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Footprint of Tropical Mesoscale Convective System Variability on Stratospheric Water Vapor
Author(s) -
Dong W. H.,
Lin Y. L.,
Zhang M. H.,
Huang X. M.
Publication year - 2020
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2019gl086320
Subject(s) - climatology , environmental science , mesoscale meteorology , sea surface temperature , water vapor , stratosphere , forcing (mathematics) , atmospheric sciences , tropical atlantic , convection , tropics , tropical climate , tropical cyclone , climate change , geology , meteorology , oceanography , geography , archaeology , fishery , biology
Mesoscale convective systems (MCSs) play a dominant role in tropical climate. However, the variabilities of their occurrences on a tropical‐wide scale remain elusive, and the way they impact the tropical stratospheric moisture remains under debate. Based on a comprehensive global MCS data set during 1985–2008, we detect distinct transitions in tropical MCS activities, with the occurrence frequency of MCS during 1995–2002 being significantly lower than those before and after this period by over 10%. The stepwise transition of tropical MCSs has a significant impact on stratospheric water vapor: Active MCS occurrences result in an overall drier stratosphere, and vice versa. We demonstrate that these changes are closely related to the sea surface temperature pattern in the tropical central Pacific and the associated Walker circulation shift on convective systems. Our results suggest that the sea surface temperature variability in tropical central Pacific may exert an important forcing on the stratospheric water vapor.