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Precipitation Unevenness in Gauge Observations and Eight Reanalyses from 1979 to 2018 over China

Precipitation is spatially and temporally unevenly distributed. The unevenness of precipitation is crucial for climate change, as well as for water resource management, environmental risk reduction, and industrial/agricultural production. In this study, gauge observations and eight reanalysis produc...

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Bibliographic Details
Published in:Journal of climate 2021-12, Vol.34 (24), p.9797-9810
Main Authors: Wu, Guocan, Li, Yun, Qin, Shun, Mao, Yuna, Wang, Kaicun
Format: Article
Language:English
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Summary:Precipitation is spatially and temporally unevenly distributed. The unevenness of precipitation is crucial for climate change, as well as for water resource management, environmental risk reduction, and industrial/agricultural production. In this study, gauge observations and eight reanalysis products are used to examine the unevenness of precipitation from 1979 to 2018 over China. The results show that all the reanalysis datasets can reproduce the spatial pattern of the annual number of wet days and precipitation intensity, as shown in the observations; however, most reanalyses overestimate the former and underestimate the latter. The mean cumulative fractions of the precipitation amount on the wettest 1, 5, and 10 days to annual total are approximately 9.3%, 29.8%, and 45.1% in the gauge observations, and are 6.6% ± 0.8%, 22.1% ± 2.5%, and 34.3%± 3.5% in the reanalyses. The mean cumulative fractions of precipitation amount on the wettest 1, 5, and 10 days to annual total display a small negative trend based on gauge observations over China (-0.06%, -0.10%, and -0.10% decade⁻¹, respectively) but are positive and stronger in the eight current reanalyses (0.08% ± 0.08%, 0.25% ± 0.08%, and 0.35% ± 0.10% decade⁻¹, respectively). The Japanese 55-year Reanalysis (JRA-55) is the best in quantifying the annual variability of the cumulative fractions of precipitation on the wettest 1, 5, and 10 days over China, while ERA-Interim is the best in reflecting their trends. The reanalyses agree best with the observations in reflecting cumulative fractions of precipitation in the Yangtze River Basin and the worst for northwestern China.
ISSN:0894-8755
1520-0442
DOI:10.1175/JCLI-D-21-0316.1