Snowmelt characterization from optical and synthetic-aperture radar observations in the La Joie Basin, British Columbia
<p>Snowmelt runoff serves both human needs and ecosystem services and is an important parameter in operational forecasting systems. Sentinel-1 synthetic-aperture-radar (SAR) observations can estimate the timing of melt within a snowpack; however, these estimates have not been applied on large...
| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2023-04-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/17/1457/2023/tc-17-1457-2023.pdf |
| _version_ | 1797852077931626496 |
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| author | S. E. Darychuk J. M. Shea B. Menounos B. Menounos A. Chesnokova G. Jost F. Weber |
| author_facet | S. E. Darychuk J. M. Shea B. Menounos B. Menounos A. Chesnokova G. Jost F. Weber |
| author_sort | S. E. Darychuk |
| collection | DOAJ |
| description | <p>Snowmelt runoff serves both human needs and ecosystem services and is an important parameter in operational forecasting systems. Sentinel-1
synthetic-aperture-radar (SAR) observations can estimate the timing of melt within a snowpack; however, these estimates have not been applied on
large spatial scales. Here we present a workflow to combine Sentinel-1 SAR and optical data from Landsat-8 and Sentinel-2 to estimate the onset and
duration of snowmelt in the La Joie Basin, a 985 <span class="inline-formula">km<sup>2</sup></span> watershed in the southern Coast Mountains of British Columbia. A backscatter threshold is used to
infer the point at which snowpack saturation occurs and the snowpack begins to produce runoff. Multispectral imagery is used to estimate snow-free
dates across the basin to define the end of the snowmelt period. SAR estimates of snowmelt onset form consistent trends in terms of elevation and aspect on
the watershed scale and reflect snowmelt records from continuous snow water equivalence observations. SAR estimates of snowpack saturation are most
effective on moderate to low slopes (<span class="inline-formula"><</span> 30<span class="inline-formula"><sup>∘</sup></span>) in open areas. The accuracy of snowmelt duration is reduced due to persistent cloud cover in
optical imagery. Despite these challenges, snowmelt duration agrees with trends in snow depths observed in the La Joie Basin. This approach has high
potential for adaptability to other alpine regions and can provide estimates of snowmelt timing in ungauged basins.</p> |
| first_indexed | 2024-04-09T19:28:11Z |
| format | Article |
| id | doaj.art-c97eb8c4415242e38c56ce57154ce536 |
| institution | Directory Open Access Journal |
| issn | 1994-0416 1994-0424 |
| language | English |
| last_indexed | 2024-04-09T19:28:11Z |
| publishDate | 2023-04-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | The Cryosphere |
| spelling | doaj.art-c97eb8c4415242e38c56ce57154ce5362023-04-05T06:43:09ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242023-04-01171457147310.5194/tc-17-1457-2023Snowmelt characterization from optical and synthetic-aperture radar observations in the La Joie Basin, British ColumbiaS. E. Darychuk0J. M. Shea1B. Menounos2B. Menounos3A. Chesnokova4G. Jost5F. Weber6Department of Geography, Earth and Environmental Sciences, University of Northern British Columbia, Prince George, British Colombia, V2N 4Z9, CanadaDepartment of Geography, Earth and Environmental Sciences, University of Northern British Columbia, Prince George, British Colombia, V2N 4Z9, CanadaDepartment of Geography, Earth and Environmental Sciences, University of Northern British Columbia, Prince George, British Colombia, V2N 4Z9, CanadaHakai Institute, Campbell River, British Columbia, V9W 0B7, CanadaDepartment of Geography, Earth and Environmental Sciences, University of Northern British Columbia, Prince George, British Colombia, V2N 4Z9, CanadaBC Hydro, Burnaby, British Columbia, V3N 4X8, CanadaBC Hydro, Burnaby, British Columbia, V3N 4X8, Canada<p>Snowmelt runoff serves both human needs and ecosystem services and is an important parameter in operational forecasting systems. Sentinel-1 synthetic-aperture-radar (SAR) observations can estimate the timing of melt within a snowpack; however, these estimates have not been applied on large spatial scales. Here we present a workflow to combine Sentinel-1 SAR and optical data from Landsat-8 and Sentinel-2 to estimate the onset and duration of snowmelt in the La Joie Basin, a 985 <span class="inline-formula">km<sup>2</sup></span> watershed in the southern Coast Mountains of British Columbia. A backscatter threshold is used to infer the point at which snowpack saturation occurs and the snowpack begins to produce runoff. Multispectral imagery is used to estimate snow-free dates across the basin to define the end of the snowmelt period. SAR estimates of snowmelt onset form consistent trends in terms of elevation and aspect on the watershed scale and reflect snowmelt records from continuous snow water equivalence observations. SAR estimates of snowpack saturation are most effective on moderate to low slopes (<span class="inline-formula"><</span> 30<span class="inline-formula"><sup>∘</sup></span>) in open areas. The accuracy of snowmelt duration is reduced due to persistent cloud cover in optical imagery. Despite these challenges, snowmelt duration agrees with trends in snow depths observed in the La Joie Basin. This approach has high potential for adaptability to other alpine regions and can provide estimates of snowmelt timing in ungauged basins.</p>https://tc.copernicus.org/articles/17/1457/2023/tc-17-1457-2023.pdf |
| spellingShingle | S. E. Darychuk J. M. Shea B. Menounos B. Menounos A. Chesnokova G. Jost F. Weber Snowmelt characterization from optical and synthetic-aperture radar observations in the La Joie Basin, British Columbia The Cryosphere |
| title | Snowmelt characterization from optical and synthetic-aperture radar observations in the La Joie Basin, British Columbia |
| title_full | Snowmelt characterization from optical and synthetic-aperture radar observations in the La Joie Basin, British Columbia |
| title_fullStr | Snowmelt characterization from optical and synthetic-aperture radar observations in the La Joie Basin, British Columbia |
| title_full_unstemmed | Snowmelt characterization from optical and synthetic-aperture radar observations in the La Joie Basin, British Columbia |
| title_short | Snowmelt characterization from optical and synthetic-aperture radar observations in the La Joie Basin, British Columbia |
| title_sort | snowmelt characterization from optical and synthetic aperture radar observations in the la joie basin british columbia |
| url | https://tc.copernicus.org/articles/17/1457/2023/tc-17-1457-2023.pdf |
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