Arctic coasts are vulnerable to the effects of climate change, including rising sea levels and
the loss of permafrost, sea ice and glaciers. Assessing the influence of anthropogenic …

Global monitoring of persistent organic pollutants (POPs) has intensified following regulatory
efforts aimed at reducing their release. In this context, we compiled over 10,000 POP …

The surface temperature is one of the main parameters for assessing climate change.
Temperature change is most pronounced in the Arctic, and therefore, it is crucial to …

The conterminous marine system of the Bering Sea serves as an important connection
between the Pacific and the Arctic. Surface water temperatures of the Northern Pacific have …

The assessment of expected changes in coastal sea surface temperature (SST) on a global
scale is becoming increasingly important due to the growing pressure on coastal …

The dry‐wet abrupt alternation (DWAA) event, which is defined as the phenomenon of dry
(or wet) spells abruptly following wet (or dry) spells, magnifies the influence of individual wet …

With global warming, the decrease in sea ice creates favorable conditions for Arctic
activities. Sea surface temperature (SST) is not only an important driven factor of sea ice …

The historical annual loading to, removal from, and cumulative burden in the Arctic Ocean
for β-hexachlorocyclohexane (β-HCH), an isomer comprising 5–12% of technical HCH, is …

In the Arctic Ocean, sea ice algae are responsible for a small but seasonally important pulse
of primary production. Their persistence is threatened by the rapid loss of sea ice from the …

As Arctic sea ice retreats during the melt season, the upper ocean warms in response to
atmospheric heat fluxes. Overall, clouds reduce these fluxes in summer, but how the …