This paper highlights preliminary results from the analysis of the first year's data from the multi-channel scanning microwave radiometer (MSMR) onboard India's Oceansat-1 satellite, over the climatologically and geologically important Antarctic and Southern Ocean regions. Weekly averaged microwave brightness temperature images formed using the MSMR data clearly demarcated open water and sea ice regions. Different levels of ice concentration also showed up as different brightness temperature values. Signatures of several large and prominent continental features like the Trans-Antarctic Mountain ranges, Gamburtsev sub-glacial mountain, Wilkes and Aurora sub-glacial basins and the Ross Ice Shelf were seen in these images. Some quasi-circular ...
Antarctic Sea Ice Processes and Climate (ASPeCt) visual ship-based observations were conducted in th...
Three mesocyclones (MCs) over the Russian (Eastern) Arctic are investigated using multispectral sate...
Discrimination of the sea ice edge is done using the microwave 50.3 GHz brightness temperature measu...
This paper discusses the features observed over the Antarctic in the passive microwave emission reg...
Space-based passive microwave radiometers have been used to monitor southern ocean sea ice character...
The ice covered regions of the polar seas influence the global climate in several ways. Any perturba...
Data from the Electrically Scanning Microwave Radiometer (ESMR) on the Nimbus 5 satellite are used t...
We describe some features of Antarctic sea ice using the Multispectral Electronic Self Scanning Radi...
The recently developed Bristol passive-microwave-satellite algorithm for deriving sea-ice concentrat...
The recently developed Bristol passive-microwave-satellite algorithm for deriving sea-ice concentrat...
Airborne observations of 19.35 GHz microwave radiation were taken over the sea ice and firn cover of...
Large changes in the sea ice cover have been observed recently. Because of the relevance of such cha...
The growth of the Weddell Sea ice cover in 1980 is examined, using Nimbus-7 satellite Scanning Multi...
Copyright © 2013 Praveen Rao Teleti, Alvarinho J. Luis. This is an open access article distributed u...
In polar regions, interactions between atmosphere and ocean are strongly influenced by presence/abse...
Antarctic Sea Ice Processes and Climate (ASPeCt) visual ship-based observations were conducted in th...
Three mesocyclones (MCs) over the Russian (Eastern) Arctic are investigated using multispectral sate...
Discrimination of the sea ice edge is done using the microwave 50.3 GHz brightness temperature measu...
This paper discusses the features observed over the Antarctic in the passive microwave emission reg...
Space-based passive microwave radiometers have been used to monitor southern ocean sea ice character...
The ice covered regions of the polar seas influence the global climate in several ways. Any perturba...
Data from the Electrically Scanning Microwave Radiometer (ESMR) on the Nimbus 5 satellite are used t...
We describe some features of Antarctic sea ice using the Multispectral Electronic Self Scanning Radi...
The recently developed Bristol passive-microwave-satellite algorithm for deriving sea-ice concentrat...
The recently developed Bristol passive-microwave-satellite algorithm for deriving sea-ice concentrat...
Airborne observations of 19.35 GHz microwave radiation were taken over the sea ice and firn cover of...
Large changes in the sea ice cover have been observed recently. Because of the relevance of such cha...
The growth of the Weddell Sea ice cover in 1980 is examined, using Nimbus-7 satellite Scanning Multi...
Copyright © 2013 Praveen Rao Teleti, Alvarinho J. Luis. This is an open access article distributed u...
In polar regions, interactions between atmosphere and ocean are strongly influenced by presence/abse...
Antarctic Sea Ice Processes and Climate (ASPeCt) visual ship-based observations were conducted in th...
Three mesocyclones (MCs) over the Russian (Eastern) Arctic are investigated using multispectral sate...
Discrimination of the sea ice edge is done using the microwave 50.3 GHz brightness temperature measu...