Abstract

Our observational study revealed that the precipitation increased over the wet area and decreased over the dry area during the past two decades. Here, we further investigate whether the current atmospheric models can quantitatively capture the characteristics of precipitation from the observation. The NASA Goddard Institute for Space Studies (GISS) model is used to examine the historic simulation of the precipitation, in which the historic greenhouse gases and aerosols are included in the radiative forcing. The consistency between the historic GISS simulation and the Global Precipitation Climatology Project (GPCP) precipitation suggests that the model can qualitatively capture the temporal trends of precipitation over the wet and dry areas. However, the precipitation trends are weaker in the model than in the observation. The observed trends of precipitation do not appear in the control simulation with the fixed concentrations of greenhouse gases and aerosols, which suggests that the global warming due to anthropogenic forcing can influence the temporal variations of precipitation over the wet and dry areas. Diagnostic studies of other variables from the model further suggest that enhanced rising air can increase the precipitation over the wet area.

Highlights

  • The influence of greenhouse gases on global warming has been investigated in numerous studies [1–3]

  • Previous studies [10, 19–23] try to separate the data into wet versus dry regions; they find that precipitation has an increasing tendency in the wet areas and has a decreasing tendency in dry areas, which is referred to as the “rich-getricher” mechanism

  • The Goddard Institute for Space Studies (GISS) model simulations imply that the anthropogenic forcing can affect the temporal variations of precipitation over the wet and dry areas

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Summary

Introduction

The influence of greenhouse gases on global warming has been investigated in numerous studies [1–3]. Compared with the Clausius-Clapeyron equation relating water vapor to the atmospheric temperature [4, 5], there is no simple relationship between precipitation and the atmospheric temperature [6–10]. This is because precipitation is influenced by more factors, such as atmospheric circulation, solar forcing, anthropogenic forcing, and cloud [11, 12]. Most observational studies [7, 10, 14, 15] and climate models [16–18] suggest that global precipitation is increasing more slowly than the total mass of water vapor in response to global warming. We will investigate whether a current climate model can capture the characteristics of the temporal variations of the precipitation by emphasizing the role of the greenhouse gases and aerosols.

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