Glacial-interglacial evolution of greenhouse gases as inferred from ice core analysis: A review of recent results
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Orbital insolation, ice volume, and greenhouse gases
2003, Quaternary Science ReviewsCitation Excerpt :For example, CH4 changes are likely to be part of the forcing of the δD (air temperature) response at Vostok (Fig. 11). Raynaud et al. (1992) estimated that the total glacial–interglacial temperature impact of CH4 accounted for 20–25% of the combined effects from CO2 and CH4. Most of this glacial–interglacial CH4 signal is at 23,000 years (Fig. 4).
Effects of volcanic eruptions on the CO<inf>2</inf> content of the atmosphere and the oceans: The 1996 eruption and flood within the Vatnajökull Glacier, Iceland
2002, Chemical GeologyCitation Excerpt :These eruptions, and their timing, winter vs. summer, could have played a role in the observed fluctuations of atmospheric CO2 during the waning stage of the last glaciation (Raynaud et al., 1992; Beerling et al., 1995).
The case for human causes of increased atmospheric CH<inf>4</inf> over the last 5000 years
2001, Quaternary Science ReviewsVolcanic and anthropogenic contributions to global weathering budgets
1998, Journal of Geochemical ExplorationPaleoproductivity of the Indian Ocean during the Tertiary Period
1995, Global and Planetary ChangePaleoproductivity and deep-sea oxygenation in Cosmonaut Sea since the last glacial maximum: impact on atmospheric CO<inf>2</inf>
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