Drought losses in China might double between the 1.5 °C and 2.0 °C warming

Proc Natl Acad Sci U S A. 2018 Oct 16;115(42):10600-10605. doi: 10.1073/pnas.1802129115. Epub 2018 Oct 1.

Abstract

We project drought losses in China under global temperature increase of 1.5 °C and 2.0 °C, based on the Standardized Precipitation Evapotranspiration Index (SPEI) and the Palmer Drought Severity Index (PDSI), a cluster analysis method, and "intensity-loss rate" function. In contrast to earlier studies, to project the drought losses, we predict the regional gross domestic product under shared socioeconomic pathways instead of using a static socioeconomic scenario. We identify increasing precipitation and evapotranspiration pattern for the 1.5 °C and 2.0 °C global warming above the preindustrial at 2020-2039 and 2040-2059, respectively. With increasing drought intensity and areal coverage across China, drought losses will soar. The estimated loss in a sustainable development pathway at the 1.5 °C warming level increases 10-fold in comparison with the reference period 1986-2005 and nearly threefold relative to the interval 2006-2015. However, limiting the temperature increase to 1.5 °C can reduce the annual drought losses in China by several tens of billions of US dollars, compared with the 2.0 °C warming.

Keywords: China; drought; drought losses; global warming; projections.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • China
  • Droughts / prevention & control
  • Droughts / statistics & numerical data*
  • Global Warming*
  • Humans
  • Models, Theoretical*
  • Seasons*
  • Temperature
  • Time Factors