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Observation of flooded ice in Arctic regions

The remote detection of flooding in the Arctic ice pack has been difficult to accomplish using conventional techniques. We have examined a case of Artie flooding (8 June 1989) with NOAA and DMSP visible and infrared measurements supplemented by DMSP microwave imager (SSM/I) data. Analysis of visible...

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Published in:International journal of remote sensing 1993, Vol.14 (7), p.1305-1324
Main Authors: GOROCH, A. K., FETT, R. W.
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Language:English
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description The remote detection of flooding in the Arctic ice pack has been difficult to accomplish using conventional techniques. We have examined a case of Artie flooding (8 June 1989) with NOAA and DMSP visible and infrared measurements supplemented by DMSP microwave imager (SSM/I) data. Analysis of visible and infrared data for a sunglint region was used to show the distribution of flooding at 72° N, 135° W. A simple model was developed for the radiative transfer at microwave wavelengths through a bring layer over ice. The predictions of the model were found to be consistent with the spatial behaviour of the SSM/I measurements. This case study demonstrates the usefulness of using combine visible, infrared, and microwave measurements to differentiate among flooded, broken ice, and open water regions, even in the presence of cloud cover or surface fog Formerly Naval Oceanographic and Atmospheric Research Laboratory
doi_str_mv 10.1080/01431169308953958
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ispartof International journal of remote sensing, 1993, Vol.14 (7), p.1305-1324
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source Taylor & Francis Engineering, Computing & Technology Archive
subjects Earth, ocean, space
Exact sciences and technology
External geophysics
Floods
Ice
Marine
Mathematical models
Q1
Snow. Ice. Glaciers
title Observation of flooded ice in Arctic regions
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