The Atlantic gateway to the Arctic Ocean is influenced by vigorous inflows of Atlantic Water.
The high-latitude impacts of these inflows have strengthened owing to climate change …

Poleward ocean heat transport is a key process in the earth system. We detail and review
the northward Atlantic Water (AW) flow, Arctic Ocean heat transport, and heat loss to the …

Warm water of subtropical origin flows northward in the Atlantic Ocean and transports heat to
high latitudes. This poleward heat transport has been implicated as one possible cause of …

Predicting Near-Term Changes in the Earth System: A Large Ensemble of Initialized Decadal
Prediction Simulations Using the Community Earth System Model in: Bulletin of the American …

Winter Arctic sea-ice concentration (SIC) decline plays an important role in Arctic
amplification which, in turn, influences Arctic ecosystems, midlatitude weather and climate …

The anthropogenically forced decline of Arctic sea ice is superimposed on strong internal
variability. Possible drivers for this variability include fluctuations in surface albedo, clouds …

Abstract The Arctic Ocean is strongly stratified by salinity in the uppermost layers. This
stratification is a key attribute of the region as it acts as an effective barrier for the vertical …

Decline in winter sea-ice concentration (SIC) in the Barents-Kara Sea significantly impacts
climate through increased heat release to the atmosphere. However, the past Barents-Kara …

Arctic sea ice loss has become a symbol of ongoing climate change, yet climate models still
struggle to reproduce it accurately, let alone predict it. A reason for this is the increasingly …

Abstract The Dansgaard-Oeschger events of the last ice age are among the best studied
abrupt climate changes, yet a comprehensive explanation is still lacking. They are most …