Chen, WN; Zhang, FY; Wang, BX; Wang, JS; Tian, DS; Han, GX
![](http://ir.yic.ac.cn/image/person.jpg)
发表期刊JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
![](http://ir.yic.ac.cn/image/waiting.gif)
ISSN2169-8953
2019-06
卷号124期号:6页码:1731-1745
关键词NITROUS-OXIDEATMOSPHERIC METHANECARBON-DIOXIDETIBETAN PLATEAUCLIMATE-CHANGEN2O FLUXESEMISSIONSCH4SOILSGRASSLANDS
研究领域Environmental Sciences; Geosciences, Multidisciplinary
DOI10.1029/2019JG005011
产权排序[Chen, Weinan; Zhang, Fangyue; Wang, Bingxue; Wang, Jinsong; Tian, Dashuan; Wen, Xuefa; Yu, Guirui; Niu, Shuli] Chinese Acad Sci, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China; [Chen, Weinan; Zhang, Fangyue; Wen, Xuefa; Yu, Guirui; Niu, Shuli] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing, Peoples R China; [Han, Guangxuan] Chinese Acad Sci, Key Lab Coastal Environm Processes & Ecol Remedia, Yantai Inst Coastal Zone Res, Yantai, Peoples R China
通讯作者Niu, Shuli(sniu@igsnrr.ac.cn)
作者部门海岸带环境过程实验室
英文摘要Temporal variations of methane flux (FCH4) and its underlying mechanisms still remain poorly understood. To quantify diurnal and seasonal patterns of FCH4 and investigate its determinants, we monitored FCH4 using eddy covariance in an alpine meadow on the Qinghai-Tibetan Plateau, China, from June 2015 to December 2016. As a strong CH4 sink, the alpine meadow on the Qinghai-Tibetan Plateau consumed 0.41 0.04 Tg CH4/year. There was an obvious diurnal pattern with more CH4 uptakes during the nighttime than the daytime for both growing and nongrowing season. The diurnal FCH4 during the growing and nongrowing season were positively correlated with air temperature (Ta), volumetric water content, friction velocity (u(*)), and vapor pressure deficit. The growing season FCH4 showed a significant quadratic polynomial relationship with the canopy conductance (G(w)) and gross primary production). FCH4 was significantly higher in the growing season than in the nongrowing season. The seasonal FCH4 was negatively correlated with soil temperature and net radiation (Rn) but not with volumetric water content and gross primary production. Ridge regression models indicated that Ta and u(*) explained 83% of the variation in the diel dynamics of FCH4 during the growing season and explained 72% of the variation during the nongrowing season. Rn accounted for 49% of variations of FCH4 at the seasonal scale. The temporal patterns and the environmental controlling factors revealed in this study may improve model parameterization for biosphere-atmosphere CH4 exchange simulation as well as the methane budget estimation. Plain Language Summary Methane (CH4) is a very important greenhouse gas, responsible for about 20% of the warming induced by long-lived greenhouse gases since 1750, and its impact is second only after carbon dioxide (CO2). However, we know much less about CH4 compared to CO2. Many basic but important questions about CH4 still remain unanswered, such as the diurnal and seasonal patterns of CH4 flux as well as the controlling factors of these temporal dynamics of CH4 flux. To answer these questions, we monitored the CH4 flux continuously in an alpine meadow ecosystem located on the eastern Qinghai-Tibetan Plateau, China, from June 2015 to December 2016. At the diurnal scale, we found that the CH4 uptake at nighttime was higher than at daytime. At the seasonal scale, we found higher CH4 uptake during summer than winter. We also found that CH4 fluxes were determined by air temperature and net radiation at the diurnal scale and seasonal scale, respectively. The temporal patterns and the controlling factors revealed in this study may help to improve the prediction of CH4 exchange processes and the estimation of methane budget from the regional to the global scale.
文章类型Article
资助机构National Key R&D Program of China [2017YFA0604801]; National Natural Science Foundation of ChinaNational Natural Science Foundation of China [31625006]; Ministry of Science and Technology of ChinaMinistry of Science and Technology, China [2016YFC0501803]; CAS international collaboration program [131A11KYSB20180010]; National Earth System Science Data Sharing Infrastructure, National Science & Technology Infrastructure of China
收录类别SCI
语种英语
关键词[WOS]NITROUS-OXIDE; ATMOSPHERIC METHANE; CARBON-DIOXIDE; TIBETAN PLATEAU; CLIMATE-CHANGE; N2O FLUXES; EMISSIONS; CH4; SOILS; GRASSLANDS
研究领域[WOS]Environmental Sciences; Geosciences, Multidisciplinary
WOS记录号WOS:000477719400022
引用统计被引频次:6[WOS][WOS记录][WOS相关记录]
文献类型期刊论文
条目标识符http://ir.yic.ac.cnhttp://ir.yic.ac.cn/handle/133337/24926
专题中科院海岸带环境过程与生态修复重点实验室_海岸带环境过程实验室
中科院海岸带环境过程与生态修复重点实验室
作者单位1.Chinese Acad Sci, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China;
2.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing, Peoples R China;
3.Chinese Acad Sci, Key Lab Coastal Environm Processes & Ecol Remedia, Yantai Inst Coastal Zone Res, Yantai, Peoples R China
推荐引用方式
GB/T 7714Chen, WN,Zhang, FY,Wang, BX,et al. Diel and Seasonal Dynamics of Ecosystem-Scale Methane Flux and Their Determinants in an Alpine Meadow[J]. JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES,2019,124(6):1731-1745.
APAChen, WN.,Zhang, FY.,Wang, BX.,Wang, JS.,Tian, DS.,...&Niu, SL.(2019).Diel and Seasonal Dynamics of Ecosystem-Scale Methane Flux and Their Determinants in an Alpine Meadow.JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES,124(6),1731-1745.
MLAChen, WN,et al."Diel and Seasonal Dynamics of Ecosystem-Scale Methane Flux and Their Determinants in an Alpine Meadow".JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES 124.6(2019):1731-1745.
PDF全文下载地址:
点我下载PDF