Microwave Determination of Snowpack Liquid Water Content.
The measurement of liquid water in snowpack based on the electrical path length difference in snowpack depth in the region of high dielectric dispersion of water is described. The measurement system consists of a previously described LFM/CW microwave system (Ellerbruck and Boyne, 1980) operating at...
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ftdtic:ADA161798 2023-05-15T16:37:50+02:00 Microwave Determination of Snowpack Liquid Water Content. Boyne,H S COLORADO STATE UNIV FORT COLLINS DEPT OF EARTH RESOURCES 1985-09-15 text/html http://www.dtic.mil/docs/citations/ADA161798 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA161798 en eng http://www.dtic.mil/docs/citations/ADA161798 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Test Facilities Equipment and Methods *SNOW MEASUREMENT VOLUME PERMEABILITY LABORATORY TESTS LAYERS LIQUIDS WATER CONTINUOUS WAVES FIELD TESTS DIELECTRICS PATHS TEST METHODS ACCURACY MICROWAVES MICROWAVE EQUIPMENT ELECTRICAL PROPERTIES MOISTURE CONTENT DEPTH STRATIGRAPHY DIELECTRIC PROPERTIES LENGTH HETEROGENEITY DILUTION DETERMINATION MICROWAVE FREQUENCY DISPERSIONS Snowpack water content Text 1985 ftdtic 2016-02-21T01:10:28Z The measurement of liquid water in snowpack based on the electrical path length difference in snowpack depth in the region of high dielectric dispersion of water is described. The measurement system consists of a previously described LFM/CW microwave system (Ellerbruck and Boyne, 1980) operating at two frequency bands 2-5 GHz and 5-8 GHz. The system is tested, evaluated and intercompared with a dilution measurement technique (Davis, et. al. 1985) in both a laboratory and field environment. It is found that the two methods of intercomparison are equivalent provided the snowpack is homogeneous and free of stratigraphy. The accuracy of the intercomparison is + or - 2.5% at the 95% level of confidence. The intercomparison of the methods is not equivalent when compared in an inhomegeneous stratified snowpack. The microwave system consistently registers a higher volumetric liquid water content than the dilution method. This discrepancy is believed due to differences in the snowpack volumes sampled. In particular, it is believed that ponded water above impermeable layers regions in the snowpack is responsible for the discrepancy. These regions could not be cored successfully for measurement by the dilution method. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Test Facilities Equipment and Methods *SNOW MEASUREMENT VOLUME PERMEABILITY LABORATORY TESTS LAYERS LIQUIDS WATER CONTINUOUS WAVES FIELD TESTS DIELECTRICS PATHS TEST METHODS ACCURACY MICROWAVES MICROWAVE EQUIPMENT ELECTRICAL PROPERTIES MOISTURE CONTENT DEPTH STRATIGRAPHY DIELECTRIC PROPERTIES LENGTH HETEROGENEITY DILUTION DETERMINATION MICROWAVE FREQUENCY DISPERSIONS Snowpack water content |
spellingShingle |
Snow Ice and Permafrost Test Facilities Equipment and Methods *SNOW MEASUREMENT VOLUME PERMEABILITY LABORATORY TESTS LAYERS LIQUIDS WATER CONTINUOUS WAVES FIELD TESTS DIELECTRICS PATHS TEST METHODS ACCURACY MICROWAVES MICROWAVE EQUIPMENT ELECTRICAL PROPERTIES MOISTURE CONTENT DEPTH STRATIGRAPHY DIELECTRIC PROPERTIES LENGTH HETEROGENEITY DILUTION DETERMINATION MICROWAVE FREQUENCY DISPERSIONS Snowpack water content Boyne,H S Microwave Determination of Snowpack Liquid Water Content. |
topic_facet |
Snow Ice and Permafrost Test Facilities Equipment and Methods *SNOW MEASUREMENT VOLUME PERMEABILITY LABORATORY TESTS LAYERS LIQUIDS WATER CONTINUOUS WAVES FIELD TESTS DIELECTRICS PATHS TEST METHODS ACCURACY MICROWAVES MICROWAVE EQUIPMENT ELECTRICAL PROPERTIES MOISTURE CONTENT DEPTH STRATIGRAPHY DIELECTRIC PROPERTIES LENGTH HETEROGENEITY DILUTION DETERMINATION MICROWAVE FREQUENCY DISPERSIONS Snowpack water content |
description |
The measurement of liquid water in snowpack based on the electrical path length difference in snowpack depth in the region of high dielectric dispersion of water is described. The measurement system consists of a previously described LFM/CW microwave system (Ellerbruck and Boyne, 1980) operating at two frequency bands 2-5 GHz and 5-8 GHz. The system is tested, evaluated and intercompared with a dilution measurement technique (Davis, et. al. 1985) in both a laboratory and field environment. It is found that the two methods of intercomparison are equivalent provided the snowpack is homogeneous and free of stratigraphy. The accuracy of the intercomparison is + or - 2.5% at the 95% level of confidence. The intercomparison of the methods is not equivalent when compared in an inhomegeneous stratified snowpack. The microwave system consistently registers a higher volumetric liquid water content than the dilution method. This discrepancy is believed due to differences in the snowpack volumes sampled. In particular, it is believed that ponded water above impermeable layers regions in the snowpack is responsible for the discrepancy. These regions could not be cored successfully for measurement by the dilution method. (Author) |
author2 |
COLORADO STATE UNIV FORT COLLINS DEPT OF EARTH RESOURCES |
format |
Text |
author |
Boyne,H S |
author_facet |
Boyne,H S |
author_sort |
Boyne,H S |
title |
Microwave Determination of Snowpack Liquid Water Content. |
title_short |
Microwave Determination of Snowpack Liquid Water Content. |
title_full |
Microwave Determination of Snowpack Liquid Water Content. |
title_fullStr |
Microwave Determination of Snowpack Liquid Water Content. |
title_full_unstemmed |
Microwave Determination of Snowpack Liquid Water Content. |
title_sort |
microwave determination of snowpack liquid water content. |
publishDate |
1985 |
url |
http://www.dtic.mil/docs/citations/ADA161798 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA161798 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA161798 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766028138100293632 |