The variability of sea ice motion in Antarcic
Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Kim, Chang-Sin | - |
| dc.contributor.author | Kim, Hyun-cheol | - |
| dc.contributor.author | Kim, Tae-Wan | - |
| dc.date.issued | 2014 | - |
| dc.identifier.uri | https://repository.kopri.re.kr/handle/201206/7094 | - |
| dc.description.abstract | We used a simplified linear formula to understand the relationship between the ice motion and wind as Kimura(2004). These previous study was evaluated relationship using speed reduction factor and turning angle in the Southern Ocean. We use the two types gridded daily sea ice products by the NSIDC | - |
| dc.description.abstract | Sea ice concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave DAta and se ice motion from Polar Pathfinder Daily 25km EASE-Grid sea ice motion vectors. Satellite-observed sea ice data was compared with ERA interim reanalysis wind data. In this study, we evaluate the variability of the sea ice concentration and motion in the Southern Ocean in order to investigate the effects of wind on the spatial and temporal variability of the sea ice motion. | - |
| dc.language | English | - |
| dc.title | The variability of sea ice motion in Antarcic | - |
| dc.title.alternative | The variability of sea ice motion in Antarcic | - |
| dc.type | Poster | - |
| dc.identifier.bibliographicCitation | Kim, Chang-Sin, Kim, Hyun-cheol, Kim, Tae-Wan. 2014. The variability of sea ice motion in Antarcic. 2014 AGU (American Ceophysical Union) FALL MEETING. San Francisco. 2014.12.15~2014.12.19. | - |
| dc.citation.conferenceDate | 2014.12.15~2014.12.19 | - |
| dc.citation.conferenceName | 2014 AGU (American Ceophysical Union) FALL MEETING | - |
| dc.citation.conferencePlace | San Francisco | - |
| dc.description.articleClassification | 포스터 | - |
| dc.identifier.localId | 2014-0250 | - |
- Appears in Collections
- 2014-2016, SaTellite Remote Sensing on West Antarctic Ocean Research (STAR) (14-16) / Kim; Hyun-cheol (PE14040; PE15040; PE16040)
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