scholarly article | Q13442814 |
P819 | ADS bibcode | 2012GeoRL..3912805L |
P356 | DOI | 10.1029/2012GL051866 |
P50 | author | Paul J. Valdes | Q63932764 |
P2093 | author name string | J. G. Levine | |
E. W. Wolff | |||
P. O. Hopcroft | |||
P2860 | cites work | What caused Earth's temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivity | Q24289402 |
Atmospheric methane and nitrous oxide of the Late Pleistocene from Antarctic ice cores | Q28283878 | ||
Atmospheric oxidation capacity sustained by a tropical forest | Q29353925 | ||
Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period | Q30623431 | ||
The role of the thermohaline circulation in abrupt climate change | Q30675841 | ||
Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years | Q31155450 | ||
Hydrogen isotopes preclude marine hydrate CH4 emissions at the onset of Dansgaard-Oeschger events | Q33615699 | ||
Rapid changes of glacial climate simulated in a coupled climate model | Q33934383 | ||
Late Holocene methane rise caused by orbitally controlled increase in tropical sources | Q34162549 | ||
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes | Q34315674 | ||
HOx radical regeneration in the oxidation of isoprene. | Q39346403 | ||
Changing boreal methane sources and constant biomass burning during the last termination | Q43532575 | ||
Development and Intercomparison of Condensed Isoprene Oxidation Mechanisms for Global Atmospheric Modeling | Q56114934 | ||
Impacts of HOxregeneration and recycling in the oxidation of isoprene: Consequences for the composition of past, present and future atmospheres | Q56749838 | ||
A global model of natural volatile organic compound emissions | Q56835371 | ||
Investigating the Causes of the Response of the Thermohaline Circulation to Past and Future Climate Changes | Q57143267 | ||
Changes in fire regimes since the Last Glacial Maximum: an assessment based on a global synthesis and analysis of charcoal data | Q57264410 | ||
Wetland methane emissions during the Last Glacial Maximum estimated from PMIP2 simulations: Climate, vegetation, and geographic controls | Q57518976 | ||
Reconciling the changes in atmospheric methane sources and sinks between the Last Glacial Maximum and the pre-industrial era | Q57589206 | ||
Systematic optimisation and climate simulation of FAMOUS, a fast version of HadCM3 | Q57921175 | ||
Simulating idealized Dansgaard-Oeschger events and their potential impacts on the global methane cycle | Q58071024 | ||
The effects of glacial atmospheric CO2 concentrations and climate on isoprene emissions by vascular plants | Q58071094 | ||
The ice age methane budget | Q58071098 | ||
A description of the FAMOUS (version XDBUA) climate model and control run | Q58073789 | ||
Modelling NOx from lightning and its impact on global chemical fields | Q58256533 | ||
In search of an ice core signal to differentiate between source-driven and sink-driven changes in atmospheric methane | Q58264127 | ||
N2O and CH4variations during the last glacial epoch: Insight into global processes | Q58265558 | ||
Changes in the atmospheric CH4gradient between Greenland and Antarctica during the Last Glacial and the transition to the Holocene | Q58265569 | ||
A global climate model study of CH4 emissions during the Holocene and glacial-interglacial transitions constrained by ice core data | Q58384563 | ||
Role of methane and biogenic volatile organic compound sources in late glacial and Holocene fluctuations of atmospheric methane concentrations | Q58397246 | ||
P433 | issue | 12 | |
P407 | language of work or name | English | Q1860 |
P921 | main subject | methane | Q37129 |
troposphere | Q40631 | ||
P577 | publication date | 2012-06-28 | |
P1433 | published in | Geophysical Research Letters | Q5535576 |
P1476 | title | 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 | |
P478 | volume | 39 |
Q57250883 | Atmospheric methane variability: Centennial-scale signals in the Last Glacial Period |
Q58265446 | Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2 |
Q38695401 | Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records |
Q21558333 | High-resolution interpolar difference of atmospheric methane around the Last Glacial Maximum |
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