Determination of actual snow-covered area using Landsat TM and digital elevation model data in Glacier National Park, Montana

Abstract In the future, data from the moderate resolution imaging spectroradiometer (MODIS) will be employed to map snow in an automated environment at a resolution of 250 m to 1 km. Using Landsat thematic mapper (TM) data, an algorithm, SNOMAP, has been developed to map snow-covered area. This algo...

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Published in:Polar Record
Main Authors: Hall, Dorothy K., Foster, James L., Chien, Janet Y.L., Riggs, George A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1995
Subjects:
Online Access:http://dx.doi.org/10.1017/s0032247400013693
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013693
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spelling crcambridgeupr:10.1017/s0032247400013693 2024-09-15T18:31:20+00:00 Determination of actual snow-covered area using Landsat TM and digital elevation model data in Glacier National Park, Montana Hall, Dorothy K. Foster, James L. Chien, Janet Y.L. Riggs, George A. 1995 http://dx.doi.org/10.1017/s0032247400013693 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013693 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 31, issue 177, page 191-198 ISSN 0032-2474 1475-3057 journal-article 1995 crcambridgeupr https://doi.org/10.1017/s0032247400013693 2024-08-07T04:03:33Z Abstract In the future, data from the moderate resolution imaging spectroradiometer (MODIS) will be employed to map snow in an automated environment at a resolution of 250 m to 1 km. Using Landsat thematic mapper (TM) data, an algorithm, SNOMAP, has been developed to map snow-covered area. This algorithm will be used, with appropriate modification, with MODIS data following the launch of the first Earth Observing System (EOS) platform in 1998. SNOMAP has been shown to be successful in mapping snow in a variety of areas using TM data. However, significant errors may be present in mountainous areas due to effects of topography. To increase the accuracy of mapping global snow-covered area in the future using MODIS data, digital elevation model (DEM) data have been registered to TM data for parts of Glacier National Park, Montana, so that snow cover on mountain slopes can be mapped. This paper shows that the use of DEM data registered to TM data increases the accuracy of mapping snow-covered area. Using SNOMAP on a subscene within the 14 March 1991 TM scene of northwestern Montana, 215 km 2 of snow is mapped when TM data are used alone to map the snow cover. We show that about 1062 km 2 of snow are actually present as measured when the TM and DEM data are registered. Approximately five times more snow is present when the effects of topography are considered for this subscene, which is in a rugged area in Glacier National Park. A simple model has been developed to determine the relationship between terrain relief and the amount of correction that must be applied to map actual snow-covered area in Glacier National Park using satellite data alone. Article in Journal/Newspaper Polar Record Cambridge University Press Polar Record 31 177 191 198
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract In the future, data from the moderate resolution imaging spectroradiometer (MODIS) will be employed to map snow in an automated environment at a resolution of 250 m to 1 km. Using Landsat thematic mapper (TM) data, an algorithm, SNOMAP, has been developed to map snow-covered area. This algorithm will be used, with appropriate modification, with MODIS data following the launch of the first Earth Observing System (EOS) platform in 1998. SNOMAP has been shown to be successful in mapping snow in a variety of areas using TM data. However, significant errors may be present in mountainous areas due to effects of topography. To increase the accuracy of mapping global snow-covered area in the future using MODIS data, digital elevation model (DEM) data have been registered to TM data for parts of Glacier National Park, Montana, so that snow cover on mountain slopes can be mapped. This paper shows that the use of DEM data registered to TM data increases the accuracy of mapping snow-covered area. Using SNOMAP on a subscene within the 14 March 1991 TM scene of northwestern Montana, 215 km 2 of snow is mapped when TM data are used alone to map the snow cover. We show that about 1062 km 2 of snow are actually present as measured when the TM and DEM data are registered. Approximately five times more snow is present when the effects of topography are considered for this subscene, which is in a rugged area in Glacier National Park. A simple model has been developed to determine the relationship between terrain relief and the amount of correction that must be applied to map actual snow-covered area in Glacier National Park using satellite data alone.
format Article in Journal/Newspaper
author Hall, Dorothy K.
Foster, James L.
Chien, Janet Y.L.
Riggs, George A.
spellingShingle Hall, Dorothy K.
Foster, James L.
Chien, Janet Y.L.
Riggs, George A.
Determination of actual snow-covered area using Landsat TM and digital elevation model data in Glacier National Park, Montana
author_facet Hall, Dorothy K.
Foster, James L.
Chien, Janet Y.L.
Riggs, George A.
author_sort Hall, Dorothy K.
title Determination of actual snow-covered area using Landsat TM and digital elevation model data in Glacier National Park, Montana
title_short Determination of actual snow-covered area using Landsat TM and digital elevation model data in Glacier National Park, Montana
title_full Determination of actual snow-covered area using Landsat TM and digital elevation model data in Glacier National Park, Montana
title_fullStr Determination of actual snow-covered area using Landsat TM and digital elevation model data in Glacier National Park, Montana
title_full_unstemmed Determination of actual snow-covered area using Landsat TM and digital elevation model data in Glacier National Park, Montana
title_sort determination of actual snow-covered area using landsat tm and digital elevation model data in glacier national park, montana
publisher Cambridge University Press (CUP)
publishDate 1995
url http://dx.doi.org/10.1017/s0032247400013693
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013693
genre Polar Record
genre_facet Polar Record
op_source Polar Record
volume 31, issue 177, page 191-198
ISSN 0032-2474 1475-3057
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0032247400013693
container_title Polar Record
container_volume 31
container_issue 177
container_start_page 191
op_container_end_page 198
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