Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition1

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: Mikel Moriana-Armendariz, Lennart Nilsen, Elisabeth J. Cooper
Format: Article in Journal/Newspaper
Language:English
French
Published: Canadian Science Publishing 2022
Subjects:
geo
Online Access:https://doi.org/10.1139/as-2020-0025
https://doaj.org/article/a87581a8fe134f21a247923853782b80
id fttriple:oai:gotriple.eu:oai:doaj.org/article:a87581a8fe134f21a247923853782b80
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:a87581a8fe134f21a247923853782b80 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 composition1 Mikel Moriana-Armendariz Lennart Nilsen Elisabeth J. Cooper 2022-09-01 https://doi.org/10.1139/as-2020-0025 https://doaj.org/article/a87581a8fe134f21a247923853782b80 en fr eng fre Canadian Science Publishing doi:10.1139/as-2020-0025 2368-7460 https://doaj.org/article/a87581a8fe134f21a247923853782b80 undefined Arctic Science, Vol 8, Iss 3, Pp 767-785 (2022) soil properties plant nutrients community composition NDVI Svalbard propriétés du sol envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.1139/as-2020-0025 2023-01-22T18:58:29Z 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 δ15N). 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 Unknown Adventdalen ENVELOPE(16.264,16.264,78.181,78.181) Arctic Svalbard Arctic Science 8 3 767 785
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
French
topic soil properties
plant nutrients
community composition
NDVI
Svalbard
propriétés du sol
envir
geo
spellingShingle soil properties
plant nutrients
community composition
NDVI
Svalbard
propriétés du sol
envir
geo
Mikel Moriana-Armendariz
Lennart Nilsen
Elisabeth J. Cooper
Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition1
topic_facet soil properties
plant nutrients
community composition
NDVI
Svalbard
propriétés du sol
envir
geo
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 δ15N). 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 Mikel Moriana-Armendariz
Lennart Nilsen
Elisabeth J. Cooper
author_facet Mikel Moriana-Armendariz
Lennart Nilsen
Elisabeth J. Cooper
author_sort Mikel Moriana-Armendariz
title Natural variation in snow depth and snow melt timing in the High Arctic have implications for soil and plant nutrient status and vegetation composition1
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 composition1
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 composition1
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 composition1
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 composition1
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 composition1
publisher Canadian Science Publishing
publishDate 2022
url https://doi.org/10.1139/as-2020-0025
https://doaj.org/article/a87581a8fe134f21a247923853782b80
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_source Arctic Science, Vol 8, Iss 3, Pp 767-785 (2022)
op_relation doi:10.1139/as-2020-0025
2368-7460
https://doaj.org/article/a87581a8fe134f21a247923853782b80
op_rights undefined
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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