Mathematical Modelling of Arctic Polygonal Tundra with Ecosys: 2. Microtopography Determines How CO2 and CH4 Exchange Responds to Changes in Temperature and Precipitation
Abstract
Abstract Differences of surface elevation in arctic polygonal landforms cause spatial variation in soil water contents ( θ ), active layer depths (ALD), and thereby in CO 2 and CH 4 exchange. Here we test hypotheses in ecosys for topographic controls on CO 2 and CH 4 exchange in trough, rim, and center features of low‐ and flat‐centered polygons (LCP and FCP) against chamber and eddy covariance (EC) measurements during 2013 at Barrow, Alaska. Larger CO 2 influxes and CH 4 effluxes were measured with chambers and modeled with ecosys in LCPs than in FCPs and in lower features (troughs) than in higher (rims) within LCPs and FCPs. Spatially aggregated CO 2 and CH 4 fluxes from ecosys were significantly correlated with EC flux measurements. Lower features were modeled as C sinks (52–56 g C m −2 yr −1 ) and CH 4 sources (4–6 g C m −2 yr −1 ), and higher features as near C neutral (−2–15 g C m −2 yr −1 ) and CH 4 neutral (0.0–0.1 g C m −2 yr −1 ). Much of the spatial and temporal variations in CO 2 and CH 4 fluxes were modeled from topographic effects on water and snow movement and thereby on θ , ALD, and soil Omore »
- Authors:
-
- Univ. of Alberta, Edmonton, AB (Canada). Dept. of Renewable Resources
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). Earth Science Division
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- OSTI Identifier:
- 1433102
- Alternate Identifier(s):
- OSTI ID: 1414484
- Grant/Contract Number:
- AC02-05CH11231; DE‐AC02‐05CH11231
- Resource Type:
- Journal Article: Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Biogeosciences
- Additional Journal Information:
- Journal Volume: 122; Journal Issue: 12; Journal ID: ISSN 2169-8953
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; 58 GEOSCIENCES; greenhouse gas exchange; modeling; ecosys; polygonal tundra; microtopography
Citation Formats
Grant, R. F., Mekonnen, Z. A., Riley, W. J., Arora, B., and Torn, M. S. Mathematical Modelling of Arctic Polygonal Tundra with Ecosys: 2. Microtopography Determines How CO2 and CH4 Exchange Responds to Changes in Temperature and Precipitation. United States: N. p., 2017.
Web. doi:10.1002/2017JG004037.
Grant, R. F., Mekonnen, Z. A., Riley, W. J., Arora, B., & Torn, M. S. Mathematical Modelling of Arctic Polygonal Tundra with Ecosys: 2. Microtopography Determines How CO2 and CH4 Exchange Responds to Changes in Temperature and Precipitation. United States. https://doi.org/10.1002/2017JG004037
Grant, R. F., Mekonnen, Z. A., Riley, W. J., Arora, B., and Torn, M. S. 2017.
"Mathematical Modelling of Arctic Polygonal Tundra with Ecosys: 2. Microtopography Determines How CO2 and CH4 Exchange Responds to Changes in Temperature and Precipitation". United States. https://doi.org/10.1002/2017JG004037. https://www.osti.gov/servlets/purl/1433102.
@article{osti_1433102,
title = {Mathematical Modelling of Arctic Polygonal Tundra with Ecosys: 2. Microtopography Determines How CO2 and CH4 Exchange Responds to Changes in Temperature and Precipitation},
author = {Grant, R. F. and Mekonnen, Z. A. and Riley, W. J. and Arora, B. and Torn, M. S.},
abstractNote = {Abstract Differences of surface elevation in arctic polygonal landforms cause spatial variation in soil water contents ( θ ), active layer depths (ALD), and thereby in CO 2 and CH 4 exchange. Here we test hypotheses in ecosys for topographic controls on CO 2 and CH 4 exchange in trough, rim, and center features of low‐ and flat‐centered polygons (LCP and FCP) against chamber and eddy covariance (EC) measurements during 2013 at Barrow, Alaska. Larger CO 2 influxes and CH 4 effluxes were measured with chambers and modeled with ecosys in LCPs than in FCPs and in lower features (troughs) than in higher (rims) within LCPs and FCPs. Spatially aggregated CO 2 and CH 4 fluxes from ecosys were significantly correlated with EC flux measurements. Lower features were modeled as C sinks (52–56 g C m −2 yr −1 ) and CH 4 sources (4–6 g C m −2 yr −1 ), and higher features as near C neutral (−2–15 g C m −2 yr −1 ) and CH 4 neutral (0.0–0.1 g C m −2 yr −1 ). Much of the spatial and temporal variations in CO 2 and CH 4 fluxes were modeled from topographic effects on water and snow movement and thereby on θ , ALD, and soil O 2 concentrations. Model results forced with meteorological data from 1981 to 2015 indicated increasing net primary productivity in higher features and CH 4 emissions in some lower and higher features since 2008, attributed mostly to recent rises in precipitation. Small‐scale variation in surface elevation causes large spatial variation of greenhouse gas (GHG) exchanges and therefore should be considered in estimates of GHG exchange in polygonal landscapes.},
doi = {10.1002/2017JG004037},
url = {https://www.osti.gov/biblio/1433102},
journal = {Journal of Geophysical Research. Biogeosciences},
issn = {2169-8953},
number = 12,
volume = 122,
place = {United States},
year = {Fri Nov 17 00:00:00 EST 2017},
month = {Fri Nov 17 00:00:00 EST 2017}
}
Web of Science
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