Export 3 results:
Sort by: Author Title Type [ Year  (Desc)]
Schilt, A, Brook EJ, Bauska TK, Baggenstos D, Fischer H, Joos F, Petrenko VV, Schaefer H, Schmitt J, Severinghaus JP, Spahni R, Stocker TF.  2014.  Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation. Nature. 516:234-+.   10.1038/nature13971   AbstractWebsite

Nitrous oxide (N2O) is an important greenhouse gas and ozone-depleting substance that has anthropogenic as well as natural marine and terrestrial sources(1). The tropospheric N2O concentrations have varied substantially in the past in concert with changing climate on glacial-interglacial and millennial timescales(2-8). It is not well understood, however, how N2O emissions from marine and terrestrial sources change in response to varying environmental conditions. The distinct isotopic compositions of marine and terrestrial N2O sources can help disentangle the relative changes in marine and terrestrial N2O emissions during past climate variations(4,9,10). Here we present N2O concentration and isotopic data for the last deglaciation, from 16,000 to 10,000 years before present, retrieved from air bubbles trapped in polar ice at Taylor Glacier, Antarctica. With the help of our data and a box model of the N2O cycle, we find a 30 per cent increase in total N2O emissions from the late glacial to the interglacial, with terrestrial and marine emissions contributing equally to the overall increase and generally evolving in parallel over the last deglaciation, even though there is no a priori connection between the drivers of the two sources. However, we find that terrestrial emissions dominated on centennial timescales, consistent with a state-of-the-art dynamic global vegetation and land surface process model that suggests that during the last deglaciation emission changes were strongly influenced by temperature and precipitation patterns over land surfaces. The results improve our understanding of the drivers of natural N2O emissions and are consistent with the idea that natural N2O emissions will probably increase in response to anthropogenic warming(11).

Kobashi, T, Severinghaus JP, Barnola JM.  2008.  4 +/- 1.5 degrees C abrupt warming 11,270 yr ago identified from trapped air in Greenland ice. Earth and Planetary Science Letters. 268:397-407.   10.1016/j.epsl.2008.01.032   AbstractWebsite

Nitrogen and argon isotopes in air trapped in a Greenland ice core (GISP2) show two prominent peaks in the interval 11,800-10,800 B.P., which indicate two large abrupt warming events. The first abrupt wanning (10 +/- 4 degrees C) is the widely documented event at the end of the Younger Dryas. Here, we report on the second abrupt warming (4 +/- 1.5 degrees C), which occurred at the end of a short lived cooler interval known as the Preboreal Oscillation (11,270 +/- 30 B.P.). A rapid snow accumulation increase suggests that the climatic transition may have occurred within a few years. The character of the Preboreal Oscillation and the subsequent abrupt warming is similar to the Dansgaard-Oeschger (D/O) events in the last glacial period, suggestive of a common mechanism, but different from another large climate change at 8,200 B.P., in which cooling was abrupt but subsequent warming was gradual. The large abrupt warming at 11,270 B.P. may be considered to be the final D/O event prior to the arrival of the present stable and warm epoch. (c) 2008 Elsevier B.V. All rights reserved.

Kobashi, T, Severinghaus JP, Brook EJ, Barnola JM, Grachev AM.  2007.  Precise timing and characterization of abrupt climate change 8200 years ago from air trapped in polar ice. Quaternary Science Reviews. 26:1212-1222.   10.1016/j.quascirev.2007.01.009   AbstractWebsite

How fast and how much climate can change has significant implications for concerns about future climate changes and their potential impacts on society. An abrupt climate change 8200 years ago (8.2 ka event) provides a test case to understand possible future climatic variability. Here, methane concentration (taken as an indicator for terrestrial hydrology) and nitrogen isotopes (Greenland temperature) in trapped air in a Greenland ice core (GISP2) are employed to scrutinize the evolution of the 8.2 ka event. The synchronous change in methane and nitrogen implies that the 8.2 ka event was a synchronous event (within +/- 4 years) at a hemispheric scale, as indicated by recent climate model results [Legrande, A. N., Schmidt, G. A., Shindell, D. T., Field, C. V., Miller, R. L., Koch, D. M., Faluvegi, G., Hoffmann, G., 2006. Consistent simulations of multiple proxy responses to an abrupt climate change event. Proceedings of the National Academy of Sciences 103, 837-842]. The event began with a large-scale general cooling and drying around similar to 8175 +/- 30 years BP (Before Present, where Present is 1950 AD). Greenland temperature cooled by 3.3 +/- 1.1 degrees C (decadal average) in less than similar to 20 years, and atmospheric methane concentration decreased by similar to 80 +/- 25 ppb over similar to 40 years, corresponding to a 15 +/- 5% emission reduction. Hemispheric scale cooling and drying.. inferred from many paleoclimate proxies, likely contributed to this emission reduction. In central Greenland, the coldest period lasted for similar to 60 years, interrupted by a milder interval of a few decades, and temperature subsequently warmed in several steps over similar to 70 years. The total duration of the 8.2 ka event was roughly 150 years. (c) 2007 Elsevier Ltd. All rights reserved.