Subglacial upwelling in winter/spring increases under-ice primary production
Subglacial upwelling of nutrient rich bottom water is known to support high summer primary production in Arctic fjord systems. However, during the winter/spring season, the importance of subglacial upwelling has not been considered yet. We hypothesized that subglacial upwelling under sea ice is pres...
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ftcopernicus:oai:publications.copernicus.org:tcd90763 2023-05-15T15:11:38+02:00 Subglacial upwelling in winter/spring increases under-ice primary production Vonnahme, Tobias Reiner Persson, Emma Dietrich, Ulrike Hejdukova, Eva Dybwad, Christine Elster, Josef Chierici, Melissa Gradinger, Rolf 2020-11-05 application/pdf https://doi.org/10.5194/tc-2020-326 https://tc.copernicus.org/preprints/tc-2020-326/ eng eng doi:10.5194/tc-2020-326 https://tc.copernicus.org/preprints/tc-2020-326/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-2020-326 2020-11-09T17:22:13Z Subglacial upwelling of nutrient rich bottom water is known to support high summer primary production in Arctic fjord systems. However, during the winter/spring season, the importance of subglacial upwelling has not been considered yet. We hypothesized that subglacial upwelling under sea ice is present in winter/spring and sufficient to increase phytoplankton primary productivity. We evaluated the effects of the subglacial upwelling on primary production in a seasonally fast ice covered Svalbard fjord (Billefjorden) influenced by a tidewater outlet glacier in April/May 2019. We found clear evidence for subglacial upwelling. Although the estimated entrainment factor (1.6) and total fluxes were lower than in summer studies, we observed substantial impact on the fjord ecosystem and primary production. The subglacial meltwater leads to a salinity stratified surface layer and sea ice formation with low bulk salinity and permeability. The combination of the stratified surface layer, a two-fold higher under-ice irradiance, and higher N and Si concentrations at the glacier front supported two orders of magnitude higher primary production (42.6 mg C m −2 d −1 ) compared to a marine reference site at the fast ice edge. The nutrient supply increased primary production by approximately 30 %. The brackish water sea ice at the glacier front with its low bulk salinity contained a reduced brine volume, limiting the inhabitable place and nutrient exchange with the underlying seawater compared to full marine sea ice. Microbial and algal communities were substantially different in subglacial influenced water and sea ice compared to the marine reference site, sharing taxa with the subglacial outflow water. We suggest that with climate change, the retreat of tidewater glaciers could lead to decreased under-ice phytoplankton primary production, while sea ice algae production and biomass may become increasingly important. Text Arctic Billefjorden Climate change glacier ice algae Phytoplankton Sea ice Svalbard Tidewater Copernicus Publications: E-Journals Arctic Svalbard Billefjorden ENVELOPE(16.417,16.417,78.563,78.563) |
institution |
Open Polar |
collection |
Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
Subglacial upwelling of nutrient rich bottom water is known to support high summer primary production in Arctic fjord systems. However, during the winter/spring season, the importance of subglacial upwelling has not been considered yet. We hypothesized that subglacial upwelling under sea ice is present in winter/spring and sufficient to increase phytoplankton primary productivity. We evaluated the effects of the subglacial upwelling on primary production in a seasonally fast ice covered Svalbard fjord (Billefjorden) influenced by a tidewater outlet glacier in April/May 2019. We found clear evidence for subglacial upwelling. Although the estimated entrainment factor (1.6) and total fluxes were lower than in summer studies, we observed substantial impact on the fjord ecosystem and primary production. The subglacial meltwater leads to a salinity stratified surface layer and sea ice formation with low bulk salinity and permeability. The combination of the stratified surface layer, a two-fold higher under-ice irradiance, and higher N and Si concentrations at the glacier front supported two orders of magnitude higher primary production (42.6 mg C m −2 d −1 ) compared to a marine reference site at the fast ice edge. The nutrient supply increased primary production by approximately 30 %. The brackish water sea ice at the glacier front with its low bulk salinity contained a reduced brine volume, limiting the inhabitable place and nutrient exchange with the underlying seawater compared to full marine sea ice. Microbial and algal communities were substantially different in subglacial influenced water and sea ice compared to the marine reference site, sharing taxa with the subglacial outflow water. We suggest that with climate change, the retreat of tidewater glaciers could lead to decreased under-ice phytoplankton primary production, while sea ice algae production and biomass may become increasingly important. |
format |
Text |
author |
Vonnahme, Tobias Reiner Persson, Emma Dietrich, Ulrike Hejdukova, Eva Dybwad, Christine Elster, Josef Chierici, Melissa Gradinger, Rolf |
spellingShingle |
Vonnahme, Tobias Reiner Persson, Emma Dietrich, Ulrike Hejdukova, Eva Dybwad, Christine Elster, Josef Chierici, Melissa Gradinger, Rolf Subglacial upwelling in winter/spring increases under-ice primary production |
author_facet |
Vonnahme, Tobias Reiner Persson, Emma Dietrich, Ulrike Hejdukova, Eva Dybwad, Christine Elster, Josef Chierici, Melissa Gradinger, Rolf |
author_sort |
Vonnahme, Tobias Reiner |
title |
Subglacial upwelling in winter/spring increases under-ice primary production |
title_short |
Subglacial upwelling in winter/spring increases under-ice primary production |
title_full |
Subglacial upwelling in winter/spring increases under-ice primary production |
title_fullStr |
Subglacial upwelling in winter/spring increases under-ice primary production |
title_full_unstemmed |
Subglacial upwelling in winter/spring increases under-ice primary production |
title_sort |
subglacial upwelling in winter/spring increases under-ice primary production |
publishDate |
2020 |
url |
https://doi.org/10.5194/tc-2020-326 https://tc.copernicus.org/preprints/tc-2020-326/ |
long_lat |
ENVELOPE(16.417,16.417,78.563,78.563) |
geographic |
Arctic Svalbard Billefjorden |
geographic_facet |
Arctic Svalbard Billefjorden |
genre |
Arctic Billefjorden Climate change glacier ice algae Phytoplankton Sea ice Svalbard Tidewater |
genre_facet |
Arctic Billefjorden Climate change glacier ice algae Phytoplankton Sea ice Svalbard Tidewater |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-2020-326 https://tc.copernicus.org/preprints/tc-2020-326/ |
op_doi |
https://doi.org/10.5194/tc-2020-326 |
_version_ |
1766342471677116416 |