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- W3000073951 abstract "The Indo-Asian Monsoon (IAM) has changed as the topographies of Asia were assembled into their current configuration. Understanding complex interactions between topography and the IAM through time has been hampered, in part, by poorly resolved topography and atmospheric dynamics in climate models. Here, we employ high-resolution (0.23° × 0.31°) global climate simulations, to more accurately capture these interactions. We find that the Himalayas and Tibet primarily redirect the onshore moisture transport and produce local orographic precipitation. The Iranian Plateau is the primary gatekeeper, insulating the pool of high-enthalpy air in the Indo-Gangetic Plain (IGP) from westerly low-enthalpy advection. But, even when such high-enthalpy air exists along the IGP, vigorous precipitation in the region (poleward of 25°N) still requires orographic steering and lifting. The large-scale circulations—largely governed by sea surface temperature gradients—robustly advect water vapor onshore regardless of topography. Thus, neither topography nor localized enthalpy air drives onshore monsoon flow." @default.
- W3000073951 created "2020-01-23" @default.
- W3000073951 creator A5014070737 @default.
- W3000073951 creator A5015696216 @default.
- W3000073951 date "2020-02-03" @default.
- W3000073951 modified "2023-10-13" @default.
- W3000073951 title "Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon" @default.
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- W3000073951 doi "https://doi.org/10.1029/2019gl085112" @default.
- W3000073951 hasPublicationYear "2020" @default.
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