Use of microwave radar data to interpret physical properties of ice and snow on the Greenland ice sheet

In situ observations of microwave radar backscatter were made at Dye-2 in south-central Greenland in 1993. Simultaneous observations of snow and ice physical properties were also acquired. Early in the season, it was found that 20° backscatter from the snow surface was determined mainly by the snow...

Full description

Bibliographic Details
Main Author: Gero, Christopher M., 1973-
Other Authors: Jezek, Kenneth C.
Format: Thesis
Language:English
Published: The Ohio State University 1995
Subjects:
Online Access:http://hdl.handle.net/1811/75895
id ftohiostateu:oai:kb.osu.edu:1811/75895
record_format openpolar
spelling ftohiostateu:oai:kb.osu.edu:1811/75895 2023-05-15T16:26:57+02:00 Use of microwave radar data to interpret physical properties of ice and snow on the Greenland ice sheet Gero, Christopher M., 1973- Jezek, Kenneth C. 1995-06 application/pdf http://hdl.handle.net/1811/75895 en_US eng The Ohio State University The Ohio State University. Department of Geological Sciences Senior Theses; 1995 http://hdl.handle.net/1811/75895 Thesis 1995 ftohiostateu 2020-08-22T19:19:27Z In situ observations of microwave radar backscatter were made at Dye-2 in south-central Greenland in 1993. Simultaneous observations of snow and ice physical properties were also acquired. Early in the season, it was found that 20° backscatter from the snow surface was determined mainly by the snow surface roughness. Later in the season the backscatter increases when temperatures are low. We attribute this fact to enhanced scattering from the ice within the radar resolution cell at the surface. This ice formed during the field season as a result of percolation and refreezing of surface meltwater. These observations have a direct implication for interpreting spaceborne SAR data acquired seasonally. No embargo Thesis Greenland Ice Sheet Ohio State University (OSU): Knowledge Bank Greenland
institution Open Polar
collection Ohio State University (OSU): Knowledge Bank
op_collection_id ftohiostateu
language English
description In situ observations of microwave radar backscatter were made at Dye-2 in south-central Greenland in 1993. Simultaneous observations of snow and ice physical properties were also acquired. Early in the season, it was found that 20° backscatter from the snow surface was determined mainly by the snow surface roughness. Later in the season the backscatter increases when temperatures are low. We attribute this fact to enhanced scattering from the ice within the radar resolution cell at the surface. This ice formed during the field season as a result of percolation and refreezing of surface meltwater. These observations have a direct implication for interpreting spaceborne SAR data acquired seasonally. No embargo
author2 Jezek, Kenneth C.
format Thesis
author Gero, Christopher M., 1973-
spellingShingle Gero, Christopher M., 1973-
Use of microwave radar data to interpret physical properties of ice and snow on the Greenland ice sheet
author_facet Gero, Christopher M., 1973-
author_sort Gero, Christopher M., 1973-
title Use of microwave radar data to interpret physical properties of ice and snow on the Greenland ice sheet
title_short Use of microwave radar data to interpret physical properties of ice and snow on the Greenland ice sheet
title_full Use of microwave radar data to interpret physical properties of ice and snow on the Greenland ice sheet
title_fullStr Use of microwave radar data to interpret physical properties of ice and snow on the Greenland ice sheet
title_full_unstemmed Use of microwave radar data to interpret physical properties of ice and snow on the Greenland ice sheet
title_sort use of microwave radar data to interpret physical properties of ice and snow on the greenland ice sheet
publisher The Ohio State University
publishDate 1995
url http://hdl.handle.net/1811/75895
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_relation The Ohio State University. Department of Geological Sciences Senior Theses; 1995
http://hdl.handle.net/1811/75895
_version_ 1766015972728111104