West Antarctic Ice Sheet (WAIS) Divide ice core ultra-high resolution continuous CH4 measurements 67.2-9.8 ka BP ...
Rhodes et al. 2015 (doi:10.1126/science.1262005)The causal mechanisms responsible for the abrupt climate changes of the Last Glacial Period remain unclear. One major difficulty is dating ice rafted debris (IRD) deposits associated with Heinrich events: Extensive icebergs influxes into the North Atla...
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ftdatacite:10.1594/pangaea.875982 2024-09-15T17:47:12+00:00 West Antarctic Ice Sheet (WAIS) Divide ice core ultra-high resolution continuous CH4 measurements 67.2-9.8 ka BP ... Rhodes, Rachael H Brook, Edward J Blunier, Thomas McConnell, Joseph R Romanini, Daniele 2017 application/zip https://dx.doi.org/10.1594/pangaea.875982 https://doi.pangaea.de/10.1594/PANGAEA.875982 en eng PANGAEA https://dx.doi.org/10.1126/science.1262005 https://dx.doi.org/10.1002/2016gb005570 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 article Collection Supplementary Publication Series of Datasets 2017 ftdatacite https://doi.org/10.1594/pangaea.87598210.1126/science.126200510.1002/2016gb005570 2024-08-01T11:01:20Z Rhodes et al. 2015 (doi:10.1126/science.1262005)The causal mechanisms responsible for the abrupt climate changes of the Last Glacial Period remain unclear. One major difficulty is dating ice rafted debris (IRD) deposits associated with Heinrich events: Extensive icebergs influxes into the North Atlantic Ocean, linked to global impacts on climate and biogeochemistry. In a new ice core record of atmospheric methane with ultra-high temporal resolution, we find abrupt methane increases within Heinrich stadials 1, 2, 4 and 5 that, uniquely, have no counterparts in Greenland temperature proxies. Using a heuristic model of tropical rainfall distribution, we propose that Hudson Strait Heinrich events caused rainfall intensification over Southern Hemisphere land areas, thereby producing excess methane in tropical wetlands. Our findings suggest that the climatic impacts of Heinrich events persisted for 740 to 1520 years.---Rhodes et al. 2017 (doi:10.1002/2016GB005570)In order to understand atmospheric methane (CH_4) ... : For more information please contact Prof. Edward Brook, Oregon State University (mailto:brooke@geo.oregonstate.edu)In the majority of cases the 2-yearly spline fit will be the most suitable for your application. -- 2 yearly cubic smoothing spline of CH_4 data from the WAIS Divide ice core: 2 yearly cubic smoothing spline fit to the "Experiment-time-integrated CH4 data from all 3 instruments" (Dataset doi:10.1594/PANGAEA.875980). The 2 yearly cubic smoothing spline fills gaps in the data set and reduces data set size, whilst also reducing noise (that could be noise linked to the wider analytical system e.g., pressure fluctuations, or archival noise that does not reflect the paleo-atmosphere).-- Experiment-time integrated data: Data integrated to the optimal integration time (n.b. where time refers to experiment time, not age of gas sample). No further smoothing or resampling algorithm has been applied. The optimal integration time was selected by performing an Allan variance test on measurements of a ... Article in Journal/Newspaper Antarc* Antarctic Greenland Hudson Strait ice core Ice Sheet Iceberg* North Atlantic DataCite |
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language |
English |
description |
Rhodes et al. 2015 (doi:10.1126/science.1262005)The causal mechanisms responsible for the abrupt climate changes of the Last Glacial Period remain unclear. One major difficulty is dating ice rafted debris (IRD) deposits associated with Heinrich events: Extensive icebergs influxes into the North Atlantic Ocean, linked to global impacts on climate and biogeochemistry. In a new ice core record of atmospheric methane with ultra-high temporal resolution, we find abrupt methane increases within Heinrich stadials 1, 2, 4 and 5 that, uniquely, have no counterparts in Greenland temperature proxies. Using a heuristic model of tropical rainfall distribution, we propose that Hudson Strait Heinrich events caused rainfall intensification over Southern Hemisphere land areas, thereby producing excess methane in tropical wetlands. Our findings suggest that the climatic impacts of Heinrich events persisted for 740 to 1520 years.---Rhodes et al. 2017 (doi:10.1002/2016GB005570)In order to understand atmospheric methane (CH_4) ... : For more information please contact Prof. Edward Brook, Oregon State University (mailto:brooke@geo.oregonstate.edu)In the majority of cases the 2-yearly spline fit will be the most suitable for your application. -- 2 yearly cubic smoothing spline of CH_4 data from the WAIS Divide ice core: 2 yearly cubic smoothing spline fit to the "Experiment-time-integrated CH4 data from all 3 instruments" (Dataset doi:10.1594/PANGAEA.875980). The 2 yearly cubic smoothing spline fills gaps in the data set and reduces data set size, whilst also reducing noise (that could be noise linked to the wider analytical system e.g., pressure fluctuations, or archival noise that does not reflect the paleo-atmosphere).-- Experiment-time integrated data: Data integrated to the optimal integration time (n.b. where time refers to experiment time, not age of gas sample). No further smoothing or resampling algorithm has been applied. The optimal integration time was selected by performing an Allan variance test on measurements of a ... |
format |
Article in Journal/Newspaper |
author |
Rhodes, Rachael H Brook, Edward J Blunier, Thomas McConnell, Joseph R Romanini, Daniele |
spellingShingle |
Rhodes, Rachael H Brook, Edward J Blunier, Thomas McConnell, Joseph R Romanini, Daniele West Antarctic Ice Sheet (WAIS) Divide ice core ultra-high resolution continuous CH4 measurements 67.2-9.8 ka BP ... |
author_facet |
Rhodes, Rachael H Brook, Edward J Blunier, Thomas McConnell, Joseph R Romanini, Daniele |
author_sort |
Rhodes, Rachael H |
title |
West Antarctic Ice Sheet (WAIS) Divide ice core ultra-high resolution continuous CH4 measurements 67.2-9.8 ka BP ... |
title_short |
West Antarctic Ice Sheet (WAIS) Divide ice core ultra-high resolution continuous CH4 measurements 67.2-9.8 ka BP ... |
title_full |
West Antarctic Ice Sheet (WAIS) Divide ice core ultra-high resolution continuous CH4 measurements 67.2-9.8 ka BP ... |
title_fullStr |
West Antarctic Ice Sheet (WAIS) Divide ice core ultra-high resolution continuous CH4 measurements 67.2-9.8 ka BP ... |
title_full_unstemmed |
West Antarctic Ice Sheet (WAIS) Divide ice core ultra-high resolution continuous CH4 measurements 67.2-9.8 ka BP ... |
title_sort |
west antarctic ice sheet (wais) divide ice core ultra-high resolution continuous ch4 measurements 67.2-9.8 ka bp ... |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://dx.doi.org/10.1594/pangaea.875982 https://doi.pangaea.de/10.1594/PANGAEA.875982 |
genre |
Antarc* Antarctic Greenland Hudson Strait ice core Ice Sheet Iceberg* North Atlantic |
genre_facet |
Antarc* Antarctic Greenland Hudson Strait ice core Ice Sheet Iceberg* North Atlantic |
op_relation |
https://dx.doi.org/10.1126/science.1262005 https://dx.doi.org/10.1002/2016gb005570 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.87598210.1126/science.126200510.1002/2016gb005570 |
_version_ |
1810496057487917056 |