Estimation of regional snowline elevation (RSLE) from MODIS images for seasonally snow covered mountain basins

•Snowline estimation from satellite data in seasonally snow covered mountain basins.•Minimizing the sum of snow covered pixels below and land pixels above the snowline.•Tested with MODIS daily snow product in the highest part of the Carpathians.•The method is more accurate than the previously used m...

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Veröffentlicht in:Journal of hydrology (Amsterdam) 2014-11, Vol.519, p.1769-1778
Hauptverfasser: Krajčí, Pavel, Holko, Ladislav, Perdigão, Rui A.P., Parajka, Juraj
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container_issue
container_start_page 1769
container_title Journal of hydrology (Amsterdam)
container_volume 519
creator Krajčí, Pavel
Holko, Ladislav
Perdigão, Rui A.P.
Parajka, Juraj
description •Snowline estimation from satellite data in seasonally snow covered mountain basins.•Minimizing the sum of snow covered pixels below and land pixels above the snowline.•Tested with MODIS daily snow product in the highest part of the Carpathians.•The method is more accurate than the previously used methods. We present a method for estimation of regional snowline elevation (RSLE) from satellite data for seasonally snow covered mountain basins. The methodology is based on finding an elevation for which the sum of snow covered pixels below and land pixels above the RSLE is minimized for each day. The methodology is tested with MODIS daily snow cover product in the period 2000–2013 in the upper Váh basin (Slovakia). The accuracy is evaluated by daily snow depth measurements at seven climate stations and additional snow course measurements at 16 profiles in the period 2000–2013. The results show that RSLE allows accurate estimation of snowline elevation. For the RSLE estimation, two thresholds need to be considered. The thresholds of maximum cloud coverage and minimum number of snow pixels considerably affect the number of days (images) available for estimation. The sensitivity evaluation indicates that the cloud threshold has less effect on the accuracy than the minimum snow threshold. Setting cloud and minimum snow thresholds to 70% and 5% respectively, results in an average RSLE estimation accuracy of 86% at climate stations. The accuracy in the forest is 92% in the winter months and drops to 70% in April. The main factors that control the accuracy and scatter around the snowline are vegetation cover and shading of terrain. The results show that spatial patterns of misclassification correspond well with forest cover and potential insolation duration in winter. The developed RSLE method is more accurate than the previously used methods of snowline elevation estimation, it decreases the scatter around the snowline and can be potentially applied in an improved cloud reduction in MODIS products as well.
doi_str_mv 10.1016/j.jhydrol.2014.08.064
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We present a method for estimation of regional snowline elevation (RSLE) from satellite data for seasonally snow covered mountain basins. The methodology is based on finding an elevation for which the sum of snow covered pixels below and land pixels above the RSLE is minimized for each day. The methodology is tested with MODIS daily snow cover product in the period 2000–2013 in the upper Váh basin (Slovakia). The accuracy is evaluated by daily snow depth measurements at seven climate stations and additional snow course measurements at 16 profiles in the period 2000–2013. The results show that RSLE allows accurate estimation of snowline elevation. For the RSLE estimation, two thresholds need to be considered. The thresholds of maximum cloud coverage and minimum number of snow pixels considerably affect the number of days (images) available for estimation. The sensitivity evaluation indicates that the cloud threshold has less effect on the accuracy than the minimum snow threshold. Setting cloud and minimum snow thresholds to 70% and 5% respectively, results in an average RSLE estimation accuracy of 86% at climate stations. The accuracy in the forest is 92% in the winter months and drops to 70% in April. The main factors that control the accuracy and scatter around the snowline are vegetation cover and shading of terrain. The results show that spatial patterns of misclassification correspond well with forest cover and potential insolation duration in winter. 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We present a method for estimation of regional snowline elevation (RSLE) from satellite data for seasonally snow covered mountain basins. The methodology is based on finding an elevation for which the sum of snow covered pixels below and land pixels above the RSLE is minimized for each day. The methodology is tested with MODIS daily snow cover product in the period 2000–2013 in the upper Váh basin (Slovakia). The accuracy is evaluated by daily snow depth measurements at seven climate stations and additional snow course measurements at 16 profiles in the period 2000–2013. The results show that RSLE allows accurate estimation of snowline elevation. For the RSLE estimation, two thresholds need to be considered. The thresholds of maximum cloud coverage and minimum number of snow pixels considerably affect the number of days (images) available for estimation. The sensitivity evaluation indicates that the cloud threshold has less effect on the accuracy than the minimum snow threshold. Setting cloud and minimum snow thresholds to 70% and 5% respectively, results in an average RSLE estimation accuracy of 86% at climate stations. The accuracy in the forest is 92% in the winter months and drops to 70% in April. The main factors that control the accuracy and scatter around the snowline are vegetation cover and shading of terrain. The results show that spatial patterns of misclassification correspond well with forest cover and potential insolation duration in winter. 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Glaciers</topic><topic>Thresholds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Krajčí, Pavel</creatorcontrib><creatorcontrib>Holko, Ladislav</creatorcontrib><creatorcontrib>Perdigão, Rui A.P.</creatorcontrib><creatorcontrib>Parajka, Juraj</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Journal of hydrology (Amsterdam)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Krajčí, Pavel</au><au>Holko, Ladislav</au><au>Perdigão, Rui A.P.</au><au>Parajka, Juraj</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Estimation of regional snowline elevation (RSLE) from MODIS images for seasonally snow covered mountain basins</atitle><jtitle>Journal of hydrology (Amsterdam)</jtitle><date>2014-11-27</date><risdate>2014</risdate><volume>519</volume><spage>1769</spage><epage>1778</epage><pages>1769-1778</pages><issn>0022-1694</issn><eissn>1879-2707</eissn><coden>JHYDA7</coden><abstract>•Snowline estimation from satellite data in seasonally snow covered mountain basins.•Minimizing the sum of snow covered pixels below and land pixels above the snowline.•Tested with MODIS daily snow product in the highest part of the Carpathians.•The method is more accurate than the previously used methods. We present a method for estimation of regional snowline elevation (RSLE) from satellite data for seasonally snow covered mountain basins. The methodology is based on finding an elevation for which the sum of snow covered pixels below and land pixels above the RSLE is minimized for each day. The methodology is tested with MODIS daily snow cover product in the period 2000–2013 in the upper Váh basin (Slovakia). The accuracy is evaluated by daily snow depth measurements at seven climate stations and additional snow course measurements at 16 profiles in the period 2000–2013. The results show that RSLE allows accurate estimation of snowline elevation. For the RSLE estimation, two thresholds need to be considered. The thresholds of maximum cloud coverage and minimum number of snow pixels considerably affect the number of days (images) available for estimation. The sensitivity evaluation indicates that the cloud threshold has less effect on the accuracy than the minimum snow threshold. 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source Elsevier ScienceDirect Journals Complete
subjects Applied geophysics
Basins
Carpathians
Clouds
Covering
Earth sciences
Earth, ocean, space
Elevation
Exact sciences and technology
External geophysics
Hydrology
Hydrology. Hydrogeology
Internal geophysics
MODIS
Mountains
Pixels
Regional snowline elevation
Snow
Snow cover
Snow. Ice. Glaciers
Thresholds
title Estimation of regional snowline elevation (RSLE) from MODIS images for seasonally snow covered mountain basins
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