Controls on the tropospheric oxidizing capacity during an idealized Dansgaard-Oeschger event, and their implications for the rapid rises in atmospheric methane during the last glacial period

scholarly article

Controls on the tropospheric oxidizing capacity during an idealized Dansgaard-Oeschger event, and their implications for the rapid rises in atmospheric methane during the last glacial period is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode2012GeoRL..3912805L
P356DOI10.1029/2012GL051866

P50authorPaul J. ValdesQ63932764
P2093author name stringJ. G. Levine
E. W. Wolff
P. O. Hopcroft
P2860cites workWhat caused Earth's temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivityQ24289402
Atmospheric methane and nitrous oxide of the Late Pleistocene from Antarctic ice coresQ28283878
Atmospheric oxidation capacity sustained by a tropical forestQ29353925
Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial periodQ30623431
The role of the thermohaline circulation in abrupt climate changeQ30675841
Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 yearsQ31155450
Hydrogen isotopes preclude marine hydrate CH4 emissions at the onset of Dansgaard-Oeschger eventsQ33615699
Rapid changes of glacial climate simulated in a coupled climate modelQ33934383
Late Holocene methane rise caused by orbitally controlled increase in tropical sourcesQ34162549
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changesQ34315674
HOx radical regeneration in the oxidation of isoprene.Q39346403
Changing boreal methane sources and constant biomass burning during the last terminationQ43532575
Development and Intercomparison of Condensed Isoprene Oxidation Mechanisms for Global Atmospheric ModelingQ56114934
Impacts of HOxregeneration and recycling in the oxidation of isoprene: Consequences for the composition of past, present and future atmospheresQ56749838
A global model of natural volatile organic compound emissionsQ56835371
Investigating the Causes of the Response of the Thermohaline Circulation to Past and Future Climate ChangesQ57143267
Changes in fire regimes since the Last Glacial Maximum: an assessment based on a global synthesis and analysis of charcoal dataQ57264410
Wetland methane emissions during the Last Glacial Maximum estimated from PMIP2 simulations: Climate, vegetation, and geographic controlsQ57518976
Reconciling the changes in atmospheric methane sources and sinks between the Last Glacial Maximum and the pre-industrial eraQ57589206
Systematic optimisation and climate simulation of FAMOUS, a fast version of HadCM3Q57921175
Simulating idealized Dansgaard-Oeschger events and their potential impacts on the global methane cycleQ58071024
The effects of glacial atmospheric CO2 concentrations and climate on isoprene emissions by vascular plantsQ58071094
The ice age methane budgetQ58071098
A description of the FAMOUS (version XDBUA) climate model and control runQ58073789
Modelling NOx from lightning and its impact on global chemical fieldsQ58256533
In search of an ice core signal to differentiate between source-driven and sink-driven changes in atmospheric methaneQ58264127
N2O and CH4variations during the last glacial epoch: Insight into global processesQ58265558
Changes in the atmospheric CH4gradient between Greenland and Antarctica during the Last Glacial and the transition to the HoloceneQ58265569
A global climate model study of CH4 emissions during the Holocene and glacial-interglacial transitions constrained by ice core dataQ58384563
Role of methane and biogenic volatile organic compound sources in late glacial and Holocene fluctuations of atmospheric methane concentrationsQ58397246
P433issue12
P407language of work or nameEnglishQ1860
P921main subjectmethaneQ37129
troposphereQ40631
P577publication date2012-06-28
P1433published inGeophysical Research LettersQ5535576
P1476titleControls on the tropospheric oxidizing capacity during an idealized Dansgaard-Oeschger event, and their implications for the rapid rises in atmospheric methane during the last glacial period
P478volume39

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cites work (P2860)
Q57250883Atmospheric methane variability: Centennial-scale signals in the Last Glacial Period
Q58265446Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2
Q38695401Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records
Q21558333High-resolution interpolar difference of atmospheric methane around the Last Glacial Maximum

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