Snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic Svalbard

The High Arctic winter is expected to be altered through ongoing and future climate change. Winter precipitation and snow depth are projected to increase and melt out dates change accordingly. Also, snow cover and depth will play an important role in protecting plant canopy from increasingly more fr...

Full description

Bibliographic Details
Published in:Ecology and Evolution
Main Authors: Semenchuk, Philipp, Elberling, Bo, Cooper, Elisabeth J.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2013
Subjects:
Online Access:https://hdl.handle.net/10037/5783
https://doi.org/10.1002/ece3.648
_version_ 1829304878621523968
author Semenchuk, Philipp
Elberling, Bo
Cooper, Elisabeth J.
author_facet Semenchuk, Philipp
Elberling, Bo
Cooper, Elisabeth J.
author_sort Semenchuk, Philipp
collection University of Tromsø: Munin Open Research Archive
container_issue 8
container_start_page 2586
container_title Ecology and Evolution
container_volume 3
description The High Arctic winter is expected to be altered through ongoing and future climate change. Winter precipitation and snow depth are projected to increase and melt out dates change accordingly. Also, snow cover and depth will play an important role in protecting plant canopy from increasingly more frequent extreme winter warming events. Flower production of many Arctic plants is dependent on melt out timing, since season length determines resource availability for flower preformation. We erected snow fences to increase snow depth and shorten growing season, and counted flowers of six species over 5 years, during which we experienced two extreme winter warming events. Most species were resistant to snow cover increase, but two species reduced flower abundance due to shortened growing seasons. Cassiope tetragona responded strongly with fewer flowers in deep snow regimes during years without extreme events, while Stellaria crassipes responded partly. Snow pack thickness determined whether winter warming events had an effect on flower abundance of some species. Warming events clearly reduced flower abundance in shallow but not in deep snow regimes of Cassiope tetragona, but only marginally for Dryas octopetala. However, the affected species were resilient and individuals did not experience any long term effects. In the case of short or cold summers, a subset of species suffered reduced reproductive success, which may affect future plant composition through possible cascading competition effects. Extreme winter warming events were shown to expose the canopy to cold winter air. The following summer most of the overwintering flower buds could not produce flowers. Thus reproductive success is reduced if this occurs in subsequent years. We conclude that snow depth influences flower abundance by altering season length and by protecting or exposing flower buds to cold winter air, but most species studied are resistant to changes.
format Article in Journal/Newspaper
genre Arctic
Cassiope tetragona
Climate change
Dryas octopetala
Stellaria crassipes
Svalbard
genre_facet Arctic
Cassiope tetragona
Climate change
Dryas octopetala
Stellaria crassipes
Svalbard
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
id ftunivtroemsoe:oai:munin.uit.no:10037/5783
institution Open Polar
language English
op_collection_id ftunivtroemsoe
op_container_end_page 2599
op_doi https://doi.org/10.1002/ece3.648
op_relation FRIDAID 1061269
http://dx.doi.org/10.1002/ece3.648
https://hdl.handle.net/10037/5783
op_rights openAccess
publishDate 2013
publisher Wiley
record_format openpolar
spelling ftunivtroemsoe:oai:munin.uit.no:10037/5783 2025-04-13T14:14:00+00:00 Snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic Svalbard Semenchuk, Philipp Elberling, Bo Cooper, Elisabeth J. 2013 https://hdl.handle.net/10037/5783 https://doi.org/10.1002/ece3.648 eng eng Wiley FRIDAID 1061269 http://dx.doi.org/10.1002/ece3.648 https://hdl.handle.net/10037/5783 openAccess VDP::Mathematics and natural science: 400::Zoology and botany: 480::Vegetation history: 495 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Vegetasjonshistorie: 495 Journal article Tidsskriftartikkel Peer reviewed 2013 ftunivtroemsoe https://doi.org/10.1002/ece3.648 2025-03-14T05:17:55Z The High Arctic winter is expected to be altered through ongoing and future climate change. Winter precipitation and snow depth are projected to increase and melt out dates change accordingly. Also, snow cover and depth will play an important role in protecting plant canopy from increasingly more frequent extreme winter warming events. Flower production of many Arctic plants is dependent on melt out timing, since season length determines resource availability for flower preformation. We erected snow fences to increase snow depth and shorten growing season, and counted flowers of six species over 5 years, during which we experienced two extreme winter warming events. Most species were resistant to snow cover increase, but two species reduced flower abundance due to shortened growing seasons. Cassiope tetragona responded strongly with fewer flowers in deep snow regimes during years without extreme events, while Stellaria crassipes responded partly. Snow pack thickness determined whether winter warming events had an effect on flower abundance of some species. Warming events clearly reduced flower abundance in shallow but not in deep snow regimes of Cassiope tetragona, but only marginally for Dryas octopetala. However, the affected species were resilient and individuals did not experience any long term effects. In the case of short or cold summers, a subset of species suffered reduced reproductive success, which may affect future plant composition through possible cascading competition effects. Extreme winter warming events were shown to expose the canopy to cold winter air. The following summer most of the overwintering flower buds could not produce flowers. Thus reproductive success is reduced if this occurs in subsequent years. We conclude that snow depth influences flower abundance by altering season length and by protecting or exposing flower buds to cold winter air, but most species studied are resistant to changes. Article in Journal/Newspaper Arctic Cassiope tetragona Climate change Dryas octopetala Stellaria crassipes Svalbard University of Tromsø: Munin Open Research Archive Arctic Svalbard Ecology and Evolution 3 8 2586 2599
spellingShingle VDP::Mathematics and natural science: 400::Zoology and botany: 480::Vegetation history: 495
VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Vegetasjonshistorie: 495
Semenchuk, Philipp
Elberling, Bo
Cooper, Elisabeth J.
Snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic Svalbard
title Snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic Svalbard
title_full Snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic Svalbard
title_fullStr Snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic Svalbard
title_full_unstemmed Snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic Svalbard
title_short Snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic Svalbard
title_sort snow cover and extreme winter warming events control flower abundance of some, but not all species in high arctic svalbard
topic VDP::Mathematics and natural science: 400::Zoology and botany: 480::Vegetation history: 495
VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Vegetasjonshistorie: 495
topic_facet VDP::Mathematics and natural science: 400::Zoology and botany: 480::Vegetation history: 495
VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Vegetasjonshistorie: 495
url https://hdl.handle.net/10037/5783
https://doi.org/10.1002/ece3.648