Modelling the effect of aerosol and greenhouse gas forcing on the South and East Asian monsoons with an intermediate complexity climate model

TL;DR

This study uses an intermediate complexity climate model to analyze how aerosols and greenhouse gases influence the South and East Asian monsoons, revealing regional variations and interactions affecting precipitation patterns.

Contribution

It provides new insights into the regional impacts of aerosol and greenhouse gas forcing on Asian monsoons using an intermediate complexity climate model.

Findings

Aerosol loading decreases summer precipitation regionally.

Precipitation reduction is linked to atmospheric stratification changes.

Doubling CO2 increases precipitation and weakens circulation.

Abstract

The South and East Asian summer monsoons are globally significant meteorological features, creating a strongly seasonal pattern of precipitation. The stability of the monsoon is of extreme importance for a vast range of ecosystems and for the livelihoods of a large share of the world's population. Simulations are performed with an intermediate complexity climate model, PLASIM, to assess the future response of the monsoons to changing concentrations of aerosols and greenhouse gases. The aerosol loading consists of a mid-tropospheric warming and a surface cooling, which is applied to India, Southeast Asia and East China, both concurrently and independently. The primary effect of increased aerosol loading is a decrease in summer precipitation in the vicinity of the applied forcing, although the regional response varies significantly. The decrease in precipitation is only partially ascribable to a decrease in the precipitable water, and instead derives from a reduction of the precipitation efficiency, due to changes in the stratification of the atmosphere. When the aerosol loading is added in all regions simultaneously, precipitation in East China is most strongly affected, with a quite distinct transition to a low precipitation regime as the radiative forcing increases beyond 60 W/m^2. The response is less abrupt as we move westward, with precipitation in South India being least affected. This lower sensitivity in South India is attributed to aerosol forcing over East China. Additionally, the effect on precipitation is approximately linear with the forcing. The impact of doubling carbon dioxide levels is to increase precipitation over the regions and weaken the circulation. When the carbon dioxide and aerosol forcings are applied at the same time, the carbon dioxide forcing partially offsets the surface cooling and reduction in precipitation associated with the aerosol response.