Methane Emissions From Land and Aquatic Ecosystems in Western Siberia: An Analysis With Methane Biogeochemistry Models

被引:1
作者
Xi, Xuan [1 ]
Zhuang, Qianlai [1 ,2 ]
Kim, Seungbum [3 ]
Zhang, Zhen [4 ,5 ]
机构
[1] Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA
[2] Purdue Univ, Dept Agron, W Lafayette, IN 47907 USA
[3] NASA Jet Prop Lab, Pasadena, CA USA
[4] Chinese Acad Sci, Inst Tibetan Plateau Res, Natl Tibetan Plateau Data Ctr TPDC, State Key Lab Tibetan Plateau Earth Syst Environm, Beijing, Peoples R China
[5] Univ Maryland, Dept Geog Sci, College Pk, MD USA
关键词
CLIMATE-CHANGE; ARCTIC LAKES; CO2; CH4; PERMAFROST; PEATLANDS; ALASKA; STATE; WATER; AREA;
D O I
10.1029/2023JG007466
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Western Siberia contains extensive wetlands and aquatic ecosystems, contributing a significant amount of methane (CH4) emissions to the atmosphere. However, estimates of CH4 fluxes over the region are poorly constrained partly due to the uncertainties from the inundated area data. This study applied two process-based biogeochemistry models to quantify the emissions from land and aquatic ecosystems over the region within the period 2000-2021 using different inundation datasets. To drive land methane modeling, we use one static wetland map and one dynamic wetland area data set called Wetland Area and Dynamics for Methane Modeling (WAD2M) (2000-2020). To drive lake methane modeling, we use the surface area of aquatic ecosystems from three datasets: (a) HydroLAKES; (b) Global Surface Water (GSW); and (c) surface water inundation from Soil Moisture Active Passive (SMAP) (2016-2021). Using these datasets, we conduct four simulations to compare emissions over the region. We find that the net methane emissions from land using the static wetland map are larger than those using WAD2M. SMAP and GSW estimate larger emissions than HydroLAKES does from aquatic ecosystems. Total emissions over the region range from 4.80 +/- 0.43 to 8.29 +/- 0.81 Tg CH4/year from 2016 to 2020, which is the intersection period of four simulations. This study is among the first to investigate methane emissions from the whole landscape in the region. Our study highlights the importance of dynamic wetland and aquatic area data in quantifying regional methane emissions. Plain Language Summary Methane (CH4) is a vital greenhouse gas that can make large differences in global climate change. In this study, we quantified total methane emissions over Western Siberia, which is a methane-emitting hotpot. We used two process-based models to quantify methane emissions from both land and aquatic ecosystems over the region. We used different combinations of wetlands and aquatic areal datasets to run four model simulations for comparison. We found that the total emissions over the region range from 4.80 +/- 0.43 to 8.29 +/- 0.81 Tg CH4/year from 2016 to 2020 depending on the land and aquatic areal dynamics. We conclude that it is important to develop dynamic wetland and aquatic area data in quantifying regional methane emissions.
引用
收藏
页数:15
相关论文
共 57 条
  • [21] METHANE EMISSION FROM NATURAL WETLANDS: GLOBAL DISTRIBUTION, AREA, AND ENVIRONMENTAL CHARACTERISTICS OF SOURCES
    Matthews, Elaine
    Fung, Inez
    [J]. GLOBAL BIOGEOCHEMICAL CYCLES, 1987, 1 (01) : 61 - 86
  • [22] Regionalization of methane emissions in the Amazon Basin with microwave remote sensing
    Melack, JM
    Hess, LL
    Gastil, M
    Forsberg, BR
    Hamilton, SK
    Lima, IBT
    Novo, EMLM
    [J]. GLOBAL CHANGE BIOLOGY, 2004, 10 (05) : 530 - 544
  • [23] GLOBAL CLIMATE-CHANGE AND TERRESTRIAL NET PRIMARY PRODUCTION
    MELILLO, JM
    MCGUIRE, AD
    KICKLIGHTER, DW
    MOORE, B
    VOROSMARTY, CJ
    SCHLOSS, AL
    [J]. NATURE, 1993, 363 (6426) : 234 - 240
  • [24] Present state of global wetland extent and wetland methane modelling: conclusions from a model inter-comparison project (WETCHIMP)
    Melton, J. R.
    Wania, R.
    Hodson, E. L.
    Poulter, B.
    Ringeval, B.
    Spahni, R.
    Bohn, T.
    Avis, C. A.
    Beerling, D. J.
    Chen, G.
    Eliseev, A. V.
    Denisov, S. N.
    Hopcroft, P. O.
    Lettenmaier, D. P.
    Riley, W. J.
    Singarayer, J. S.
    Subin, Z. M.
    Tian, H.
    Zuercher, S.
    Brovkin, V.
    van Bodegom, P. M.
    Kleinen, T.
    Yu, Z. C.
    Kaplan, J. O.
    [J]. BIOGEOSCIENCES, 2013, 10 (02) : 753 - 788
  • [25] Estimating the volume and age of water stored in global lakes using a geo-statistical approach
    Messager, Mathis Loic
    Lehner, Bernhard
    Grill, Guenther
    Nedeva, Irena
    Schmitt, Oliver
    [J]. NATURE COMMUNICATIONS, 2016, 7
  • [26] Olefeldt D, 2016, ORNL DAAC, DOI 10.3334/ORNLDAAC/1332
  • [27] Interannual variability of surface water extent at the global scale, 1993-2004
    Papa, F.
    Prigent, C.
    Aires, F.
    Jimenez, C.
    Rossow, W. B.
    Matthews, E.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2010, 115
  • [28] High-resolution mapping of global surface water and its long-term changes
    Pekel, Jean-Francois
    Cottam, Andrew
    Gorelick, Noel
    Belward, Alan S.
    [J]. NATURE, 2016, 540 (7633) : 418 - +
  • [29] An image-based inventory of the spatial structure of West Siberian wetlands
    Peregon, A.
    Maksyutov, S.
    Yamagata, Y.
    [J]. ENVIRONMENTAL RESEARCH LETTERS, 2009, 4 (04):
  • [30] Modeling regional to global CH4 emissions of boreal and arctic wetlands
    Petrescu, A. M. R.
    van Beek, L. P. H.
    van Huissteden, J.
    Prigent, C.
    Sachs, T.
    Corradi, C. A. R.
    Parmentier, F. J. W.
    Dolman, A. J.
    [J]. GLOBAL BIOGEOCHEMICAL CYCLES, 2010, 24