Evapotranspiration Data Product from NESDIS GET-D System Upgraded for GOES-16 ABI Observations

dc.contributor.authorFang, Li
dc.contributor.authorZhan, Xiwu
dc.contributor.authorSchull, Mitchell
dc.contributor.authorKalluri, Satya
dc.contributor.authorLaszlo, Istvan
dc.contributor.authorYu, Peng
dc.contributor.authorCarter, Corinne
dc.contributor.authorHain, Christopher
dc.contributor.authorAnderson, Martha
dc.date.accessioned2023-11-13T19:32:55Z
dc.date.available2023-11-13T19:32:55Z
dc.date.issued2019-11-12
dc.description.abstractEvapotranspiration (ET) is a major component of the global and regional water cycle. An operational Geostationary Operational Environmental Satellite (GOES) ET and Drought (GET-D) product system has been developed by the National Environmental Satellite, Data and Information Service (NESDIS) in the National Oceanic and Atmospheric Administration (NOAA) for numerical weather prediction model validation, data assimilation, and drought monitoring. GET-D system was generating ET and Evaporative Stress Index (ESI) maps at 8 km spatial resolution using thermal observations of the Imagers on GOES-13 and GOES-15 before the primary operational GOES satellites transitioned to GOES-16 and GOES-17 with the Advanced Baseline Imagers (ABI). In this study, the GET-D product system is upgraded to ingest the thermal observations of ABI with the best spatial resolution of 2 km. The core of the GET-D system is the Atmosphere-Land Exchange Inversion (ALEXI) model, which exploits the mid-morning rise in the land surface temperature to deduce the land surface fluxes including ET. Satellite-based land surface temperature and solar insolation retrievals from ABI and meteorological forcing from NOAA NCEP Climate Forecast System (CFS) are the major inputs to the GET-D system. Ancillary data required in GET-D include land cover map, leaf area index, albedo and cloud mask. This paper presents preliminary results of ET from the upgraded GET-D system after a brief introduction of the ALEXI model and the architecture of GET-D system. Comparisons with in situ ET measurements showed that the accuracy of the GOES-16 ABI based ET is similar to the results from the legacy GET-D ET based on GOES-13/15 Imager data. The agreement with the in situ measurements is satisfactory with a correlation of 0.914 averaged from three Mead sites. Further evaluation of the ABI-based ET product, upgrade efforts of the GET-D system for ESI products, and conclusions for the ABI-based GET-D products are discussed.
dc.description.urihttps://doi.org/10.3390/rs11222639
dc.identifierhttps://doi.org/10.13016/dspace/za71-jh8h
dc.identifier.citationFang, L.; Zhan, X.; Schull, M.; Kalluri, S.; Laszlo, I.; Yu, P.; Carter, C.; Hain, C.; Anderson, M. Evapotranspiration Data Product from NESDIS GET-D System Upgraded for GOES-16 ABI Observations. Remote Sens. 2019, 11, 2639.
dc.identifier.urihttp://hdl.handle.net/1903/31376
dc.language.isoen_US
dc.publisherMDPI
dc.relation.isAvailableAtCollege of Computer, Mathematical & Natural Sciencesen_us
dc.relation.isAvailableAtGeologyen_us
dc.relation.isAvailableAtDigital Repository at the University of Marylanden_us
dc.relation.isAvailableAtUniversity of Maryland (College Park, MD)en_us
dc.subjectevapotranspiration (ET)
dc.subjectGOES-R
dc.subjectGET-D
dc.subjectdrought monitoring
dc.titleEvapotranspiration Data Product from NESDIS GET-D System Upgraded for GOES-16 ABI Observations
dc.typeArticle
local.equitableAccessSubmissionNo

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