Информация о цитировании статьи получена из
Web of Science,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 27 ноября 2016 г.
Аннотация:This study was motivated by a strong warming signal
seen in mooring-based and oceanographic survey data
collected in 2004 in the Eurasian Basin of the Arctic
Ocean. The source of this and earlier Arctic Ocean changes
lies in interactions between polar and sub-polar basins.
Evidence suggests such changes are abrupt, or pulse-like,
taking the form of propagating anomalies that can be traced
to higher-latitudes. For example, an anomaly found in 2004
in the eastern Eurasian Basin took 1.5 years to propagate
from the Norwegian Sea to the Fram Strait region, and
additional 4.5–5 years to reach the Laptev Sea slope.
While the causes of the observed changes will require further
investigation, our conclusio ns are consistent with prevailing
ideas suggesting the Arctic Ocean is in transition towards a
new, warmer state.