Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon
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...
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Wiley
2020-02-01
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| Series: | Geophysical Research Letters |
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| Online Access: | https://doi.org/10.1029/2019GL085112 |
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| author | R. P. Acosta M. Huber |
| author_facet | R. P. Acosta M. Huber |
| author_sort | R. P. Acosta |
| collection | DOAJ |
| description | 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. |
| format | Article |
| id | doaj-art-5829cd7e75b34e7e93eb6e2888bd15b1 |
| institution | OA Journals |
| issn | 0094-8276 1944-8007 |
| language | English |
| publishDate | 2020-02-01 |
| publisher | Wiley |
| record_format | Article |
| series | Geophysical Research Letters |
| spelling | doaj-art-5829cd7e75b34e7e93eb6e2888bd15b12025-08-20T01:50:15ZengWileyGeophysical Research Letters0094-82761944-80072020-02-01473n/an/a10.1029/2019GL085112Competing Topographic Mechanisms for the Summer Indo‐Asian MonsoonR. P. Acosta0M. Huber1Department of Earth, Atmospheric, and Planetary Sciences Purdue University West Lafayette IN USADepartment of Earth, Atmospheric, and Planetary Sciences Purdue University West Lafayette IN USAAbstract 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.https://doi.org/10.1029/2019GL085112Asian MonsoonIndian MonsoonHigh‐resolution Climate ModelingTopography‐Atmosphere InteractionsTibetan PlateauHimalayan Mountains |
| spellingShingle | R. P. Acosta M. Huber Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon Geophysical Research Letters Asian Monsoon Indian Monsoon High‐resolution Climate Modeling Topography‐Atmosphere Interactions Tibetan Plateau Himalayan Mountains |
| title | Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon |
| title_full | Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon |
| title_fullStr | Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon |
| title_full_unstemmed | Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon |
| title_short | Competing Topographic Mechanisms for the Summer Indo‐Asian Monsoon |
| title_sort | competing topographic mechanisms for the summer indo asian monsoon |
| topic | Asian Monsoon Indian Monsoon High‐resolution Climate Modeling Topography‐Atmosphere Interactions Tibetan Plateau Himalayan Mountains |
| url | https://doi.org/10.1029/2019GL085112 |
| work_keys_str_mv | AT rpacosta competingtopographicmechanismsforthesummerindoasianmonsoon AT mhuber competingtopographicmechanismsforthesummerindoasianmonsoon |