Vegetation Influence and Environmental Controls on Greenhouse Gas Fluxes from a Drained Thermokarst Lake in the Western Canadian Arctic

Thermokarst features are widespread in ice-rich regions of the circumpolar Arctic. The rate of thermokarst lake formation and drainage is anticipated to accelerate as the climate warms. However, it is uncertain how these dynamic features impact the terrestrial Arctic carbon cycle. Methane (CH 4 ) an...

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Main Authors: Skeeter, June, Christen, Andreas, Laforce, Andrée-Anne, Humphreys, Elyn, Henry, Greg
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/bg-2019-477
https://www.biogeosciences-discuss.net/bg-2019-477/
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spelling ftcopernicus:oai:publications.copernicus.org:bgd82125 2023-05-15T14:55:48+02:00 Vegetation Influence and Environmental Controls on Greenhouse Gas Fluxes from a Drained Thermokarst Lake in the Western Canadian Arctic Skeeter, June Christen, Andreas Laforce, Andrée-Anne Humphreys, Elyn Henry, Greg 2020-02-12 application/pdf https://doi.org/10.5194/bg-2019-477 https://www.biogeosciences-discuss.net/bg-2019-477/ eng eng doi:10.5194/bg-2019-477 https://www.biogeosciences-discuss.net/bg-2019-477/ eISSN: 1726-4189 Text 2020 ftcopernicus https://doi.org/10.5194/bg-2019-477 2020-02-17T15:42:00Z Thermokarst features are widespread in ice-rich regions of the circumpolar Arctic. The rate of thermokarst lake formation and drainage is anticipated to accelerate as the climate warms. However, it is uncertain how these dynamic features impact the terrestrial Arctic carbon cycle. Methane (CH 4 ) and carbon dioxide (CO 2 ) fluxes were measured during peak growing season using eddy covariance and chambers at Illisarvik, a 0.16 km 2 thermokarst lake basin that was experimentally drained in 1978 on Richards Island, Northwest Territories, Canada. Vegetation in the basin differs markedly from the surrounding dwarf-shrub tundra and included patches of tall shrubs, grasses and sedges with some bare ground and a small pond in the centre. During the study period, temperature and wind conditions were highly variable and soil water content decreased steadily. Basin scaled net ecosystem exchange (NEE) measured by eddy covariance was −1.5 [CI 95 % ± 0.2] g C-CO 2 m −2 d −1 NEE followed a marked diurnal pattern with no trend during the study period. NEE was primary controlled by photosynthetic photon flux density and influenced by vapor pressure deficit, volumetric water content and the presence of shrubs. By contrast, net methane exchange (NME) was low (8.7 [CI 95 % ± 0.4] mg CH 4 m −2 d −1 and had little impact on the carbon balance of the basin during the study period. NME displayed high spatial variability, sedge areas in the basin were the strongest source of CH 4 while upland areas outside the basin were a net sink. Soil moisture and temperature were the main environmental factors influencing NME, having a positive and negative effect respectively. Text Arctic Northwest Territories Richards Island Thermokarst Tundra Copernicus Publications: E-Journals Arctic Canada Northwest Territories
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Thermokarst features are widespread in ice-rich regions of the circumpolar Arctic. The rate of thermokarst lake formation and drainage is anticipated to accelerate as the climate warms. However, it is uncertain how these dynamic features impact the terrestrial Arctic carbon cycle. Methane (CH 4 ) and carbon dioxide (CO 2 ) fluxes were measured during peak growing season using eddy covariance and chambers at Illisarvik, a 0.16 km 2 thermokarst lake basin that was experimentally drained in 1978 on Richards Island, Northwest Territories, Canada. Vegetation in the basin differs markedly from the surrounding dwarf-shrub tundra and included patches of tall shrubs, grasses and sedges with some bare ground and a small pond in the centre. During the study period, temperature and wind conditions were highly variable and soil water content decreased steadily. Basin scaled net ecosystem exchange (NEE) measured by eddy covariance was −1.5 [CI 95 % ± 0.2] g C-CO 2 m −2 d −1 NEE followed a marked diurnal pattern with no trend during the study period. NEE was primary controlled by photosynthetic photon flux density and influenced by vapor pressure deficit, volumetric water content and the presence of shrubs. By contrast, net methane exchange (NME) was low (8.7 [CI 95 % ± 0.4] mg CH 4 m −2 d −1 and had little impact on the carbon balance of the basin during the study period. NME displayed high spatial variability, sedge areas in the basin were the strongest source of CH 4 while upland areas outside the basin were a net sink. Soil moisture and temperature were the main environmental factors influencing NME, having a positive and negative effect respectively.
format Text
author Skeeter, June
Christen, Andreas
Laforce, Andrée-Anne
Humphreys, Elyn
Henry, Greg
spellingShingle Skeeter, June
Christen, Andreas
Laforce, Andrée-Anne
Humphreys, Elyn
Henry, Greg
Vegetation Influence and Environmental Controls on Greenhouse Gas Fluxes from a Drained Thermokarst Lake in the Western Canadian Arctic
author_facet Skeeter, June
Christen, Andreas
Laforce, Andrée-Anne
Humphreys, Elyn
Henry, Greg
author_sort Skeeter, June
title Vegetation Influence and Environmental Controls on Greenhouse Gas Fluxes from a Drained Thermokarst Lake in the Western Canadian Arctic
title_short Vegetation Influence and Environmental Controls on Greenhouse Gas Fluxes from a Drained Thermokarst Lake in the Western Canadian Arctic
title_full Vegetation Influence and Environmental Controls on Greenhouse Gas Fluxes from a Drained Thermokarst Lake in the Western Canadian Arctic
title_fullStr Vegetation Influence and Environmental Controls on Greenhouse Gas Fluxes from a Drained Thermokarst Lake in the Western Canadian Arctic
title_full_unstemmed Vegetation Influence and Environmental Controls on Greenhouse Gas Fluxes from a Drained Thermokarst Lake in the Western Canadian Arctic
title_sort vegetation influence and environmental controls on greenhouse gas fluxes from a drained thermokarst lake in the western canadian arctic
publishDate 2020
url https://doi.org/10.5194/bg-2019-477
https://www.biogeosciences-discuss.net/bg-2019-477/
geographic Arctic
Canada
Northwest Territories
geographic_facet Arctic
Canada
Northwest Territories
genre Arctic
Northwest Territories
Richards Island
Thermokarst
Tundra
genre_facet Arctic
Northwest Territories
Richards Island
Thermokarst
Tundra
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-2019-477
https://www.biogeosciences-discuss.net/bg-2019-477/
op_doi https://doi.org/10.5194/bg-2019-477
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