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Using the Regional Atmospheric Modeling System (RAMS) we show that agricultural intensification and irrigation can modify the surface moisture and energy distribution, which alters the boundary layer and regional convergence, mesoscale convection, and precipitation patterns over the Indian monsoon region.
Yang, X. et al. Holocene stalagmite δ18O records in the East Asian monsoon region and their correlation with those in the Indian monsoon region.
However, the mechanism of such effects in the Asian monsoon region remains unclear.
The scientific explanation of speleothem δ18O in Chinese monsoon region is a greatly debated issue.
These agricultural changes, including irrigation modify the mesoscale convection and rain patterns in the Indian monsoon region.
This domain is part of the North American Monsoon region, and the summer period (June–July August, JJA) was considered.
Similar(20)
values for different 'homogeneous monsoon regions'.
For further information on prominent monsoon regions, see Indian monsoon, West African monsoon, Malaysian-Australian monsoon, and North American monsoon.
Climatic patterns reminiscent of monsoons also occur in areas outside of the prominent monsoon regions.
Gadgil, S., Joshi, N. V. & Joseph, P. V. Ocouplingoverere coupling over monsoon regions.
At the surface in monsoon regions, both dry and wet spells result.
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