globalchange  > 气候减缓与适应
DOI: 10.1002/grl.50380
论文题名:
The response of atmospheric nitrous oxide to climate variations during the last glacial period
作者: Schilt A.; Baumgartner M.; Eicher O.; Chappellaz J.; Schwander J.; Fischer H.; Stocker T.F.
刊名: Geophysical Research Letters
ISSN: 0094-9093
EISSN: 1944-8824
出版年: 2013
卷: 40, 期:9
起始页码: 1888
结束页码: 1893
语种: 英语
英文关键词: glacial ; greenhouse gas ; Heinrich event ; ice core ; NGRIP ; nitrous oxide
Scopus关键词: glacial ; Heinrich Events ; Ice core ; NGRIP ; Nitrous oxide ; Atmospheric chemistry ; Greenhouse gases ; Nitrogen oxides ; Salinity measurement ; Climate change ; climate variation ; concentration (composition) ; Dansgaard-Oeschger cycle ; glacial-interglacial cycle ; greenhouse gas ; GRIP ; Heinrich event ; Holocene ; ice core ; Last Glacial ; nitrous oxide
英文摘要: Detailed insight into natural variations of the greenhouse gas nitrous oxide (N2O) in response to changes in the Earth's climate system is provided by new measurements along the ice core of the North Greenland Ice Core Project (NGRIP). The presented record reaches from the early Holocene back into the previous interglacial with a mean time resolution of about 75years. Between 11 and 120kyrBP, atmospheric N2O concentrations react substantially to the last glacial-interglacial transition (Termination 1) and millennial time scale climate variations of the last glacial period. For long-lasting Dansgaard/Oeschger (DO) events, the N2O increase precedes Greenland temperature change by several hundred years with an increase rate of about 0.8-1.3ppbv/century, which accelerates to about 3.8-10.7ppbv/century at the time of the rapid warming in Greenland. Within each bundle of DO events, the new record further reveals particularly low N2O concentrations at the approximate time of Heinrich events. This suggests that the response of marine and/or terrestrial N2O emissions on a global scale are different for stadials with and without Heinrich events. Key Points High-resolution record of atmospheric N2O from 11 to 120 kyr BPSubstantial N2O response to the last glacial-interglacial transition (T1)DO and Heinrich event cycles visible in the atmospheric N2O concentration ©2013. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84879106864&doi=10.1002%2fgrl.50380&partnerID=40&md5=3dc55e9dbc0797634670b0e9f0613e77
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/6357
Appears in Collections:气候减缓与适应

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作者单位: Climate and Environmental Physics, Oeschger Centre for Climate Change, University of Bern, Bern, Switzerland

Recommended Citation:
Schilt A.,Baumgartner M.,Eicher O.,et al. The response of atmospheric nitrous oxide to climate variations during the last glacial period[J]. Geophysical Research Letters,2013-01-01,40(9).
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