Add to ORKGThe purpose of this study is to investigate sea ice distribution off Queen Maud Land on the basis of NOAA AVHRR data received from 1987 to 1989 at Syowa Station. These data are very useful for examining the mesoscale phenomena. There are several characteristics such as coastal polynyas and sea ice eddies in the image. A coastal polynya was observed along the shelf break. Sea ice eddies were found at the ice edge which is located 60-200km off the Antarctic coast from December to February. These eddies are characterized by horizontal scale of 30-50km and small propagation of a few cm/s westward
We describe some features of Antarctic sea ice using the Multispectral Electronic Self Scanning Radi...
Antarctic coastal polynyas are very high sea-ice production areas. The resultant large amount of bri...
This study deals with observations and simulations of the evolution of coastal polynias focusing on ...
Characteristics of sea ice drift off Queen Maud Land are described on the basis of the Argos buoy de...
Mesoscale ice-ocean features off Syowa Station are examined using NOAA advanced very high resolution...
Discrimination of the sea ice edge is done using the microwave 50.3 GHz brightness temperature measu...
The different channels of the NOAA-AVHRR (National Oceanic and Atmospheric Administration-Advanced V...
In a coastal region where strong offshore winds and currents prevail, newly-formed sea ice is remove...
Data on surface features collected by the Japanese Antarctic Research Expedition (JARE) along traver...
International audienceThe image presented in this study is a mosaic showing the Barents and Kara sea...
The ice covered regions of the polar seas influence the global climate in several ways. Any perturba...
The growth of the Weddell Sea ice cover in 1980 is examined, using Nimbus-7 satellite Scanning Multi...
Antarctic coastal polynyas are very high sea-ice production areas. The resultant large amount of bri...
We drilled an ice core at the top of the coastal Derwael Ice Rise, Dronning Maud Land, Antarctica. T...
The data are approximately 800 km of airborne electromagnetic survey of coastal sea ice and sub-ice ...
We describe some features of Antarctic sea ice using the Multispectral Electronic Self Scanning Radi...
Antarctic coastal polynyas are very high sea-ice production areas. The resultant large amount of bri...
This study deals with observations and simulations of the evolution of coastal polynias focusing on ...
Characteristics of sea ice drift off Queen Maud Land are described on the basis of the Argos buoy de...
Mesoscale ice-ocean features off Syowa Station are examined using NOAA advanced very high resolution...
Discrimination of the sea ice edge is done using the microwave 50.3 GHz brightness temperature measu...
The different channels of the NOAA-AVHRR (National Oceanic and Atmospheric Administration-Advanced V...
In a coastal region where strong offshore winds and currents prevail, newly-formed sea ice is remove...
Data on surface features collected by the Japanese Antarctic Research Expedition (JARE) along traver...
International audienceThe image presented in this study is a mosaic showing the Barents and Kara sea...
The ice covered regions of the polar seas influence the global climate in several ways. Any perturba...
The growth of the Weddell Sea ice cover in 1980 is examined, using Nimbus-7 satellite Scanning Multi...
Antarctic coastal polynyas are very high sea-ice production areas. The resultant large amount of bri...
We drilled an ice core at the top of the coastal Derwael Ice Rise, Dronning Maud Land, Antarctica. T...
The data are approximately 800 km of airborne electromagnetic survey of coastal sea ice and sub-ice ...
We describe some features of Antarctic sea ice using the Multispectral Electronic Self Scanning Radi...
Antarctic coastal polynyas are very high sea-ice production areas. The resultant large amount of bri...
This study deals with observations and simulations of the evolution of coastal polynias focusing on ...