Ecological significance of litter redistribution by wind and snow in arctic landscapes

During winter in the Arctic, plant litter is scoured from exposed hills and ridges by wind and snow and is redistributed to other portions of the landscape. The aim of this research was to quantify the physical and biological consequences of this litter redistribution. Litter biomass accumulation wa...

Full description

Bibliographic Details
Published in:Ecography
Main Authors: Fahnestock, J. T., Povirk, K. L., Welker, J. M.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2000
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1600-0587.2000.tb00181.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1600-0587.2000.tb00181.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1600-0587.2000.tb00181.x
id crwiley:10.1111/j.1600-0587.2000.tb00181.x
record_format openpolar
spelling crwiley:10.1111/j.1600-0587.2000.tb00181.x 2024-09-09T19:21:22+00:00 Ecological significance of litter redistribution by wind and snow in arctic landscapes Fahnestock, J. T. Povirk, K. L. Welker, J. M. 2000 http://dx.doi.org/10.1111/j.1600-0587.2000.tb00181.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1600-0587.2000.tb00181.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1600-0587.2000.tb00181.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Ecography volume 23, issue 5, page 623-631 ISSN 0906-7590 1600-0587 journal-article 2000 crwiley https://doi.org/10.1111/j.1600-0587.2000.tb00181.x 2024-06-18T04:13:55Z During winter in the Arctic, plant litter is scoured from exposed hills and ridges by wind and snow and is redistributed to other portions of the landscape. The aim of this research was to quantify the physical and biological consequences of this litter redistribution. Litter biomass accumulation was ten times greater in areas of high deposition (e.g. snow drifts) than in areas of low deposition. Spring snow melt was delayed by several days and soils were cooler throughout the growing season and throughout winter in areas of increased litter deposition than areas with no litter. Photosynthetically active radiation (PAR) was reduced to near zero with small accumulations of litter. Annual C and N inputs from allochthonous litter were 143 g Cm‐2 and 14 g Nm in high lilter areas and 3.4 g C m −2 and 0.3 g N m‐2 in non‐drift, ambient litter deposition areas. Although PAR and soil temperatures were significantly reduced with increased litter deposition, we did not observe significant delays in key plant phenological events of several species or measure a decrease in gross ecosystem photosynthesis. We did measure a significant increase in ecosystem respiration with increased litter deposition, which resulted in a shift in the net C balance of dry heath tundra from near zero with no litter to a net source of CO 2 to the atmosphere. Our study indicates that the redistribution of litter by wind and snow during winter is an important mechanism of nutrient transfer across the arctic landscape and that allochthonous litter inputs are of great enough magnitude to alter the carbon balance of some areas of the arctic landscape. Article in Journal/Newspaper Arctic Tundra Wiley Online Library Arctic Ecography 23 5 623 631
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description During winter in the Arctic, plant litter is scoured from exposed hills and ridges by wind and snow and is redistributed to other portions of the landscape. The aim of this research was to quantify the physical and biological consequences of this litter redistribution. Litter biomass accumulation was ten times greater in areas of high deposition (e.g. snow drifts) than in areas of low deposition. Spring snow melt was delayed by several days and soils were cooler throughout the growing season and throughout winter in areas of increased litter deposition than areas with no litter. Photosynthetically active radiation (PAR) was reduced to near zero with small accumulations of litter. Annual C and N inputs from allochthonous litter were 143 g Cm‐2 and 14 g Nm in high lilter areas and 3.4 g C m −2 and 0.3 g N m‐2 in non‐drift, ambient litter deposition areas. Although PAR and soil temperatures were significantly reduced with increased litter deposition, we did not observe significant delays in key plant phenological events of several species or measure a decrease in gross ecosystem photosynthesis. We did measure a significant increase in ecosystem respiration with increased litter deposition, which resulted in a shift in the net C balance of dry heath tundra from near zero with no litter to a net source of CO 2 to the atmosphere. Our study indicates that the redistribution of litter by wind and snow during winter is an important mechanism of nutrient transfer across the arctic landscape and that allochthonous litter inputs are of great enough magnitude to alter the carbon balance of some areas of the arctic landscape.
format Article in Journal/Newspaper
author Fahnestock, J. T.
Povirk, K. L.
Welker, J. M.
spellingShingle Fahnestock, J. T.
Povirk, K. L.
Welker, J. M.
Ecological significance of litter redistribution by wind and snow in arctic landscapes
author_facet Fahnestock, J. T.
Povirk, K. L.
Welker, J. M.
author_sort Fahnestock, J. T.
title Ecological significance of litter redistribution by wind and snow in arctic landscapes
title_short Ecological significance of litter redistribution by wind and snow in arctic landscapes
title_full Ecological significance of litter redistribution by wind and snow in arctic landscapes
title_fullStr Ecological significance of litter redistribution by wind and snow in arctic landscapes
title_full_unstemmed Ecological significance of litter redistribution by wind and snow in arctic landscapes
title_sort ecological significance of litter redistribution by wind and snow in arctic landscapes
publisher Wiley
publishDate 2000
url http://dx.doi.org/10.1111/j.1600-0587.2000.tb00181.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1600-0587.2000.tb00181.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1600-0587.2000.tb00181.x
geographic Arctic
geographic_facet Arctic
genre Arctic
Tundra
genre_facet Arctic
Tundra
op_source Ecography
volume 23, issue 5, page 623-631
ISSN 0906-7590 1600-0587
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/j.1600-0587.2000.tb00181.x
container_title Ecography
container_volume 23
container_issue 5
container_start_page 623
op_container_end_page 631
_version_ 1809761580702760960