AGW Observer

Observations of anthropogenic global warming

Papers on 1940s dip in atmospheric CO2

Posted by Ari Jokimäki on December 1, 2011

This is a list of papers on 1940s dip in atmospheric CO2 concentration. The list is not complete, and will most likely be updated in the future in order to make it more thorough and more representative.

Update: (February 1, 2016) Rubino et al. (2013) added.

A revised 1000 year atmospheric δ13C-CO2 record from Law Dome and South Pole, Antarctica – Rubino et al. (2013) “We present new measurements of δ13C of CO2 extracted from a high-resolution ice core from Law Dome (East Antarctica), together with firn measurements performed at Law Dome and South Pole, covering the last 150 years. Our analysis is motivated by the need to better understand the role and feedback of the carbon (C) cycle in climate change, by advances in measurement methods, and by apparent anomalies when comparing ice core and firn air δ13C records from Law Dome and South Pole. We demonstrate improved consistency between Law Dome ice, South Pole firn, and the Cape Grim (Tasmania) atmospheric δ13C data, providing evidence that our new record reliably extends direct atmospheric measurements back in time. We also show a revised version of early δ13C measurements covering the last 1000 years, with a mean preindustrial level of −6.50‰. Finally, we use a Kalman Filter Double Deconvolution to infer net natural CO2 fluxes between atmosphere, ocean, and land, which cause small δ13C deviations from the predominant anthropogenically induced δ13C decrease. The main features found from the previous δ13C record are confirmed, including the ocean as the dominant cause for the 1940 A.D. CO2 leveling. Our new record provides a solid basis for future investigation of the causes of decadal to centennial variations of the preindustrial atmospheric CO2 concentration. Those causes are of potential significance for predicting future CO2 levels and when attempting atmospheric verification of recent and future global carbon emission mitigation measures through Coupled Climate Carbon Cycle Models.” Rubino, M., et al. (2013), A revised 1000 year atmospheric δ13C-CO2 record from Law Dome and South Pole, Antarctica, J. Geophys. Res. Atmos., 118, 8482–8499, doi:10.1002/jgrd.50668. [Full text]

Climate effects on atmospheric carbon dioxide over the last century – Rafelski et al. (2009) “The buildup of atmospheric CO2 since 1958 is surprisingly well explained by the simple premise that 57% of the industrial emissions (fossil fuel burning and cement manufacture) has remained airborne. This premise accounts well for the rise both before and after 1980 despite a decrease in the growth rate of fossil fuel CO2 emissions, which occurred at that time, and by itself should have caused the airborne fraction to decrease. In contrast, the buildup prior to 1958 was not simply proportional to cumulative fossil fuel emissions, and notably included a period during the 1940s when CO2 growth stalled despite continued fossil fuel emissions. Here we show that the constancy of the airborne fraction since 1958 can be in part explained by decadal variations in global land air temperature, which caused a warming-induced release of CO2 from the land biosphere to the atmosphere. We also show that the 1940s plateau may be related to these decadal temperature variations. Furthermore, we show that there is a close connection between the phenomenology producing CO2 variability on multidecadal and El Niño timescales.” Lauren Elmegreen Rafelski, Stephen C. Piper, Ralph F. Keeling, Tellus B, Volume 61, Issue 5, pages 718–731, November 2009, DOI: 10.1111/j.1600-0889.2009.00439.x.

Law Dome CO2, CH4 and N2O ice core records extended to 2000 years BP – MacFarling Meure et al. (2006) “New measurements of atmospheric greenhouse gas concentrations in ice from Law Dome, Antarctica reproduce published Law Dome CO2 and CH4 records, extend them back to 2000 years BP, and include N2O. They have very high air age resolution, data density and measurement precision. Firn air measurements span the past 65 years and overlap with the ice core and direct atmospheric observations. Major increases in CO2, CH4 and N2O concentrations during the past 200 years followed a period of relative stability beforehand. Decadal variations during the industrial period include the stabilization of CO2 and slowing of CH4 and N2O growth in the 1940s and 1950s. Variations of up to 10 ppm CO2, 40 ppb CH4 and 10 ppb N2O occurred throughout the preindustrial period. Methane concentrations grew by 100 ppb from AD 0 to 1800, possibly due to early anthropogenic emissions.” MacFarling Meure, C., D. Etheridge, C. Trudinger, P. Steele, R. Langenfelds, T. van Ommen, A. Smith, and J. Elkins (2006), Geophys. Res. Lett., 33, L14810, doi:10.1029/2006GL026152.

Role of land cover changes for atmospheric CO2 increase and climate change during the last 150 years – Brovkin et al. (2004) Not mentioned in the abstract, but in the article they say: “The period between 1938 and 1950 is interesting because of an almost constant atmospheric CO2 recorded at Law Dome, despite substantial fossil fuel emissions (about 1.3 PgCyr-1). … We conclude that the stalling of atmospheric CO2 during the 1940s was unlikely to have been caused by changes in land cover, although this might be one of the contributing factors. Other factors, like internal variability of the climate system, may also be responsible (Joos et al., 1999). Better statistics for land cover changes during the 1940s would help to clarify the role of land cover changes in this period.” Victor Brovkin, Stephen Sitch, Werner Von Bloh, Martin Claussen, Eva Bauer, Wolfgang Cramer, Global Change Biology, Volume 10, Issue 8, pages 1253–1266, August 2004, DOI: 10.1111/j.1365-2486.2004.00812.x. [Full text]

Kalman filter analysis of ice core data 2. Double deconvolution of CO2 and δ13C measurements – Trudinger et al. (2002) “A new method for deconvolving ice core CO2 and δ13CO2 measurements to estimate net CO2 uptake by the terrestrial biosphere and the oceans has been developed. The method, which uses the Kalman filter, incorporates statistical analysis into the calculation. This allows a more rigorous analysis of CO2 variability than the usual deconvolution method. The Kalman filter method estimates uncertainties on the deduced fluxes as part of the calculation. The deconvolution method is applied to the Law Dome CO2 and δ13C ice core record. The calculation suggests that natural variability in CO2 fluxes may be as large as 1 GtC yr−1 (GtC is gigatonnes carbon, 1 Gt = 1015 g) on the timescale of just less than a decade. The Law Dome CO2 measurements show a slight decrease in CO2 around the 1940s. Analysis with the carbon cycle model and a numerical model of firn processes suggests that about 3 GtC yr−1 uptake (mostly oceanic) is required in the 1940s to match the ice core measurements. The estimates of variation in the terrestrial biospheric flux between 1950 and 1980 from the double deconvolution calculation are in very good agreement with an independent estimate of the global terrestrial flux from a climate-driven ecosystem model.” Trudinger, C. M., I. G. Enting, P. J. Rayner, and R. J. Francey (2002), J. Geophys. Res., 107(D20), 4423, doi:10.1029/2001JD001112.

Biotic Feedbacks in the Warming of the Earth – Woodwell et al. (1998) Not mentioned in the abstract, but in the article they say: “Except for the brief period 1935–1945 heat-trapping gases continued to accumulate in the atmosphere (Etheridge et al., 1996). The coincidence between the cooling and the brief stabilization of concentration around 1940 is, perhaps, significant.” G. M. Woodwell, F. T. Mackenzie, R. A. Houghton, M. Apps, E. Gorham and E. Davidson, Climatic Change, Volume 40, Numbers 3-4, 495-518, DOI: 10.1023/A:1005345429236. [Full text]

Terrestrial carbon storage during the past 200 years: A Monte Carlo Analysis of CO2 data from ice core and atmospheric measurements – Bruno & Joos (1997) Issue is mentioned here and there in the article. Bruno, M., and F. Joos (1997), Global Biogeochem. Cycles, 11(1), 111–124, doi:10.1029/96GB03611. [Full text]

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