Interannual variations in tundra methane emission: A 4‐year time series at fixed sites
Abstract. This paper summarizes 4 years (1987‐1990) of weekly net CH4flux measurements at permanent sites representing important plant components of Arctic tundra. The data coincide with variations in precipitation and temperature of interest in regional and global modeling efforts and are useful in...
Published in: | Global Biogeochemical Cycles |
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Language: | English |
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1992
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ftcdlib:qt7637c1pd 2023-05-15T14:58:46+02:00 Interannual variations in tundra methane emission: A 4‐year time series at fixed sites Whalen, SC Reeburgh, WS 139 - 159 1992-01-01 application/pdf http://www.escholarship.org/uc/item/7637c1pd english eng eScholarship, University of California qt7637c1pd http://www.escholarship.org/uc/item/7637c1pd Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Whalen, SC; & Reeburgh, WS. (1992). Interannual variations in tundra methane emission: A 4‐year time series at fixed sites. Global Biogeochemical Cycles, 6(2), 139 - 159. doi:10.1029/92GB00430. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/7637c1pd article 1992 ftcdlib https://doi.org/10.1029/92GB00430 2018-07-06T22:51:22Z Abstract. This paper summarizes 4 years (1987‐1990) of weekly net CH4flux measurements at permanent sites representing important plant components of Arctic tundra. The data coincide with variations in precipitation and temperature of interest in regional and global modeling efforts and are useful in placing bounds on the role of tundra in the global CH4budget. Precipitation in the study area during the summer emission period ranged from twice to half the long‐term mean, and air temperature anomalies were about +2 °C. This data set also permits consideration of temporal (seasonal to interannual) and spatial variability in CH4flux. We studied the relationship between the net CH4flux and subsurface properties (water table depth, thaw depth, soil temperature, /pCH4distributions) at these permanent sites during the 1988 and 1989 emission periods. Net CH4emission and subsurface properties are largely unrelated. Relationships between soil temperature (or any single variable) and emission are site specific and are of little value as flux predictors. Parameters that integrate conditions influencing flux appear to be the best flux predictors over the emission period. We estimate that Arctic wet meadow and tussock:shrub tundra presently emit about 42 ± 26 Tg CH4yr−1to the atmosphere. This estimate has a North American bias, but it is supported by measurements in a range of locations, transect studies, and model calculations. Copyright 1992 by the American Geophysical Union. Article in Journal/Newspaper Arctic Tundra University of California: eScholarship Arctic Global Biogeochemical Cycles 6 2 139 159 |
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Open Polar |
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University of California: eScholarship |
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ftcdlib |
language |
English |
description |
Abstract. This paper summarizes 4 years (1987‐1990) of weekly net CH4flux measurements at permanent sites representing important plant components of Arctic tundra. The data coincide with variations in precipitation and temperature of interest in regional and global modeling efforts and are useful in placing bounds on the role of tundra in the global CH4budget. Precipitation in the study area during the summer emission period ranged from twice to half the long‐term mean, and air temperature anomalies were about +2 °C. This data set also permits consideration of temporal (seasonal to interannual) and spatial variability in CH4flux. We studied the relationship between the net CH4flux and subsurface properties (water table depth, thaw depth, soil temperature, /pCH4distributions) at these permanent sites during the 1988 and 1989 emission periods. Net CH4emission and subsurface properties are largely unrelated. Relationships between soil temperature (or any single variable) and emission are site specific and are of little value as flux predictors. Parameters that integrate conditions influencing flux appear to be the best flux predictors over the emission period. We estimate that Arctic wet meadow and tussock:shrub tundra presently emit about 42 ± 26 Tg CH4yr−1to the atmosphere. This estimate has a North American bias, but it is supported by measurements in a range of locations, transect studies, and model calculations. Copyright 1992 by the American Geophysical Union. |
format |
Article in Journal/Newspaper |
author |
Whalen, SC Reeburgh, WS |
spellingShingle |
Whalen, SC Reeburgh, WS Interannual variations in tundra methane emission: A 4‐year time series at fixed sites |
author_facet |
Whalen, SC Reeburgh, WS |
author_sort |
Whalen, SC |
title |
Interannual variations in tundra methane emission: A 4‐year time series at fixed sites |
title_short |
Interannual variations in tundra methane emission: A 4‐year time series at fixed sites |
title_full |
Interannual variations in tundra methane emission: A 4‐year time series at fixed sites |
title_fullStr |
Interannual variations in tundra methane emission: A 4‐year time series at fixed sites |
title_full_unstemmed |
Interannual variations in tundra methane emission: A 4‐year time series at fixed sites |
title_sort |
interannual variations in tundra methane emission: a 4‐year time series at fixed sites |
publisher |
eScholarship, University of California |
publishDate |
1992 |
url |
http://www.escholarship.org/uc/item/7637c1pd |
op_coverage |
139 - 159 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Tundra |
genre_facet |
Arctic Tundra |
op_source |
Whalen, SC; & Reeburgh, WS. (1992). Interannual variations in tundra methane emission: A 4‐year time series at fixed sites. Global Biogeochemical Cycles, 6(2), 139 - 159. doi:10.1029/92GB00430. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/7637c1pd |
op_relation |
qt7637c1pd http://www.escholarship.org/uc/item/7637c1pd |
op_rights |
Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1029/92GB00430 |
container_title |
Global Biogeochemical Cycles |
container_volume |
6 |
container_issue |
2 |
container_start_page |
139 |
op_container_end_page |
159 |
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1766330894605352960 |