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\begin{document}

\title{Warming of the Barents and GIN Seas}



\author[1]{James Carton}%
\author[2]{leon Chafik}%
\author[3]{Michael Steele}%
\affil[1]{University of Maryland}%
\affil[2]{University of Sweden}%
\affil[3]{University of Washington/APL}%


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  \date{May 27, 2024}


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\begin{abstract}
MAJOR POINTS: 1) The Barents and GIN basins are warming rapidly and
exhibiting strong strong interannual variability. 2) While interannual
variability of heat content in the GIN Seas is controlled by Atlantic
water transport, we show interannual variability of heat content in the
Barents is controlled by surface flux (see also Schlichtholtz et al
2011). 3) Interannual variations in surface flux are the result of
variations in wintertime latent heat loss resulting from intrusions of
warm moist air from the south. 4) (not shown) these variations also
control winter sea ice cover.%
\end{abstract}%



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