2022
DOI: 10.3390/atmos13111922
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Spatial-Temporal Variations of Extreme Precipitation Characteristics and Its Correlation with El Niño-Southern Oscillation during 1960–2019 in Hubei Province, China

Abstract: Extreme precipitation could result in many disasters, such as floods, drought, and soil erosion, further bringing severe economic loss. Based on the daily precipitation records during 1960–2019 of 26 stations obtained from the National Meteorological Science Data Center of China, 10 extreme precipitation indices (EPIs: annual total precipitation (PRCPTOT), max-1-day precipitation amount (RX1day), max-5-day precipitation amount (RX5day), number of heavy rain days (R10), number of very heavy rain days (R10), sim… Show more

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Cited by 3 publications
(1 citation statement)
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“…Particularly, the El Niño-Southern Oscillation (ENSO) plays a crucial role in driving the interannual variations of extreme dry conditions in China (Cao et al [33] ; Wang and Li [34] ). The El Niño-like SST can lead to the intensification and westward shift of the Northwestern Pacific subtropical high, resulting in reduced precipitation and increased temperatures in South and Southwestern China, which in turn favor the occurrence of drought events (Wang et al [35] ). In addition, Asian large-scale orography forcing, particularly the Tibetan Plateau (TP), significantly increases ascent, low-middle cloud formation, and resultant strong spring cloud radiative cooling over Southeastern China (SEC) and downstream ocean, thereby affecting climate change (Kiehl and Trenberth [36] ; Li et al [37] ).…”
Section: Introductionmentioning
confidence: 99%
“…Particularly, the El Niño-Southern Oscillation (ENSO) plays a crucial role in driving the interannual variations of extreme dry conditions in China (Cao et al [33] ; Wang and Li [34] ). The El Niño-like SST can lead to the intensification and westward shift of the Northwestern Pacific subtropical high, resulting in reduced precipitation and increased temperatures in South and Southwestern China, which in turn favor the occurrence of drought events (Wang et al [35] ). In addition, Asian large-scale orography forcing, particularly the Tibetan Plateau (TP), significantly increases ascent, low-middle cloud formation, and resultant strong spring cloud radiative cooling over Southeastern China (SEC) and downstream ocean, thereby affecting climate change (Kiehl and Trenberth [36] ; Li et al [37] ).…”
Section: Introductionmentioning
confidence: 99%