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Title: Mathematical Modelling of Arctic Polygonal Tundra with Ecosys: 2. Microtopography Determines How CO2 and CH4 Exchange Responds to Changes in Temperature and Precipitation

Journal Article · · Journal of Geophysical Research. Biogeosciences
DOI:https://doi.org/10.1002/2017JG004037· OSTI ID:1433102
 [1];  [2];  [2]; ORCiD logo [2];  [2]
  1. Univ. of Alberta, Edmonton, AB (Canada). Dept. of Renewable Resources
  2. Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). Earth Science Division

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.

Research Organization:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
AC02-05CH11231; DE‐AC02‐05CH11231
OSTI ID:
1433102
Alternate ID(s):
OSTI ID: 1414484
Journal Information:
Journal of Geophysical Research. Biogeosciences, Vol. 122, Issue 12; ISSN 2169-8953
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 40 works
Citation information provided by
Web of Science

References (28)

Methane efflux from boreal wetlands: Theory and testing of the ecosystem model Ecosys with chamber and tower flux measurements: METHANE EFFLUX FROM BOREAL WETLANDS journal October 2002
Methane exchange in a poorly-drained black spruce forest over permafrost observed using the eddy covariance technique journal December 2015
The transition zones (ecotone) between boreal forests and peatlands: Ecological controls on ecosystem productivity along a transition zone between upland black spruce forest and a poor forested fen in central Saskatchewan journal November 2014
Modeling the spatiotemporal variability in subsurface thermal regimes across a low-relief polygonal tundra landscape journal January 2016
Modeling stomatal and nonstomatal effects of water deficits on CO 2 fixation in a semiarid grassland : MODELING WATER DEFICIT EFFECTS ON CO journal August 2007
Effects of Fine-Scale Topography on CO 2 Flux Components of Alaskan Coastal Plain Tundra: Response to Contrasting Growing Seasons journal May 2011
Methane emissions from Alaska Arctic tundra: An assessment of local spatial variability journal January 1992
Small-scale hydrological variation determines landscape CO2 fluxes in the high Arctic journal June 2006
Estimating uncertainties in individual eddy covariance flux measurements: A comparison of methods and a proposed new method journal March 2011
Modelling contrasting responses of wetland productivity to changes in water table depth journal January 2012
Decadal variations of active-layer thickness in moisture-controlled landscapes, Barrow, Alaska journal January 2010
Geophysical estimation of shallow permafrost distribution and properties in an ice-wedge polygon-dominated Arctic tundra region journal January 2016
Modelling effects of seasonal variation in water table depth on net ecosystem CO 2 exchange of a tropical peatland journal January 2014
Direct uptake of soil nitrogen by mosses journal December 2005
Future increases in Arctic precipitation linked to local evaporation and sea-ice retreat journal May 2014
Micro-topographic patterns unravel controls of soil water and temperature on soil respiration in three Siberian tundra systems journal July 2008
Environmental and physical controls on northern terrestrial methane emissions across permafrost zones journal November 2012
Isotopic insights into methane production, oxidation, and emissions in Arctic polygon tundra journal June 2016
Modeling the effects of hydrology on gross primary productivity and net ecosystem productivity at Mer Bleue bog journal January 2011
Microtopographic controls on ecosystem functioning in the Arctic Coastal Plain journal January 2011
Methane fluxes during the initiation of a large-scale water table manipulation experiment in the Alaskan Arctic tundra: WATER TABLE IMPACTS ON METHANE FLUXES journal May 2009
Growing season methane emissions from a permafrost peatland of northeast China: Observations using open-path eddy covariance method journal March 2017
Coincident aboveground and belowground autonomous monitoring to quantify covariability in permafrost, soil, and vegetation properties in Arctic tundra: ABOVEGROUND AND BELOWGROUND CODYNAMICS journal June 2017
Ecosystem CO 2 and CH 4 exchange in a mixed tundra and a fen within a hydrologically diverse Arctic landscape: 2. Modeled impacts of climate change : CO journal July 2015
Ecosystem CO 2 and CH 4 exchange in a mixed tundra and a fen within a hydrologically diverse Arctic landscape: 1. Modeling versus measurements : CO journal July 2015
Mathematical Modelling of Arctic Polygonal Tundra with Ecosys : 1. Microtopography Determines How Active Layer Depths Respond to Changes in Temperature and Precipitation : Active Layer Depth in Polygonal Tundra journal December 2017
Carbon turnover in Alaskan tundra soils: effects of organic matter quality, temperature, moisture and fertilizer journal May 2006
Identifying multiscale zonation and assessing the relative importance of polygon geomorphology on carbon fluxes in an Arctic tundra ecosystem: ZONATION APPROACH IN AN ARCTIC ECOSYSTEM journal April 2015

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Pathways of ice-wedge degradation in polygonal tundra under different hydrological conditions journal January 2019
Impacts of temperature and soil characteristics on methane production and oxidation in Arctic tundra journal January 2018
21st century tundra shrubification could enhance net carbon uptake of North America Arctic tundra under an RCP8.5 climate trajectory journal May 2018
Large carbon cycle sensitivities to climate across a permafrost thaw gradient in subarctic Sweden journal January 2019
Ground subsidence effects on simulating dynamic high-latitude surface inundation under permafrost thaw using CLM5 journal January 2019
Ground subsidence effects on simulating dynamic high-latitude surface inundation under permafrost thaw using CLM5 text January 2019