The approach to the DMSP SSMI (Defense Meteorological Satellite Program; Special Sensor Microwave Imager) sea-ice validation effort is to demonstrate a quantitative relationship between the SSMI-derived sea ice parameters and those same parameters derived from other data sets including visible and infrared satellite imagery, aerial photographic and high-resolution microwave aircraft imagery. The question to be addressed is to what accuracy (relative to these other observations) can the following ice parameters be determined: (1) position of the ice boundary; (2) total sea ice concentration; and (3) multiyear sea ice concentration. Specific tasks include: (1) a study of the interrelationship of surface information content and sensor spatial ...
The multi-year sea ice (MY) concentration as determined with the NASA Team algorithm (NTA) shows an ...
During March 1979, field operations were carried out in the Marginal Ice Zone (MIZ) of the Bering Se...
Sea ice is a very important component of the climate system. While the Arctic sea ice extent has ret...
The history of the program is described along with the SSM/I sensor, including its calibration and g...
This document addresses the task of developing and executing a plan for validating the algorithm use...
An intercalibration between F13 Special Sensor Microwave Imager (SSMI) and F17 Special Sensor Microw...
Existing SSM/I algorithms are imperfect at mapping total and partial ice concentrations. This paper ...
The United States National Ice Center (NIC) provides weekly ice analyses of the Arctic and Antarctic...
Sea ice concentrations, derived from passive microwave satellite sensor measurements, provide today ...
Data derived from the Nimbus 7 scanning multichannel microwave radiometer (SMMR) are discussed and t...
A new SSM/I algorithm is described that is based on near real-time data fusion with portions of oper...
An Arctic and Antarctic sea ice area and extent dataset has been generated by EUMETSAT's Ocean and ...
Preliminary results of sea ice and techniques for calculating sea ice concentration and multiyear fr...
The most consistent means of investigating the global sea ice cover is by satellite passive microwav...
New sea ice classifying algorithm based on the 85-GHz channel of DMSP SSM/I is developed for the Sea...
The multi-year sea ice (MY) concentration as determined with the NASA Team algorithm (NTA) shows an ...
During March 1979, field operations were carried out in the Marginal Ice Zone (MIZ) of the Bering Se...
Sea ice is a very important component of the climate system. While the Arctic sea ice extent has ret...
The history of the program is described along with the SSM/I sensor, including its calibration and g...
This document addresses the task of developing and executing a plan for validating the algorithm use...
An intercalibration between F13 Special Sensor Microwave Imager (SSMI) and F17 Special Sensor Microw...
Existing SSM/I algorithms are imperfect at mapping total and partial ice concentrations. This paper ...
The United States National Ice Center (NIC) provides weekly ice analyses of the Arctic and Antarctic...
Sea ice concentrations, derived from passive microwave satellite sensor measurements, provide today ...
Data derived from the Nimbus 7 scanning multichannel microwave radiometer (SMMR) are discussed and t...
A new SSM/I algorithm is described that is based on near real-time data fusion with portions of oper...
An Arctic and Antarctic sea ice area and extent dataset has been generated by EUMETSAT's Ocean and ...
Preliminary results of sea ice and techniques for calculating sea ice concentration and multiyear fr...
The most consistent means of investigating the global sea ice cover is by satellite passive microwav...
New sea ice classifying algorithm based on the 85-GHz channel of DMSP SSM/I is developed for the Sea...
The multi-year sea ice (MY) concentration as determined with the NASA Team algorithm (NTA) shows an ...
During March 1979, field operations were carried out in the Marginal Ice Zone (MIZ) of the Bering Se...
Sea ice is a very important component of the climate system. While the Arctic sea ice extent has ret...