Abstract

Based on the historical and future outputs of 17 coupled model intercomparison project phase 5 (CMIP5) models, simulation of the precipitation extremes in China was evaluated under baseline climate condition compared to a gridded daily observation dataset CN05.1. The variations in precipitation extremes for eight global warming targets were also projected. The 17 individual models and the multi-model ensemble accurately reproduced the spatial distribution of precipitation extremes, although they were limited in their ability to capture the temporal characteristics. A notable dry bias existed in Southeast China, while a wet bias was present in North and Northwest China. The precipitation extremes in China were projected to be more frequent and more intense as global temperature rise reached the 1.5, 2.0, 2.5, 3.0, 3.5, 4.0, 4.5, and 5.0 °C warming targets. The projected percentage changes in the annual number of days with precipitation >50 mm (R50) and total precipitation during days in which the daily precipitation exceeds the 99th percentile (R99p) are projected to increase by 25.81 and 69.14 % relative to the baseline climate for a 1.5 °C warming target, and by 95.52 and 162.00 % for a 4.0 °C warming target, respectively. As the global mean temperature rise increased from 1.5 to 5 °C, the subregions considerably affected by the East Asian summer monsoon (e.g., Southwest China, South China, and the Yangtze-Huai River Valley) were projected to experience a more dramatic increase in extreme precipitation events, in both number of days and intensity, while North and Northwest China were projected to suffer from relatively slight increases. The model uncertainties in the projected precipitation extremes in China by 17 CMIP5 models increase as global temperature rise increases.

Highlights

  • Global-scale warming has been determined to dominate climate change across the globe over the past century (IPCC 2013)

  • As the global mean temperature rise increased from 1.5 to 5 °C, the subregions considerably affected by the East Asian summer monsoon (e.g., Southwest China, South China, and the Yangtze-Huai River Valley) were projected to experience a more dramatic increase in extreme precipitation events, in both number of days and intensity, while North and Northwest China were projected to suffer from relatively slight increases

  • 3 Evaluation of precipitation extremes in China simulated by 17 coupled model intercomparison project phase 5 (CMIP5) models

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Summary

Introduction

Global-scale warming has been determined to dominate climate change across the globe over the past century (IPCC 2013). According to climate model projection results, the global mean temperature rise is expected to reach the 4, 4.5, and 5 °C warming targets by the end of twenty-first century (Zhang et al 2013a; Guo et al 2016). Using a high-resolution regional climate model RegCM3, Lang and Sui (2013) found that the number of days where daily precipitation was C10 mm/day and the maximum 5-day total precipitation for China would increase by 0.4 days and 5.1 mm for a 2 °C warming target with respect to the baseline period (1986–2005). The purpose of this study is to explore the characteristics of changes in extreme heavy precipitation events for eight global warming targets (1.5, 2.0, 2.5, 3.0, 3.5, 4.0, 4.5, and 5.0 °C), which will inform policymakers’ understanding of the potential impacts of climate change, allow for the formation of appropriate adaptation strategies, and support an agreement related to the international negotiations on climate change.

Model and observation dataset
Selection of the analyzed time period
Calculation method
Definition of extreme precipitation indices
Division of six subregions in China
Evaluation of model-simulated temporal variability of precipitation extremes
Evaluation of model-simulated spatial features of precipitation extremes
Temporal evolution of precipitation extremes in China from 2006 to 2099
Projected timings to reach eight warming targets using the 17 CMIP5 models
Conclusion and discussion
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