Climate Dynamics

, Volume 36, Issue 9, pp 1633–1647

Simulation of the anthropogenic aerosols over South Asia and their effects on Indian summer monsoon

  • Zhenming Ji
  • Shichang Kang
  • Dongfeng Zhang
  • Chunzi Zhu
  • Jia Wu
  • Ying Xu
Article

DOI: 10.1007/s00382-010-0982-0

Cite this article as:
Ji, Z., Kang, S., Zhang, D. et al. Clim Dyn (2011) 36: 1633. doi:10.1007/s00382-010-0982-0

Abstract

A regional climate model coupled with a chemistry-aerosol model is employed to simulate the anthropogenic aerosols including sulfate, black carbon and organic carbon and their direct effect on climate over South Asia. The model is driven by the NCAR/NCEP re-analysis data. Multi-year simulations with half, normal and double emission fluxes are conducted. Results show that the model performs well in reproducing present climate over the region. Simulations of the aerosol optical depth and surface concentration of aerosols are also reasonable although to a less extent. The negative radiative forcing is found at the top of atmosphere and largely depended on emission concentration. Surface air temperature decreases by 0.1–0.5°C both in pre-monsoon and monsoon seasons. The range and intensity of cooling areas enlarge while aerosol emission increases. Changes in precipitation are between −25 and 25%. Different diversifications of rainfall are showed with three emission scenarios. The changes of precipitation are consistent with varieties of monsoon onset dates in pre-monsoon season. In the regions of increasing precipitation, monsoon onset is advanced and vice versa. In northeast India and Myanmar, aerosols lead the India summer monsoon onset advancing 1–2 pentads, and delaying by 1–2 pentads in central and southeast India. These changes are mainly caused by the anomaly of local Hadley circulations and enhancive precipitation. Tibetan Plateau played a crucial role in the circulation changes.

Keywords

Indian summer monsoonRegional climate modelAerosolsClimate effect

Copyright information

© Springer-Verlag 2010

Authors and Affiliations

  • Zhenming Ji
    • 1
    • 2
    • 3
  • Shichang Kang
    • 1
    • 4
  • Dongfeng Zhang
    • 5
  • Chunzi Zhu
    • 6
  • Jia Wu
    • 2
  • Ying Xu
    • 2
  1. 1.Key Laboratory of Tibetan Environment Changes and Land Surface ProcessesInstitute of Tibetan Plateau Research, Chinese Academy of SciencesBeijingChina
  2. 2.National Climate CenterBeijingChina
  3. 3.Graduate University of Chinese Academy of SciencesBeijingChina
  4. 4.State Key Laboratory of Cryospheric ScienceChinese Academy of SciencesLanzhouChina
  5. 5.Shanxi Meteorological BureauTaiyuanChina
  6. 6.College of Atmospheric ScienceNanjing University of Information Science TechnologyNanjingChina