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• W3136194572 endingPage "632" @default.
• W3136194572 startingPage "611" @default.
• W3136194572 abstract "Abstract Based on the hourly gauge-satellite merged precipitation data with the spatial resolution of 0.1° × 0.1° during 2013 ~ 2018, we have evaluated the performance of the convection-permitting Weather Research and Forecasting model at Nanjing University (WRF_NJU) in forecasting the precipitation diurnal variation and the associated atmospheric circulation over the eastern Tibetan Plateau and its surrounding regions during summer. Results indicate that WRF_NJU model can well reproduce the diurnal cycle of the summer precipitation in terms of the diurnal peak time, duration and magnitude. In addition, the eastward propagation of rainfall systems with long duration along the eastern Tibetan Plateau (ETP) and its adjacent areas can also be properly captured. The WRF_NJU model can reasonably reproduce the relevant atmospheric circulation during summer as well. However, the model tends to underestimate the summer precipitation amount (PA) and precipitation frequency (PF) over most time of a day. Relatively larger biases in the occurring time and magnitude of PA and PF diurnal peaks can be noted over the ETP and Sichuan Basin. Further analysis suggests that the underestimation of PA over the ETP is attributed to the much lower moisture supply, weaker low-level southwesterly winds and less convective available potential energy (CAPE) in the WRF_NJU model than in ERA5. Over Sichuan Basin, the underestimated PA is related to the weaker upward motion, which is corresponding to the cold biases of surface air temperature in WRF_NJU. Findings of this study provide the basic model biases and may be helpful to further improve the model physical processes." @default.
• W3136194572 created "2021-03-29" @default.
• W3136194572 creator A5004210622 @default.
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• W3136194572 creator A5064962959 @default.
• W3136194572 creator A5084282171 @default.
• W3136194572 creator A5084741506 @default.
• W3136194572 date "2021-03-23" @default.
• W3136194572 modified "2023-10-16" @default.
• W3136194572 title "Diurnal cycle of summer precipitation over the Eastern Tibetan Plateau and surrounding regions simulated in a convection-permitting model" @default.
• W3136194572 cites W1509747376 @default.
• W3136194572 cites W1653781294 @default.
• W3136194572 cites W1826780856 @default.
• W3136194572 cites W1944739169 @default.
• W3136194572 cites W1968616135 @default.
• W3136194572 cites W1969004359 @default.
• W3136194572 cites W1972193627 @default.
• W3136194572 cites W1980367911 @default.
• W3136194572 cites W1981670386 @default.
• W3136194572 cites W1984559227 @default.
• W3136194572 cites W1985479415 @default.
• W3136194572 cites W1989324328 @default.
• W3136194572 cites W1993602905 @default.
• W3136194572 cites W1995386015 @default.
• W3136194572 cites W1997416260 @default.
• W3136194572 cites W2005698219 @default.
• W3136194572 cites W2006615756 @default.
• W3136194572 cites W2009809171 @default.
• W3136194572 cites W2014074374 @default.
• W3136194572 cites W2021942307 @default.
• W3136194572 cites W2023308405 @default.
• W3136194572 cites W2023465072 @default.
• W3136194572 cites W2024956085 @default.
• W3136194572 cites W2030637940 @default.
• W3136194572 cites W2036903113 @default.
• W3136194572 cites W2037254286 @default.
• W3136194572 cites W2041200453 @default.
• W3136194572 cites W2042580095 @default.
• W3136194572 cites W2044480475 @default.
• W3136194572 cites W2046274250 @default.
• W3136194572 cites W2047220310 @default.
• W3136194572 cites W2056286716 @default.
• W3136194572 cites W2056827281 @default.
• W3136194572 cites W2061243737 @default.
• W3136194572 cites W2062698821 @default.
• W3136194572 cites W2066761143 @default.
• W3136194572 cites W2069784490 @default.
• W3136194572 cites W2070158856 @default.
• W3136194572 cites W2071612376 @default.
• W3136194572 cites W2074506429 @default.
• W3136194572 cites W2074622742 @default.
• W3136194572 cites W2089432462 @default.
• W3136194572 cites W2090302124 @default.
• W3136194572 cites W2091341211 @default.
• W3136194572 cites W2094256348 @default.
• W3136194572 cites W2097846111 @default.
• W3136194572 cites W2101394945 @default.
• W3136194572 cites W2103518822 @default.
• W3136194572 cites W2115466864 @default.
• W3136194572 cites W2116065142 @default.
• W3136194572 cites W2116149712 @default.
• W3136194572 cites W2121745948 @default.
• W3136194572 cites W2125337722 @default.
• W3136194572 cites W2125805649 @default.
• W3136194572 cites W2129031626 @default.
• W3136194572 cites W2130803606 @default.
• W3136194572 cites W2134506346 @default.
• W3136194572 cites W2139940184 @default.
• W3136194572 cites W2145724864 @default.
• W3136194572 cites W2151788810 @default.
• W3136194572 cites W2162915715 @default.
• W3136194572 cites W2167414301 @default.
• W3136194572 cites W2171317906 @default.
• W3136194572 cites W2172954498 @default.
• W3136194572 cites W2178483954 @default.
• W3136194572 cites W2329167291 @default.
• W3136194572 cites W2339557483 @default.
• W3136194572 cites W2513550624 @default.
• W3136194572 cites W2516236395 @default.
• W3136194572 cites W2532471958 @default.
• W3136194572 cites W2532651267 @default.
• W3136194572 cites W2536595330 @default.
• W3136194572 cites W2611921120 @default.
• W3136194572 cites W2751992959 @default.
• W3136194572 cites W2766809502 @default.
• W3136194572 cites W2770767637 @default.
• W3136194572 cites W2774421483 @default.
• W3136194572 cites W2777814343 @default.
• W3136194572 cites W2786865944 @default.
• W3136194572 cites W2789356037 @default.
• W3136194572 cites W2793688347 @default.
• W3136194572 cites W2802541873 @default.
• W3136194572 cites W2807613185 @default.
• W3136194572 cites W2809641348 @default.
• W3136194572 cites W2883210500 @default.
• W3136194572 cites W2905396630 @default.

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