Abstract

AbstractWhile the IPCC Fifth Assessment Working Group I report assessed observed changes in extreme precipitation on the basis of both absolute and percentile-based extreme indices, human influence on extreme precipitation has rarely been evaluated on the basis of percentile-based extreme indices. Here we conduct a formal detection and attribution analysis on changes in four percentile-based precipitation extreme indices. The indices include annual precipitation totals from days with precipitation exceeding the 99th and 95th percentiles of wet-day precipitation in 1961–90 (R99p and R95p) and their contributions to annual total precipitation (R99pTOT and R95pTOT). We compare these indices from a set of newly compiled observations during 1951–2014 with simulations from models participating in phase 6 of the Coupled Model Intercomparison Project (CMIP6). We show that most land areas with observations experienced increases in these extreme indices with global warming during the historical period 1951–2014. The new CMIP6 models are able to reproduce these overall increases, although with considerable over- or underestimations in some regions. An optimal fingerprinting analysis reveals detectable anthropogenic signals in the observations of these indices averaged over the globe and over most continents. Furthermore, signals of greenhouse gases can be separately detected, taking other forcing into account, over the globe and over Asia in these indices except for R95p. In contrast, signals of anthropogenic aerosols and natural forcings cannot be detected in any of these indices at either global or continental scales.

Highlights

  • Changes in extreme precipitation are attracting attention because of the disastrous effects of extreme precipitation on human life, social economy, agriculture, and ecosystems (IPCC 2013)

  • We find for our analyzed precipitation indices that the linear decompositions are generally reasonable since the response to all-known historical (ALL) forcing is very similar to the sum of those from the greenhouse gas (GHG), AER, and NAT forcings

  • Negative trends are found mainly in a southwest–northeast belt from Southwest China to Northeast China, in western North America, and in southeastern Australia, with the most negative trends occurring to R95p

Read more

Summary

Introduction

Changes in extreme precipitation are attracting attention because of the disastrous effects of extreme precipitation on human life, social economy, agriculture, and ecosystems (IPCC 2013). Diagram (Taylor 2001) with the spatial correlation and normalized standard deviation for mean annual indices during 1951– 2014 from observations and simulations over the global and three continental regions (Fig. S9 in the online supplemental material).

Results
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call