3.8 Article

Evapotranspiration and Vegetation Cover Classifications Maps Based on Cloud Computing at the Arab Countries Scale

Journal

EARTH SYSTEMS AND ENVIRONMENT
Volume 6, Issue 4, Pages 837-849

Publisher

SPRINGER INT PUBL AG
DOI: 10.1007/s41748-022-00320-2

Keywords

Reference evapotranspiration (ETo); Potential crop evapotranspiration (ETc); Vegetation cover density; Google Earth Engine (GEE); SARE model

Funding

  1. Science, Technology & Innovation Funding Authority (STDF)
  2. Egyptian Knowledge Bank (EKB)

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This study utilized remote sensing and meteorological data to create climate categories and crop vegetation coverage maps for Arab countries, while validating the reliability of the model.
According to the most recent Koppen-Geiger classification, Arab countries are divided into seven climate classes. Ground data availability is limited in developing countries, and ground meteorological data are scarce and concentrated in a few locations, rather than station maintenance capability being adequate for the responsibilities. The current study uses remote sensing and meteorological data to create regional classification maps of reference evapotranspiration (ETo), potential crop evapotranspiration, and vegetation cover in Arab countries from 2005 to 2020. The Stand-alone Remote Sensing Approach to Estimate Reference Evapotranspiration (SARE) was used to estimate ETo using satellite data from 2005 to 2020. The Land Surface Temperature (LST) and Normalized Difference Vegetation Index (NDVI) were extracted from MODIS satellite data and used in the SARE model, in addition to elevation (E), Julian day (J), and Latitude (Lat). To validate the SARE model results, the FAO-Penman-Monteith model was applied to 35 ground meteorological stations distributed across Arab countries to cover all climate classes based on the most recent Koppen-Geiger climate classification. Google Earth Engine was used to create the classification. The statistical indices produced acceptable results, with average RMSE values ranging from 6.9 to 17.3 (mm/month), while correlation coefficient (r) and index of agreement (d) values are more significant than 0.9. To be included in the ETc calculation, the crop coefficient (K-c) was calculated using NDVI 250 m spatial resolution. The density of the vegetation cover is used to classify it (low to high). The average vegetation cover was calculated to be greater than 31.5 Mha. The minimum vegetation cover was 14.9 Mha, and the maximum vegetation cover was 49.2 Mha. 15.8 Mha can be cultivated without supplementary irrigation for at least one agricultural season, according to the rainfall classification map.

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