Open AccessPrediction CH4 Emissions from the Wetlands in the Sanjiang Plain of Northeastern China in the 21st Century
Author(s) -
Tingting Li,
Qing Zhang,
Wen Zhang,
Guocheng Wang,
Yanyu Lu,
Li Yu,
Ran Zhang
Publication year - 2016
Publication title -
plos one
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.99
H-Index - 332
ISSN - 1932-6203
DOI - 10.1371/journal.pone.0158872
Subject(s) - sanjiang plain , wetland , environmental science , climate change , china , wetland conservation , vegetation (pathology) , primary production , greenhouse gas , ecosystem , hydrology (agriculture) , representative concentration pathways , physical geography , ecology , climate model , geography , marsh , geology , biology , medicine , geotechnical engineering , archaeology , pathology
The Sanjiang Plain has been experienced significant wetland loss due to expanded agricultural activities, and will be potentially restored by the China National Wetland Conservation Action Plan (NWCP) in future. The objective of this study is to evaluate the impact of future climate warming and wetland restoration on wetland CH 4 emissions in northeast China. We used an atmosphere-vegetation interaction model (AVIM2) to drive a modified biogeophysical model (CH4MOD wetland ), and projected CH 4 flux variations from the Sanjiang Plain wetlands under different Representative Concentration Pathway scenarios throughout the 21 st century. Model validation showed that the regressions between the observed and simulated CH 4 fluxes by the modified model produced an R 2 of 0.49 with a slope of 0.87 (p<0.001, n = 237). According to the AVIM2 simulation, the net primary productivity of the Sanjiang Plain wetlands will increase by 38.2 g m -2 yr -1 , 116.6 g m -2 yr -1 and 250.4 g m -2 yr -1 under RCP 2.6, RCP 4.5 and RCP 8.5, respectively, by the end of this century. For RCP 2.6, 4.5 and 8.5 scenarios, the CH 4 fluxes will increase by 5.7 g m -2 yr -1 , 57.5 g m -2 yr -1 and 112.2 g m -2 yr -1 . Combined with the wetland restoration, the regional emissions will increase by 0.18‒1.52 Tg. The CH 4 emissions will be stimulated by climate change and wetland restoration. Regional wetland restoration planning should be directed against different climate scenarios in order to suppress methane emissions.