The Arctic has warmed more than twice as fast as the global average since the late twentieth
century, a phenomenon known as Arctic amplification (AA). Recently, there have been …

Numerous components of the Arctic freshwater system (atmosphere, ocean, cryosphere, and
terrestrial hydrology) have experienced large changes over the past few decades, and these …

Arctic cyclone activity is investigated in the context of climate change and variability by using
a modified automated cyclone identification and tracking algorithm, which differs from …

Arctic climate system change has accelerated tremendously since the beginning of this
century, and a strikingly extreme sea‐ice loss occurred in summer 2007. However, the …

This paper identified an atmospheric circulation anomaly–dipole structure anomaly in the
Arctic atmosphere and its relationship with winter sea ice motion, based on the International …

The Fram Strait is very important with regard to heat and mass exchange in the Arctic Ocean,
and the large quantities of heat carried north by the West Spitsbergen Current (WSC) …

As the world warms, the expectation is that the freshwater outflows from the Arctic Ocean to
the North Atlantic will strengthen and may act to suppress the rate of the climatically …

Runoff from Arctic rivers constitutes a major freshwater influx to the Arctic Ocean. In these
nival-dominated river systems, the majority of annual discharge is released during the spring …

The sea ice simulations by the Intergovernmental Panel on Climate Change Fourth
Assessment Report (IPCC AR4) models for the climate of the twentieth century and for …

Two major oceanographic changes have recently propagated through several trophic levels
in coastal areas of Southeast Greenland (SEG). Firstly, the amount of drift‐ice exported from …