Estimating Soil Respiration in a Subalpine Landscape Using Point, Terrain, Climate, and Greenness Data

被引:18
作者
Berryman, Erin M. [1 ]
Vanderhoof, Melanie K. [2 ]
Bradford, John B. [3 ]
Hawbaker, Todd J. [2 ]
Henne, Paul D. [2 ]
Burns, Sean P. [4 ,5 ]
Frank, John M. [6 ]
Birdsey, Richard A. [7 ]
Ryan, Michael G. [6 ,8 ]
机构
[1] US Forest Serv, USDA, Forest Hlth Assessment & Appl Sci Team, Ft Collins, CO 80526 USA
[2] US Geol Survey, Geosci & Environm Change Sci Ctr, Box 25046, Denver, CO 80225 USA
[3] US Geol Survey, Southwest Biol Sci Ctr, Flagstaff, AZ 86001 USA
[4] Univ Colorado, Dept Geog, Boulder, CO 80309 USA
[5] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA
[6] US Forest Serv, Rocky Mt Res Stn, USDA, Ft Collins, CO USA
[7] Woods Hole Res Ctr, Falmouth, MA USA
[8] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80523 USA
关键词
NET PRIMARY PRODUCTION; EDDY COVARIANCE; ECOSYSTEM RESPIRATION; CARBON-DIOXIDE; CO2; FLUX; CHAMBER MEASUREMENTS; SPATIAL SCALES; HIGH-ELEVATION; LONG-TERM; FOREST;
D O I
10.1029/2018JG004613
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Landscape carbon (C) flux estimates help assess the ability of terrestrial ecosystems to buffer further increases in anthropogenic carbon dioxide (CO2) emissions. Advances in remote sensing have led to coarse-scale estimates of gross primary productivity (GPP; e.g., MODIS 17), yet efforts to develop spatial respiration products are lacking. Here we demonstrate a method to predict growing season soil respiration at a regional scale in a mixed subalpine ecosystem. We related field measurements (n=396) of growing season soil respiration mostly from subalpine forests in the Southern Rocky Mountains ecoregion to a suite of biophysical predictors using a Random Forest model (30-m pixel size). We found that Landsat Enhanced Vegetation Index, growing season aridity index, temperature, precipitation, elevation, and slope aspect explained spatiotemporal variability in soil respiration. Our model had a psuedo-r(2) of 0.45 and root-mean-square error of roughly one quarter of the mean value of respiration. Predicted growing season soil respiration across the region was remarkably consistent across 2004, 2005, and 2006 (150-day sums of 542.8, 544.3, and 536.5g C/m(2), respectively). Yet we observed substantial variability in spatial patterns of soil respiration predictions that varied among years, suggesting that our method is sensitive to changes in respiration drivers. Mean predicted growing season soil respiration was 73% of MODIS GPP, while predicted soil respiration was generally within 20% of nocturnal net ecosystem exchange from nearby eddy covariance towers. Thus, geospatial and remotely sensed data sets can be used to estimate soil respiration at landscape scales. Soil respiration returns carbon dioxide back to the atmosphere and is an important part of the carbon cycle, but estimates of soil respiration across large landscapes are difficult to come by. Soil respiration is sensitive to changes in climate and vegetation, which are available as mapped data products, thanks to remote sensing and geospatial technology. We developed a statistical model that mapped soil respiration across three forests and an entire region based on climate and vegetation spatial data. While this work was limited to subalpine forests in the Southern Rocky Mountains, our method can be used in other ecosystems to better understand how ecosystems interact with atmospheric carbon dioxide.
引用
收藏
页码:3231 / 3249
页数:19
相关论文
共 91 条
[1]  
Bechtold W. A., 2005, The enhanced Forest inventory and analysis program National Sampling Design and estimation procedures, DOI DOI 10.2737/SRS-GTR-80
[2]   Total belowground carbon flux in subalpine forests is related to leaf area index, soil nitrogen, and tree height [J].
Berryman, E. ;
Ryan, M. G. ;
Bradford, J. B. ;
Hawbaker, T. J. ;
Birdsey, R. .
ECOSPHERE, 2016, 7 (08)
[3]   Complex terrain alters temperature and moisture limitations of forest soil respiration across a semiarid to subalpine gradient [J].
Berryman, E. M. ;
Barnard, H. R. ;
Adams, H. R. ;
Burns, M. A. ;
Gallo, E. ;
Brooks, P. D. .
JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES, 2015, 120 (04) :707-723
[4]   Component and whole-system respiration fluxes in northern deciduous forests [J].
Bolstad, PV ;
Davis, KJ ;
Martin, J ;
Cook, BD ;
Wang, W .
TREE PHYSIOLOGY, 2004, 24 (05) :493-504
[5]   Evaluating litter decomposition in earth system models with long-term litterbag experiments: an example using the Community Land Model version 4 (CLM4) [J].
Bonan, Gordon B. ;
Hartman, Melannie D. ;
Parton, William J. ;
Wieder, William R. .
GLOBAL CHANGE BIOLOGY, 2013, 19 (03) :957-974
[6]   Contribution of root respiration to soil surface CO2 flux in a boreal black spruce chronosequence [J].
Bond-Lamberty, B ;
Wang, CK ;
Gower, ST .
TREE PHYSIOLOGY, 2004, 24 (12) :1387-1395
[7]   A global database of soil respiration data [J].
Bond-Lamberty, B. ;
Thomson, A. .
BIOGEOSCIENCES, 2010, 7 (06) :1915-1926
[8]   Multi-Year Lags between Forest Browning and Soil Respiration at High Northern Latitudes [J].
Bond-Lamberty, Ben ;
Bunn, Andrew G. ;
Thomson, Allison M. .
PLOS ONE, 2012, 7 (11)
[9]   Temperature-associated increases in the global soil respiration record [J].
Bond-Lamberty, Ben ;
Thomson, Allison .
NATURE, 2010, 464 (7288) :579-U132
[10]   Environmental forcing does not induce diel or synoptic variation in the carbon isotope content of forest soil respiration [J].
Bowling, D. R. ;
Egan, J. E. ;
Hall, S. J. ;
Risk, D. A. .
BIOGEOSCIENCES, 2015, 12 (16) :5143-5160