Warming amplification over the Arctic Pole (AP hereafter) and Third Pole (Tibetan Plateau,
TP hereafter) can trigger a series of climate responses and have global consequences …

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 …

The Arctic is warming at a rate twice the global average and severe winter weather is
reported to be increasing across many heavily populated mid-latitude regions, but there is …

This chapter assesses the state of physical, biological and social knowledge concerning the
Arctic and Antarctic ocean and cryosphere, how they are affected by climate change, and …

The possibility that Arctic sea ice loss weakens mid-latitude westerlies, promoting more
severe cold winters, has sparked more than a decade of scientific debate, with apparent …

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 article provides a synthesis of the latest observational trends and projections for the
future of the Arctic. First, the Arctic is already changing rapidly as a result of climate change …

Northern midlatitudes, over central Eurasia in particular, have experienced frequent severe
winters in recent decades,–. A remote influence of Arctic sea-ice loss has been …

Recent boreal winters have exhibited a large-scale seesaw temperature pattern
characterized by an unusually warm Arctic and cold continents. Whether there is any …

The threat posed by invasive non-native species worldwide requires a global approach to
identify which introduced species are likely to pose an elevated risk of impact to native …