Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheet
<p>Subarctic West Greenland is populated by thousands of seasonally ice-free lakes. Using remotely sensed observations, we analyse the surface water temperatures of six lakes during 1995–2022 to identify factors influencing their variability. The connectivity to the Greenland Ice Sheet (GrIS)...
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| Language: | English |
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Copernicus Publications
2025-08-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/19/3139/2025/tc-19-3139-2025.pdf |
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| author | L. Carrea C. J. Merchant C. J. Merchant R. I. Woolway N. McCarroll N. McCarroll |
| author_facet | L. Carrea C. J. Merchant C. J. Merchant R. I. Woolway N. McCarroll N. McCarroll |
| author_sort | L. Carrea |
| collection | DOAJ |
| description | <p>Subarctic West Greenland is populated by thousands of seasonally ice-free lakes. Using remotely sensed observations, we analyse the surface water temperatures of six lakes during 1995–2022 to identify factors influencing their variability. The connectivity to the Greenland Ice Sheet (GrIS) has a clear influence on lake surface temperature, with ice-sheet-marginal lakes experiencing smaller average summer maximum temperature (<span class="inline-formula"><6</span> <span class="inline-formula">°C</span>) and minimal interannual variability. A lake fed by a GrIS-originating river has the fastest seasonal response and largest seasonal amplitude with average maximum temperatures above 13 <span class="inline-formula">°C</span>. The seasonal cycle of surface water temperature for all studied lakes is asymmetrical, with faster warming observed after ice-off and a slower cooling of water towards winter freezing. We find that during the study period, the onset of positive stratification occurred earlier, at rates of up to 0.5 <span class="inline-formula">d yr<sup>−1</sup></span>, and that July–August temperatures increased at rates up to 0.1 <span class="inline-formula">°C yr<sup>−1</sup></span>, although the GrIS-connected lakes show smaller increases. Our analysis suggests that the main meteorological factor determining interannual variability of surface water temperature in the studied lakes is air temperature. This study highlights the important role of remote sensing for long-term monitoring of Greenland lakes under climate change.</p> |
| format | Article |
| id | doaj-art-dbd6167ba5b34fbda57f600bc5d924a8 |
| institution | Kabale University |
| issn | 1994-0416 1994-0424 |
| language | English |
| publishDate | 2025-08-01 |
| publisher | Copernicus Publications |
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| series | The Cryosphere |
| spelling | doaj-art-dbd6167ba5b34fbda57f600bc5d924a82025-08-20T06:19:23ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242025-08-01193139315810.5194/tc-19-3139-2025Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheetL. Carrea0C. J. Merchant1C. J. Merchant2R. I. Woolway3N. McCarroll4N. McCarroll5Meteorology Department, University of Reading, Reading, UKMeteorology Department, University of Reading, Reading, UKNational Centre for Earth Observations, University of Reading, Reading, UKSchool of Ocean Sciences, Bangor University, Bangor, UKMeteorology Department, University of Reading, Reading, UKNational Centre for Earth Observations, University of Reading, Reading, UK<p>Subarctic West Greenland is populated by thousands of seasonally ice-free lakes. Using remotely sensed observations, we analyse the surface water temperatures of six lakes during 1995–2022 to identify factors influencing their variability. The connectivity to the Greenland Ice Sheet (GrIS) has a clear influence on lake surface temperature, with ice-sheet-marginal lakes experiencing smaller average summer maximum temperature (<span class="inline-formula"><6</span> <span class="inline-formula">°C</span>) and minimal interannual variability. A lake fed by a GrIS-originating river has the fastest seasonal response and largest seasonal amplitude with average maximum temperatures above 13 <span class="inline-formula">°C</span>. The seasonal cycle of surface water temperature for all studied lakes is asymmetrical, with faster warming observed after ice-off and a slower cooling of water towards winter freezing. We find that during the study period, the onset of positive stratification occurred earlier, at rates of up to 0.5 <span class="inline-formula">d yr<sup>−1</sup></span>, and that July–August temperatures increased at rates up to 0.1 <span class="inline-formula">°C yr<sup>−1</sup></span>, although the GrIS-connected lakes show smaller increases. Our analysis suggests that the main meteorological factor determining interannual variability of surface water temperature in the studied lakes is air temperature. This study highlights the important role of remote sensing for long-term monitoring of Greenland lakes under climate change.</p>https://tc.copernicus.org/articles/19/3139/2025/tc-19-3139-2025.pdf |
| spellingShingle | L. Carrea C. J. Merchant C. J. Merchant R. I. Woolway N. McCarroll N. McCarroll Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheet The Cryosphere |
| title | Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheet |
| title_full | Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheet |
| title_fullStr | Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheet |
| title_full_unstemmed | Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheet |
| title_short | Factors influencing lake surface water temperature variability in West Greenland and the role of the ice sheet |
| title_sort | factors influencing lake surface water temperature variability in west greenland and the role of the ice sheet |
| url | https://tc.copernicus.org/articles/19/3139/2025/tc-19-3139-2025.pdf |
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