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...
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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 |
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Wiley Online Library |
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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 |
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1809761580702760960 |