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 …

Arctic Amplification is a fundamental feature of past, present, and modelled future climate.
However, the causes of this “amplification” within Earth's climate system are not fully …

Arctic amplification—the amplified surface warming in the Arctic relative to the globe—is a
robust feature of climate change. However, there is a considerable spread in the reported …

Observations show that reduced regional sea-ice cover is coincident with cold mid-latitude
winters on interannual timescales. However, it remains unclear whether these observed …

This paper examines the trajectories followed by intense intrusions of moist air into the Arctic
polar region during autumn and winter and their impact on local temperature and sea ice …

Recent rapid Arctic sea ice loss was documented as combined results from anthropogenic
forcing and climate system internal variability. However, the role of internal variability is not …

The role of transient Arctic sea ice loss in the projected greenhouse gas–induced late-
twentieth-to late-twenty-first-century climate change is investigated using the Geophysical …

Atmospheric rivers (ARs), intrusions of warm and moist air, can effectively drive weather
extremes over the Arctic and trigger subsequent impact on sea ice and climate. What …

The Arctic has been warming faster than elsewhere, especially during the cold season.
According to the leading theory, ice‐albedo feedback warms the Arctic Ocean during the …

Abstract Greenland Ice Sheet (GrIS) mass loss has accelerated since the turn of the twenty‐
first century. Several recent episodes of rapid GrIS ablation coincided with intense moisture …