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Cloud patterns in the Bering Sea
This page contains archived content and is no longer being updated. At the time of publication, it represented the best available science. However, more recent observations and studies may have rendered some content obsolete.
The Aleutian Islands seem to be dividing two large weather systems in this Moderate Resolution Imaging Spectroradiometer (MODIS) image, collected on January 21, 2006, by NASA’s Terra satellite. The clouds define the lines of high and low air pressure as well as any weather map. In the top of the image, the clouds circle clockwise around a high-pressure system in an anticyclone, while a cyclone in the bottom section of the image swirls counter-clockwise around a low-pressure system. The center of the anticyclone contains air that is under high pressure, so air entering the system is pushed down and out, away from the center. The spin of the Earth sends this air into a clock-wise circle. In this image, only the bottom half of the anticyclone, where the air flows over open water and clouds form, is clearly visible.
A cyclone, by contrast, rotates around the center of a low-pressure system. In this case, air rises as it rushes into the area of low pressure. The opposite direction of this movement (up and in instead of down and out) means that the air is pulled into a counter-clockwise rotation around the center. Anticyclones usually bring fair weather, while cyclones carry rain and strong winds. Both cyclones and anticyclones are common in the Arctic during the winter. Their formation is driven by temperature differences between the frigid, frozen land and the warmer ocean. The cyclone seen here is a semi-permanent feature called the Aleutian Low. To read more, see the Arctic Climatology and Meteorology Primer published by the National Snow and Ice Data Center.