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...
| Main Author: | |
|---|---|
| Format: | Text |
| Language: | unknown |
| Published: |
DigitalCommons@USU
2017
|
| Subjects: | |
| 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. |
|---|