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The role of tropical volcanic eruptions in exacerbating Indian droughts

Listed in National Center for Atmospheric Research

The Indian summer monsoon rainfall (ISMR) is vital for the livelihood of millions of people in the Indian region; droughts caused by monsoon failures often resulted in famines.

Description

Large volcanic eruptions have been linked with reductions in ISMR, but the responsible mechanisms remain unclear. Here, using 145-year (1871-2016) records of volcanic eruptions and ISMR, we show that ISMR deficits prevail for two years after moderate and large (VEI>3) tropical volcanic eruptions; this is not the case for extra-tropical eruptions.

Moreover, tropical volcanic eruptions strengthen El Nino and weaken La Nina conditions, further enhancing Indian droughts. Using climate-model simulations of the 2011 Nabro volcanic eruption, we show that eruption induced an El Nino like warming in the central Pacific for two consecutive years due to Kelvin wave dissipation triggered by the eruption. This El Nino like warming in the central Pacific led to a precipitation reduction in the Indian region.

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In addition, solar dimming caused by the volcanic plume in 2011 reduced Indian rainfall.

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Provenance · 1 source records, 7 field assertions
SourceKeyLast seenRaw
National Center for Atmospheric Researchb5edbfaf-f5a1-42c1-b2f7-9dd2de3971f410 d agoJSON v1
FieldAssertionExtractorEvidence
concepts[field].local:field:earth-environmentalmapping · data ucar educonnector:data_ucar_edu@1.0.0
concepts[field].local:field:ocean-atmosphericmapping · data ucar educonnector:data_ucar_edu@1.0.0
created_datesource · data ucar educonnector:data_ucar_edu@1.0.0
descriptionsource · data ucar educonnector:data_ucar_edu@1.0.0/notes
publication_datesource · data ucar educonnector:data_ucar_edu@1.0.0
titlesource · data ucar educonnector:data_ucar_edu@1.0.0/title
updated_datesource · data ucar educonnector:data_ucar_edu@1.0.0