Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition

Snow cover is a key component in Arctic ecosystems and will likely be affected by changes in winter precipitation. Increased snow depth and consequent later snowmelt leads to greater microbial mineralization in winter, improving soil and vegetation nutrient status. We studied areas with naturally di...

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Published in:Arctic Science
Main Authors: Moriana Armendariz, Mikel, Nilsen, Lennart, Cooper, Elisabeth J.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2022
Subjects:
Online Access:https://hdl.handle.net/10037/27733
https://doi.org/10.1139/as-2020-0025
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/27733 2023-05-15T13:05:43+02:00 Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition Moriana Armendariz, Mikel Nilsen, Lennart Cooper, Elisabeth J. 2022-02-16 https://hdl.handle.net/10037/27733 https://doi.org/10.1139/as-2020-0025 eng eng Canadian Science Publishing Arctic Science Moriana Armendariz, Nilsen, Cooper. Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition. Arctic Science. 2022;8(3):767-785 FRIDAID 2087797 doi:10.1139/as-2020-0025 2368-7460 https://hdl.handle.net/10037/27733 Attribution 4.0 International (CC BY 4.0) openAccess Copyright 2022 The Author(s) https://creativecommons.org/licenses/by/4.0 CC-BY Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2022 ftunivtroemsoe https://doi.org/10.1139/as-2020-0025 2022-12-15T00:02:36Z Snow cover is a key component in Arctic ecosystems and will likely be affected by changes in winter precipitation. Increased snow depth and consequent later snowmelt leads to greater microbial mineralization in winter, improving soil and vegetation nutrient status. We studied areas with naturally differing snow depths and date of snowmelt in Adventdalen, Svalbard. Soil properties, plant leaf nutrient status, and species composition along with the normalized difference vegetation index (NDVI) were compared for three snowmelt regimes (Early, Mid, and Late). We showed that (1) Late regimes (snow beds) had wetter soils, higher pH, and leaves of Bistorta vivipara (L.) Delarbre and Salix polaris Wahlenb. had higher concentration of nutrients (nitrogen and δ 15 N). Little to no difference was found in soil nutrient concentrations between snowmelt regimes. (2) Late regimes had highest NDVI values, whereas those of Early and Mid regimes were similar. (3) Vegetation composition differed between Early and Late regimes, with Dryas octopetala L. and Luzula arcuata subsp. confusa (Lange) characterizing the former and Equisetum arvense L. and Eriophorum scheuchzeri Hoppe the latter. (4) Trends for plant nutrient contents were similar to those found in a nearby snow manipulation experiment. Snow distribution and time of snowmelt played an important role in determining regional environmental heterogeneity, patchiness in plant community distribution, their species composition, and plant phenology. Article in Journal/Newspaper Adventdalen Arctic Arctic Dryas octopetala Eriophorum Eriophorum scheuchzeri Salix polaris Svalbard University of Tromsø: Munin Open Research Archive Adventdalen ENVELOPE(16.264,16.264,78.181,78.181) Arctic Svalbard Arctic Science 8 3 767 785
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
description Snow cover is a key component in Arctic ecosystems and will likely be affected by changes in winter precipitation. Increased snow depth and consequent later snowmelt leads to greater microbial mineralization in winter, improving soil and vegetation nutrient status. We studied areas with naturally differing snow depths and date of snowmelt in Adventdalen, Svalbard. Soil properties, plant leaf nutrient status, and species composition along with the normalized difference vegetation index (NDVI) were compared for three snowmelt regimes (Early, Mid, and Late). We showed that (1) Late regimes (snow beds) had wetter soils, higher pH, and leaves of Bistorta vivipara (L.) Delarbre and Salix polaris Wahlenb. had higher concentration of nutrients (nitrogen and δ 15 N). Little to no difference was found in soil nutrient concentrations between snowmelt regimes. (2) Late regimes had highest NDVI values, whereas those of Early and Mid regimes were similar. (3) Vegetation composition differed between Early and Late regimes, with Dryas octopetala L. and Luzula arcuata subsp. confusa (Lange) characterizing the former and Equisetum arvense L. and Eriophorum scheuchzeri Hoppe the latter. (4) Trends for plant nutrient contents were similar to those found in a nearby snow manipulation experiment. Snow distribution and time of snowmelt played an important role in determining regional environmental heterogeneity, patchiness in plant community distribution, their species composition, and plant phenology.
format Article in Journal/Newspaper
author Moriana Armendariz, Mikel
Nilsen, Lennart
Cooper, Elisabeth J.
spellingShingle Moriana Armendariz, Mikel
Nilsen, Lennart
Cooper, Elisabeth J.
Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition
author_facet Moriana Armendariz, Mikel
Nilsen, Lennart
Cooper, Elisabeth J.
author_sort Moriana Armendariz, Mikel
title Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition
title_short Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition
title_full Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition
title_fullStr Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition
title_full_unstemmed Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition
title_sort natural variation in snow depth and snow melt timing in the high arctic have implications for soil and plant nutrient status and vegetation composition
publisher Canadian Science Publishing
publishDate 2022
url https://hdl.handle.net/10037/27733
https://doi.org/10.1139/as-2020-0025
long_lat ENVELOPE(16.264,16.264,78.181,78.181)
geographic Adventdalen
Arctic
Svalbard
geographic_facet Adventdalen
Arctic
Svalbard
genre Adventdalen
Arctic
Arctic
Dryas octopetala
Eriophorum
Eriophorum scheuchzeri
Salix polaris
Svalbard
genre_facet Adventdalen
Arctic
Arctic
Dryas octopetala
Eriophorum
Eriophorum scheuchzeri
Salix polaris
Svalbard
op_relation Arctic Science
Moriana Armendariz, Nilsen, Cooper. Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition. Arctic Science. 2022;8(3):767-785
FRIDAID 2087797
doi:10.1139/as-2020-0025
2368-7460
https://hdl.handle.net/10037/27733
op_rights Attribution 4.0 International (CC BY 4.0)
openAccess
Copyright 2022 The Author(s)
https://creativecommons.org/licenses/by/4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1139/as-2020-0025
container_title Arctic Science
container_volume 8
container_issue 3
container_start_page 767
op_container_end_page 785
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