariance flux towers. However, for operational estimation of ET at a regional scale, methods like crop models or remote sensing-based techniques provide a reliable alternative. Estimation of ET using the remote sensing technique uses the various geophysical and biophysical parameters collected from the satellite platform. The satellite platform enables to estimate ET over a large area at a frequent time interval with reliable accuracy levels acceptable for several applications. This chapter discusses the different methods of deriving the ET and the justification for adopting the Priestley Taylor algorithm. It also describes the methodology of deriving the terrestrial ET in a near real-time basis and discusses the intra-seasonal dynamics and comparison with the field ET data.
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Acknowledgements
This work is carried out under National Hydrology Project at National Remote Sensing Centre, ISRO Hyderabad. The authors thank SAC-ISRO and IMD for providing data for the project. The authors thank Data Processing group and agriculture group of NRSC Hyderabad for providing data support for this project. The authors would like to thank Director NRSC for providing guidance and support.
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Chandrasekar, K. et al. (2022). Satellite-Based Terrestrial Evapotranspiration Product for India. In: Jha, C.S., Pandey, A., Chowdary, V., Singh, V. (eds) Geospatial Technologies for Resources Planning and Management. Water Science and Technology Library, vol 115. Springer, Cham. https://doi.org/10.1007/978-3-030-98981-1_17
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