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Looking for facts and information? See About the Cryosphere.
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Weather and climate patterns in the Arctic can influence weather and climate around the world, particularly in the Northern Hemisphere.
The Arctic region acts as a heat sink for the Earth: the Arctic loses more heat to space than it absorbs from the sun's rays. In contrast, lower latitudes get more heat from the sun than they lose to space. Warm air and water move into the Arctic from tropical and temperate regions, and cold air and water moves from the Arctic into lower latitudes; the constant movement of air is reflected in day to day changes in weather patterns. Over a whole year, and looking at the globe as a whole, the heat gain in lower latitudes gets balanced out, on average, by heat loss in the polar regions.
When a winter snowstorm or cold snap hits temperate regions, people sometimes refer to the frigid temperatures as "Arctic." Cold air does in fact move from the Arctic into other regions, just as warm air from the south moves into polar regions. Storms tend to form at the boundaries between cold and warm air. Cold air moving down from the north is experienced as a cold front. Arctic blizzards can cause whiteouts, making life for people and animals difficult.
Some recent studies have argued that long-term changes in Arctic sea ice and climate may have impacts on weather patterns in other parts of the world, but so far the research remains largely inconclusive.
Last updated: 4 May 2020
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