KOPRI Repository

The variability of sea ice motion in Antarcic

Cited 0 time in wos
Cited 0 time in scopus
Metadata Downloads
The variability of sea ice motion in Antarcic
Kim, Chang-Sin
Kim, Tae-Wan
Kim, Hyun-cheol
Lee, SangHoon
Issue Date
Kim, Chang-Sin, et al. 2014. The variability of sea ice motion in Antarcic. 2014 AGU(American Geophysical Union) FALL MEETING. San Francisco. 2014.12.15.-19.
As well known, sea ice is a vital component in the marginal ice zone as well as the global climate system. Antarctic sea ice is reported to be sensitive to surface wind forcing. 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 National Snow and Ice Data Center (NSIDC) ; Sea Ice Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave Data and sea ice motion from Polar Pathfinder Daily 25 km 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. Moreover, we need to know the change in the sea ice motion in accordance with the sea ice characteristics in Antarctic.
Conference Name
2014 AGU(American Geophysical Union) FALL MEETING
Conference Place
San Francisco
Conference Date
Files in This Item
There are no files associated with this item.
General Conditions
      ROMEO Green
    Can archive pre-print and post-print or publisher's version/PDF
      ROMEO Blue
    Can archive post-print (ie final draft post-refereeing) or publisher's version/PDF
      ROMEO Yellow
    Can archive pre-print (ie pre-refereeing)
      ROMEO White
    Archiving not formally supported

    Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.