TY - JOUR
T1 - On the Controlling Factors for Globally Extreme Humid Heat
AU - Raymond, Colin
AU - Matthews, Tom
AU - Horton, Radley M.
AU - Fischer, Erich M.
AU - Fueglistaler, Stephan
AU - Ivanovich, Catherine
AU - Suarez-Gutierrez, Laura
AU - Zhang, Yi
N1 - Publisher Copyright:
© 2021 American Geophysical Union. All Rights Reserved. California Institute of Technology. Government sponsorship acknowledged.
PY - 2021/12/16
Y1 - 2021/12/16
N2 - Humid heat presents a major societal challenge through its impacts on human health, energy demand, and economic productivity, underlined by the projected emergence of conditions beyond human tolerance. However, systematic assessment of what drives the most extreme humid heat worldwide has been lacking. Here, we investigate factors determining the location and magnitude of humid-heat extremes, framing our analysis around the four regions with the highest values: the southern Persian Gulf, north-central Pakistan, eastern South Asia, and the western Amazon. We find that strong boundary-layer moisture fluxes, together with stability that inhibits moist convection, explain well the timing and location of near-surface humid-heat extremes. These favorable conditions are achieved through regionally distinct factors, including shallow sea breezes in the Persian Gulf and large-scale subsidence in eastern South Asia. Our results demonstrate some of the principal controls on the most intense humid heat, both globally and for particular regions and heat events.
AB - Humid heat presents a major societal challenge through its impacts on human health, energy demand, and economic productivity, underlined by the projected emergence of conditions beyond human tolerance. However, systematic assessment of what drives the most extreme humid heat worldwide has been lacking. Here, we investigate factors determining the location and magnitude of humid-heat extremes, framing our analysis around the four regions with the highest values: the southern Persian Gulf, north-central Pakistan, eastern South Asia, and the western Amazon. We find that strong boundary-layer moisture fluxes, together with stability that inhibits moist convection, explain well the timing and location of near-surface humid-heat extremes. These favorable conditions are achieved through regionally distinct factors, including shallow sea breezes in the Persian Gulf and large-scale subsidence in eastern South Asia. Our results demonstrate some of the principal controls on the most intense humid heat, both globally and for particular regions and heat events.
KW - boundary-layer meteorology
KW - climate dynamics
KW - compound extremes
KW - humid heat
KW - multi-scale interactions
UR - http://www.scopus.com/inward/record.url?scp=85120806146&partnerID=8YFLogxK
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U2 - 10.1029/2021GL096082
DO - 10.1029/2021GL096082
M3 - Article
AN - SCOPUS:85120806146
SN - 0094-8276
VL - 48
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 23
M1 - e2021GL096082
ER -