Premium
The Atmospheric Response to North Atlantic SST Trends, 1870–2019
Author(s) -
Karnauskas Kristopher B.,
Zhang Lei,
Amaya Dillon J.
Publication year - 2021
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 - 10.1029/2020gl090677
Subject(s) - ocean gyre , climatology , intertropical convergence zone , north atlantic oscillation , forcing (mathematics) , sea surface temperature , atlantic equatorial mode , atmospheric circulation , atlantic multidecadal oscillation , westerlies , thermohaline circulation , atmosphere (unit) , subtropics , geology , shutdown of thermohaline circulation , north atlantic deep water , environmental science , oceanography , geography , precipitation , meteorology , fishery , biology
Sea surface temperature (SST) observations in the North Atlantic since 1870 reveal a region of enhanced warming off the northeastern coast of North America, and a region of cooling to the south of Greenland. It has been hypothesized that these adjacent SST trends are a result of long‐term changes in the buoyancy‐driven ocean circulation—a slowdown of the Atlantic Meridional Overturning Circulation. The impacts of these historical SST trends on the atmosphere are estimated using idealized atmospheric general circulation model experiments in which the global atmosphere is exposed to modern climatological forcing minus the aforementioned regional SST trends. The local response includes a negative North Atlantic Oscillation tendency and southward shift of the wind forcing for the subtropical gyre. Due to planetary wave propagation, the regional SST trends also induce a northward shift of the intertropical convergence zone over the Indian Ocean. Implications for climate feedbacks and projections are discussed.