The response of atmospheric nitrous oxide to climate variations during the last glacial period
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 i...
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ftoregonstate:ir.library.oregonstate.edu:qv33s272s 2024-09-15T18:09:07+00:00 The response of atmospheric nitrous oxide to climate variations during the last glacial period Schilt, Adrian Baumgartner, Matthias Eicher, Olivier Chappellaz, Jérôme Schwander, Jakob Fischer, Hubertus Stocker, Thomas F. https://ir.library.oregonstate.edu/concern/articles/qv33s272s English [eng] eng unknown American Geophysical Union https://ir.library.oregonstate.edu/concern/articles/qv33s272s Copyright Not Evaluated Article ftoregonstate 2024-07-22T18:06:06Z 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 75 years. Between 11 and 120 kyr BP, 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 0.8-1.3 ppbv/century, which accelerates to about 3.8-10.7 ppbv/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. Keywords: N2O, Variability, Lifetimes, Ocean circulation, Late pleistocene, Millennial scale, Monsoon, Record, North Atlantic, Ice cores Keywords: N2O, Variability, Lifetimes, Ocean circulation, Late pleistocene, Millennial scale, Monsoon, Record, North Atlantic, Ice cores Article in Journal/Newspaper Greenland Greenland ice core Greenland Ice core Project ice core NGRIP North Atlantic North Greenland North Greenland Ice Core Project ScholarsArchive@OSU (Oregon State University) |
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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 75 years. Between 11 and 120 kyr BP, 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 0.8-1.3 ppbv/century, which accelerates to about 3.8-10.7 ppbv/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. Keywords: N2O, Variability, Lifetimes, Ocean circulation, Late pleistocene, Millennial scale, Monsoon, Record, North Atlantic, Ice cores Keywords: N2O, Variability, Lifetimes, Ocean circulation, Late pleistocene, Millennial scale, Monsoon, Record, North Atlantic, Ice cores |
format |
Article in Journal/Newspaper |
author |
Schilt, Adrian Baumgartner, Matthias Eicher, Olivier Chappellaz, Jérôme Schwander, Jakob Fischer, Hubertus Stocker, Thomas F. |
spellingShingle |
Schilt, Adrian Baumgartner, Matthias Eicher, Olivier Chappellaz, Jérôme Schwander, Jakob Fischer, Hubertus Stocker, Thomas F. The response of atmospheric nitrous oxide to climate variations during the last glacial period |
author_facet |
Schilt, Adrian Baumgartner, Matthias Eicher, Olivier Chappellaz, Jérôme Schwander, Jakob Fischer, Hubertus Stocker, Thomas F. |
author_sort |
Schilt, Adrian |
title |
The response of atmospheric nitrous oxide to climate variations during the last glacial period |
title_short |
The response of atmospheric nitrous oxide to climate variations during the last glacial period |
title_full |
The response of atmospheric nitrous oxide to climate variations during the last glacial period |
title_fullStr |
The response of atmospheric nitrous oxide to climate variations during the last glacial period |
title_full_unstemmed |
The response of atmospheric nitrous oxide to climate variations during the last glacial period |
title_sort |
response of atmospheric nitrous oxide to climate variations during the last glacial period |
publisher |
American Geophysical Union |
url |
https://ir.library.oregonstate.edu/concern/articles/qv33s272s |
genre |
Greenland Greenland ice core Greenland Ice core Project ice core NGRIP North Atlantic North Greenland North Greenland Ice Core Project |
genre_facet |
Greenland Greenland ice core Greenland Ice core Project ice core NGRIP North Atlantic North Greenland North Greenland Ice Core Project |
op_relation |
https://ir.library.oregonstate.edu/concern/articles/qv33s272s |
op_rights |
Copyright Not Evaluated |
_version_ |
1810446529697153024 |