4.6 Article

Intraseasonal, Seasonal, and Interannual Characteristics of Regional Monsoon Simulations in CESM2

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2019MS001962

Keywords

global coupled Earth system modeling; Asian-Australian monsoon; west African monsoon; north American monsoon; south American monsoon

Funding

  1. National Science Foundation (NSF) [1460742]
  2. Regional and Global Model Analysis (RGMA) component of the Earth and Environmental System Modeling Program of the U.S. Department of Energy's Office of Biological and Environmental Research (BER) via National Science Foundation [IA 1947282]
  3. National Center for Atmospheric Research - National Science Foundation (NSF) [1852977]
  4. Directorate For Geosciences
  5. Div Atmospheric & Geospace Sciences [1460742] Funding Source: National Science Foundation

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A survey of intraseasonal, seasonal, and interannual precipitation and 850 hPa winds for various monsoon regimes around the world is presented for the Community Earth System Model Version 2 (CESM2) compared to observations and the previous generation CESM1. In CESM2 the south Asian monsoon has a reduction of excessive precipitation in the western Indian Ocean and an increase of precipitation in the eastern Bay of Bengal and land areas of Vietnam, Cambodia, and Laos. The seasonal timing of the south Asian monsoon, monsoon-ENSO connections, and monsoon intraseasonal variability all are improved compared to CESM1. For the Australian monsoon, deficient precipitation over the Maritime Continent has been improved in CESM2 with increases of precipitation over the large tropical islands of Borneo, Celebes, and Papua New Guinea and decreases over southwestern Australia. In the West African monsoon, May-June seasonal rainfall occurs more preferentially over the African coast in CESM2 as in observations, and excessive rainfall over the Ethiopian region is reduced. During July-September in the West African monsoon, deficient precipitation over equatorial Africa in CESM1 has been lessened in CESM2, and there are increases in precipitation over the Guinean coast, though there is little overall improvement in the South African monsoon. In the South American monsoon, precipitation in CESM2 is improved with increased precipitation over the Amazon in central and western Brazil. CESM2 simulates a reduction of excessive precipitation seen in CESM1 over coastal Mexico extending up into the U.S. Great Plains in the North American monsoon.

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