Atmospheric Moisture Transport and Arctic Sea Ice Decline

Global transport of moisture its effect on Arctic Sea Ice Extent (SIE).

The long‐term decline in the annual mean Arctic Sea Ice Extent (SIE) is one of the clearest indicators of climate change, and certainly one that generates more scientific and social concern than most. The environmental implications of the retreat of the Arctic ice are of great importance, and the study of its causes and consequences encompasses a very broad spectrum of disciplines, including atmospheric and oceanic sciences, ecology, marine biology, and even economics and energy resources.

A recent WIREs Climate Change review discusses the transport of moisture to the Arctic and its effect on SIE. The review includes a synthesis of our knowledge regarding the main sources supplying moisture to the Arctic, the changes experienced over the last few decades due to variations in the transport of moisture, the factors that control interannual variability, and the inherent contrast in the mechanisms related to the effect of changes in moisture transport on SIE in the Arctic.

Major modes of climate variability that affect the Arctic region and their configuration associated with the greater transport of moisture toward the Arctic system.

The precise identification of the moisture sources for the Arctic depends on both the definition of the Arctic region itself and the approach used to identify the sources, with remote regions over the extratropical Atlantic and Pacific Oceans being universally important, as are some continental areas over Siberia and North America.

This review reaffirms the absence of any clear agreement regarding the trends in atmospheric moisture transport to the Arctic, and highlights discrepancies between different data sets and approaches in the quantification of moisture transport, implying that its long-term impact on the intensification of the hydrological cycle in the Arctic remains unclear.

The authors confirm the influence of the major modes of climate variability, planetary circulation patterns, and changes in cyclonic activity in the variability of moisture transport to the Arctic and reaffirms that the effect of moisture transport on the Arctic SIE through changes in humidity, cloud cover, and precipitation is a complex scientific problem that requires detailed analysis over the decades to come.

Kindly contributed by the Authors.

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