The Weddell Sea Anomaly
The Weddell Sea Anomaly refers to a recurrent feature of the summertime Southern Hemisphere mid-latitude to high-latitude ionosphere, where electron densities have been observed to maximize around the Weddell Sea Region (which is about 50°S latitude and 95°W longitude) during the night, rather than...
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Format: | Text |
Language: | unknown |
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DigitalCommons@USU
2017
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Online Access: | https://digitalcommons.usu.edu/researchweek/ResearchWeek2017/Session5Poster/30 |
Summary: | The Weddell Sea Anomaly refers to a recurrent feature of the summertime Southern Hemisphere mid-latitude to high-latitude ionosphere, where electron densities have been observed to maximize around the Weddell Sea Region (which is about 50°S latitude and 95°W longitude) during the night, rather than during the day as would be expected. |
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