Related Experiment Video
Updated: Aug 13, 2025

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
Additional risk in extreme precipitation in China from 1.5 °C to 2.0 °C global warming levels
Wei Li1, Zhihong Jiang2, Xuebin Zhang3
1Key Laboratory of Meteorological Disaster of Ministry of Education, Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disaster, Nanjing University of Information Science and Technology, Nanjing 210044, China.
Abstract:
To avoid dangerous climate change impact, the Paris Agreement sets out two ambitious goals: to limit the global warming to be well below 2 °C and to pursue effort for the global warming to be below 1.5 °C above the pre-industrial level. As climate change risks may be region-dependent, changes in magnitude and probability of extreme precipitation over China are investigated under those two global warming levels based on simulations from the Coupled Model Inter-Comparison Projects Phase 5. The focus is on the added changes due to the additional half a degree warming from 1.5 °C to 2 °C. Results show that regional average changes in the magnitude do not depend on the return periods with a relative increase around 7% and 11% at the 1.5 °C and 2 °C global warming levels, respectively. The additional half a degree global warming adds an additional increase in the magnitude by nearly 4%. The regional average changes in term of occurrence probabilities show dependence on the return periods, with rarer events (longer return periods) having larger increase of risk. For the 100-year historical event, the probability is projected to increase by a factor of 1.6 and 2.4 at the 1.5 °C and 2 °C global warming levels, respectively. The projected changes in extreme precipitation are independent of the RCP scenarios.
Related Concept Videos
Global Climate Change
What is Weather?
What is Climate?
Precipitation and Co-precipitation
Responses to Heat and Cold Stress
Responses to Drought and Flooding

