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    Upper tropospheric moistening during the Asian summer monsoon in a changing climate

    This study investigates the projected changes in the upper troposphere and lower stratosphere (UTLS) water vapor over the Asian summer monsoon (ASM) region based on satellite records, numerical simulations usi...

    Bhupendra Bahadur Singh, R. Krishnan, T. P. Sabin, Ramesh K. Vellore in Climate Dynamics (2024)

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    Linkage of water vapor distribution in the lower stratosphere to organized Asian summer monsoon convection

    Accumulation of water vapor in the upper troposphere/lower stratosphere (UT/LS) over the Asian continent is a recognized feature during the boreal summer monsoon. While there has been a debate on the role of m...

    Bhupendra Bahadur Singh, Raghavan Krishnan, D. C. Ayantika in Climate Dynamics (2021)

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    Widespread fog over the Indo-Gangetic Plains and possible links to boreal winter teleconnections

    Boreal wintertime planetary-scale atmospheric circulations and their possible consequences to widespread fog occurrences over the Indo-Gangetic Plains (IGP) region of the Himalayan valley are investigated in t...

    Dipti Hingmire, Ramesh K. Vellore, R. Krishnan, N. V. Ashtikar in Climate Dynamics (2019)

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    Monsoon-extratropical circulation interactions in Himalayan extreme rainfall

    Extreme precipitation and flood episodes in the Himalayas are oftentimes traced to synoptic situations involving connections between equatorward advancing upper level extratropical circulations and moisture-la...

    Ramesh K. Vellore, Michael L. Kaplan, R. Krishnan, John M. Lewis in Climate Dynamics (2016)

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    On the anomalous precipitation enhancement over the Himalayan foothills during monsoon breaks

    An intriguing feature associated with ‘breaks’ in the Indian summer monsoon is the occurrence of intense/flood-producing precipitation confined to central-eastern parts of the Himalayan (CEH) foothills and nor...

    Ramesh K. Vellore, R. Krishnan, Jayant Pendharkar in Climate Dynamics (2014)