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Evaluation of the Perspective of ERA-Interim and ERA5 Reanalyses for Calculation of Drought Indicators for Uzbekistan

Natella RakhmatovaResearch Hydrometeorological Institute (NIGMI), Centre of Hydrometeorological Service of the Republic of Uzbekistan (Uzhydromet), 72, 1st Bodomzor yuli str., Tashkent 100052, UzbekistanM. L. ArushanovResearch Hydrometeorological Institute (NIGMI), Centre of Hydrometeorological Service of the Republic of Uzbekistan (Uzhydromet), 72, 1st Bodomzor yuli str., Tashkent 100052, UzbekistanLyudmila ShardakovaResearch Hydrometeorological Institute (NIGMI), Centre of Hydrometeorological Service of the Republic of Uzbekistan (Uzhydromet), 72, 1st Bodomzor yuli str., Tashkent 100052, UzbekistanBakhriddin NishonovCentre of Hydrometeorological Service of the Republic of Uzbekistan (Uzhydromet), 72, 1st Bodomzor yuli str., Tashkent 100052, UzbekistanRaisa TaryannikovaCentre of Hydrometeorological Service of the Republic of Uzbekistan (Uzhydromet), 72, 1st Bodomzor yuli str., Tashkent 100052, UzbekistanValeriya RakhmatovaCentre of Hydrometeorological Service of the Republic of Uzbekistan (Uzhydromet), 72, 1st Bodomzor yuli str., Tashkent 100052, UzbekistanDmitry BelikovCenter for Environmental Remote Sensing, Chiba University, 1–33 Yayoi-cho, Inage-ku, Chiba 263-8522, Japan
Atmospherejournal2021en
ABI

Annotatsiya

The arid and semiarid regions of Uzbekistan are sensitive and vulnerable to climate change. However, the sparse and very unevenly distributed meteorological stations within the region provide limited data for studying the region’s climate variation. The aim of this work was to evaluate the performance of the European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA)-Interim and ERA5 products for the fields of near-surface temperature, humidity, and precipitation over Uzbekistan from 1981 to 2018 using observations from 74 meteorological stations. Major results suggested that the reanalysis datasets match well with most of the observed climate records, especially in the plain areas. While ERA5, with a high spatial resolution of 0.1°, is able more accurately reproduce mountain ranges and valleys. Compared to ERA-Interim, the climatological biases in temperature, humidity, and total precipitation from ERA5 are clearly reduced, and the representation of inter-annual variability is improved over most regions of Uzbekistan. Both reanalyses show a high level of agreement with observations on the standardized precipitation evaporation index (SPEI) with a correlation coefficient of 0.7–0.8.Although both of these ECMWF products can be successfully implemented for the calculation of atmospheric drought indicators for Uzbekistan and adjacent regions of Central Asia, the newer and advanced ERA5 is preferred.

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Koʻrsatkichlar — AkademScholar · Tez orada