Abstract

By using the gridded 0.25° × 0.25° observation dataset of CN05.1 provided by the China Meteorological Administration, this study investigates the variations in nine extreme precipitation indices over the Guangdong-Hong Kong-Macao Greater Bay Area (GBA) in China from 1961 to 2018. Based on trends and interannual variations, the nine kinds of extreme precipitation are classified into four categories: category 1 includes very wet days (R95P), extremely wet days (R99P), the maximum 1-day precipitation amount (RX1day), and the maximum 5-day precipitation amount (RX5day). Category 2 is the number of heavy precipitation days (R10day), the number of very heavy precipitation days (R20day), and the simple daily intensity index (SDII). Categories 3 and 4 are consecutive wet days (CWDday) and consecutive dry days (CDDday), respectively. For the extreme precipitation in category 1, the abrupt change point from fewer to more values occurs in 1991 in summer. Three abrupt change points, from fewer to more in 1972 and 2009 and from more to fewer in 1994, occur in spring. For the extreme precipitation in category 2, the abrupt change point from fewer to more values occurs in 1993 in summer. Three abrupt change points, from fewer to more in 1965 and 2010 and from more to fewer in 1990, occur in spring. Annually and seasonally, abrupt changes occur in the early 2010s for CWDday which clearly increase and for CDDday which clearly decrease. In addition, CWDday exhibit abrupt change points from fewer to more in 1966 and from more to fewer in 1983 in spring. The variations in these extreme precipitation events have significant periodic oscillations of 3–5 years, quasi-8 years, or 8–14 years. During periods 1961–1994, 1995–2009, and 2010–2018, the changes in the annual and most seasonal R95P, R99P, R10day, R20day, and SDII are consistent with those of precipitation. The values in the latter period are increasing compared with those in the former stage. The changes in RX1day, RX5day, CWDday, and CDDday have their own characteristics.

Highlights

  • It is certain that global mean surface temperature has increased since the late 19th century and the first decade of the 21st century has been the warmest (Stocker et al, 2013)

  • By using the gridded 0.25°×0.25° observation dataset of CN05.1 provided by the China Meteorological Administration, this study investigates the variations of the nine precipitation extreme indices over the Guangdong-Hong Kong-Macao Greater Bay Area (GBA) in China in the period from 1961 to 2018

  • Based on trends and inter-annual variations, the nine kinds of extreme precipitation are classified into four categories: the category 1 is the very wet days (R95P), the extremely wet days (R99P), the maximum 1-day precipitation amount (RX1day) and the maximum 5-day precipitation amount (RX5day)

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Summary

Introduction

It is certain that global mean surface temperature has increased since the late 19th century and the first decade of the 21st century has been the warmest (Stocker et al, 2013). The frequency and amount of extreme precipitation increased in South China, Southeast Asia and North China while have a decreasing trend in Yangtze River basin (Sun and Zhang et al, 2017; Cui et al, 2019; Wang et al.,2020). The spatial distribution of summer extreme precipitation events demonstrates remarkable regional differences and an increasing trend is found in the middle and lower reaches of the Yangtze River, South China, and Northwest China, while a decreasing trend occurs in Northeast China, North China, and part of Southwest China (Long et al, 2016). The consecutive dry days and simple daily intensity index have significantly increased, while other extreme precipitation indexes have non-significant increasing trends in the Pearl River Basin in South China (Zhao et al, 2014). Providing scientific basis for relevant departments to deal with climate change

Data And Methods
Variation characteristics of various extreme precipitation
Response of extreme precipitation to abrupt climate change
Conclusions
Full Text
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