WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?

© 2016 Swedish Society for Anthropology and Geography In this short communication, we report on dissolved organic and inorganic carbon concentrations from a summer stream monitoring campaign at the main hydrological catchment of the Tarfala Research Station in northern Sweden. Further, we place thes...

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Published in:Geografiska Annaler: Series A, Physical Geography
Main Authors: Lyon, SW, Jantze, EJ, Dahlke, HE, Jaramillo, F, Winterdahl, M
Format: Article in Journal/Newspaper
Language:English
Published: eScholarship, University of California 2016
Subjects:
Online Access:http://www.escholarship.org/uc/item/0jj6n2km
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spelling ftcdlib:qt0jj6n2km 2023-05-15T16:12:02+02:00 WHY MONITOR CARBON IN HIGH-ALPINE STREAMS? Lyon, SW Jantze, EJ Dahlke, HE Jaramillo, F Winterdahl, M 237 - 245 2016-09-01 application/pdf http://www.escholarship.org/uc/item/0jj6n2km english eng eScholarship, University of California qt0jj6n2km http://www.escholarship.org/uc/item/0jj6n2km public Lyon, SW; Jantze, EJ; Dahlke, HE; Jaramillo, F; & Winterdahl, M. (2016). WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?. Geografiska Annaler, Series A: Physical Geography, 98(3), 237 - 245. doi:10.1111/geoa.12136. UC Davis: Retrieved from: http://www.escholarship.org/uc/item/0jj6n2km carbon monitoring alpine streams article 2016 ftcdlib https://doi.org/10.1111/geoa.12136 2017-10-06T22:51:07Z © 2016 Swedish Society for Anthropology and Geography In this short communication, we report on dissolved organic and inorganic carbon concentrations from a summer stream monitoring campaign at the main hydrological catchment of the Tarfala Research Station in northern Sweden. Further, we place these unique high-alpine observations in the context of a relevant subset of Sweden's national monitoring programme. Our analysis shows that while the monitoring programme (at least for total organic carbon) may have relatively good representativeness across a range of forest coverages, alpine/tundra environments are potentially underrepresented. As for dissolved inorganic carbon, there is currently no national monitoring in Sweden. Since the selection of stream water monitoring locations and monitored constituents at the national scale can be motivated by any number of goals (or limitations), monitoring at the Tarfala Research Station along with other research catchment sites across Fennoscandia becomes increasingly important and can offer potential complementary data necessary for improving process understanding. Research catchment sites (typically not included in national monitoring programmes) can help cover small-scale landscape features and thus complement national monitoring thereby improving the ability to capture hot spots and hot moments of biogeochemical export. This provides a valuable baseline of current conditions in high-alpine environments against which to gauge future changes in response to potential climatic and land cover shifts. Article in Journal/Newspaper Fennoscandia Northern Sweden Tarfala Tundra University of California: eScholarship Tarfala ENVELOPE(18.608,18.608,67.914,67.914) Geografiska Annaler: Series A, Physical Geography 98 3 237 245
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language English
topic carbon
monitoring
alpine
streams
spellingShingle carbon
monitoring
alpine
streams
Lyon, SW
Jantze, EJ
Dahlke, HE
Jaramillo, F
Winterdahl, M
WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?
topic_facet carbon
monitoring
alpine
streams
description © 2016 Swedish Society for Anthropology and Geography In this short communication, we report on dissolved organic and inorganic carbon concentrations from a summer stream monitoring campaign at the main hydrological catchment of the Tarfala Research Station in northern Sweden. Further, we place these unique high-alpine observations in the context of a relevant subset of Sweden's national monitoring programme. Our analysis shows that while the monitoring programme (at least for total organic carbon) may have relatively good representativeness across a range of forest coverages, alpine/tundra environments are potentially underrepresented. As for dissolved inorganic carbon, there is currently no national monitoring in Sweden. Since the selection of stream water monitoring locations and monitored constituents at the national scale can be motivated by any number of goals (or limitations), monitoring at the Tarfala Research Station along with other research catchment sites across Fennoscandia becomes increasingly important and can offer potential complementary data necessary for improving process understanding. Research catchment sites (typically not included in national monitoring programmes) can help cover small-scale landscape features and thus complement national monitoring thereby improving the ability to capture hot spots and hot moments of biogeochemical export. This provides a valuable baseline of current conditions in high-alpine environments against which to gauge future changes in response to potential climatic and land cover shifts.
format Article in Journal/Newspaper
author Lyon, SW
Jantze, EJ
Dahlke, HE
Jaramillo, F
Winterdahl, M
author_facet Lyon, SW
Jantze, EJ
Dahlke, HE
Jaramillo, F
Winterdahl, M
author_sort Lyon, SW
title WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?
title_short WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?
title_full WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?
title_fullStr WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?
title_full_unstemmed WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?
title_sort why monitor carbon in high-alpine streams?
publisher eScholarship, University of California
publishDate 2016
url http://www.escholarship.org/uc/item/0jj6n2km
op_coverage 237 - 245
long_lat ENVELOPE(18.608,18.608,67.914,67.914)
geographic Tarfala
geographic_facet Tarfala
genre Fennoscandia
Northern Sweden
Tarfala
Tundra
genre_facet Fennoscandia
Northern Sweden
Tarfala
Tundra
op_source Lyon, SW; Jantze, EJ; Dahlke, HE; Jaramillo, F; & Winterdahl, M. (2016). WHY MONITOR CARBON IN HIGH-ALPINE STREAMS?. Geografiska Annaler, Series A: Physical Geography, 98(3), 237 - 245. doi:10.1111/geoa.12136. UC Davis: Retrieved from: http://www.escholarship.org/uc/item/0jj6n2km
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op_doi https://doi.org/10.1111/geoa.12136
container_title Geografiska Annaler: Series A, Physical Geography
container_volume 98
container_issue 3
container_start_page 237
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