dc.contributor.authorSamanta, Dhrubajyoti
dc.contributor.authorHameed, Saji N.
dc.contributor.authorJin, Dachao
dc.contributor.authorThilakan, Vishnu
dc.contributor.authorGanai, Malay
dc.contributor.authorRao, Suryachandra A.
dc.contributor.authorDeshpande, Medha
dc.date.accessioned2019-01-11T05:20:44Z
dc.date.available2019-01-11T05:20:44Z
dc.date.issued2018
dc.identifier.citationSamanta, D., Hameed, S. N., Jin, D., Thilakan, V., Ganai, M., Rao, S. A., & Deshpande, M. (2018). Impact of a narrow coastal Bay of Bengal sea surface temperature front on an Indian summer monsoon simulation. Scientific Reports, 8(1), 17694-. doi:10.1038/s41598-018-35735-3en_US
dc.identifier.urihttp://hdl.handle.net/10220/47446
dc.description.abstractA dry bias in climatological Central Indian rainfall plagues Indian summer monsoon (ISM) simulations in multiple generations of climate models. Here, using observations and regional climate modeling, we focus on a warm coastal Bay of Bengal sea surface temperature (SST) front and its impact on Central Indian rainfall. The SST front, featuring sharp gradients as large as 0.5 °C/100 km, is colocated with a mixed layer depth (MLD) front, in a region where salinity variations are known to control MLD. Regional climate simulations coupling a regional atmospheric model with an ocean mixed layer model are performed. A simulation with observed MLD climatology reproduces SST, rainfall, and atmospheric circulation associated with ISM reasonably well; it also eliminates the dry bias over Central India significantly. Perturbing MLD structure in the simulations, we isolate the SST front’s impact on the simulated ISM climate state. This experiment offers insights into ISM climatological biases in the coupled NCEP Climate Forecast System version-2. We suggest that the warm SST front is essential to Central Indian rainfall as it helps to sustain deep and intense convection in its vicinity, which may be a source for the vortex cores seeding the monsoon low-pressure systems.en_US
dc.format.extent12 p.en_US
dc.language.isoenen_US
dc.relation.ispartofseriesScientific Reportsen_US
dc.rights© 2018 The Author(s). This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.en_US
dc.subjectSea Surface Temperatureen_US
dc.subjectIndian Summer Monsoonen_US
dc.subjectDRNTU::Social sciences::Geography::Environmental sciencesen_US
dc.titleImpact of a narrow coastal Bay of Bengal sea surface temperature front on an Indian summer monsoon simulationen_US
dc.typeJournal Article
dc.contributor.schoolAsian School of the Environmenten_US
dc.identifier.doihttp://dx.doi.org/10.1038/s41598-018-35735-3
dc.description.versionPublished versionen_US


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