Paper
30 November 2006 Global lightning activity observed by TRMM and monsoon onset
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Abstract
Monsoons are generally considered to be developed by land-ocean differential heating. However, it is revealed from the one to two months time lag between the maximum lightning activity/surface temperature and the monsoon rain onset that the diabatic heating generated by deep cumulus convection is another driving mechanism for monsoon development. The TRMM LIS observations, rainfall measurements, and the ERA-40 reanalyses were analyzed to demonstrate this monsoon development.
© (2006) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Tsing-Chang (Mike) Chen "Global lightning activity observed by TRMM and monsoon onset", Proc. SPIE 6404, Remote Sensing and Modeling of the Atmosphere, Oceans, and Interactions, 64040O (30 November 2006); https://doi.org/10.1117/12.695315
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KEYWORDS
Lithium

Convection

Troposphere

Solids

Atmospheric modeling

Calcium

Prototyping

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