4.7 Article

Interannual Variation of Summer Atmospheric Heat Source over the Tibetan Plateau and the Role of Convection around the Western Maritime Continent

Journal

JOURNAL OF CLIMATE
Volume 29, Issue 1, Pages 121-138

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-15-0181.1

Keywords

Circulation; Dynamics; Large-scale motions; Atm; Ocean Structure; Phenomena; Monsoons; Physical Meteorology and Climatology; Latent heating; cooling; Variability; Interannual variability

Funding

  1. National Natural Science Foundation of China [91337107, 91337215, 41375081]
  2. National Basic Research Program of China [2012CB417202, 2014CB953900]
  3. Basic Research and Operation Program of the CMA Institute of Plateau Meteorology [BROP 201514]
  4. Special Funds of Guangdong Province of China (Thousand-Talent Plan'' Fund) [YCJ2013-196]

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The impacts of summer atmospheric heat source over the Tibetan Plateau (TP) on regional climate variation have attracted extensive attention. However, few studies have focused on possible causes of the interannual variation of atmospheric heat source over the TP. Total heat (TH) is generally composed of three components: surface sensible heat, latent heat release of condensation (LH), and radiative convergence. In this study, it is found that interannual variation of summer TH is dominated by LH in the central and eastern TP. The atmospheric circulation patterns associated with the TH over the TP in June are different from those in July and August. Large TH is accompanied by a cyclone centered over the South China Sea in June, which is replaced by an anticyclone in July and August. The interannual variation of July-August TH over the central and eastern TP is significantly affected by convection around the western Maritime Continent (WMC) that modulates the LH over the southeastern TP. Enhanced WMC convection induces an anticyclone to the south of the TP, which favors water vapor transport to the southeastern TP and thus an increase in precipitation. Enhanced convection over the southeastern TP may exert a positive feedback on local precipitation through pumping more water vapor from the southern boundary. Both observations and model simulations indicate that the enhanced WMC convection can induce the anticyclone to the south of the TP and convection-circulation is important for maintenance of the anticyclone.

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