Wind-Driven Upwelling in the Southern Ocean and the Deglacial Rise in Atmospheric CO2

By R. Anderson, Saleem H Ali, L. Bradtmiller, S. Nielsen, M. Fleisher, B. Anderson, L. Burckle. Science, 2009

1,172 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry, Oceanography

View Paper: https://www.semanticscholar.org/paper/03032d41bd5fa89157a0ce69b47cedb322a96db5

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The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Ryan Abernathey
2. Hans Renssen
3. P. Ceppi
4. Hugues Goosse
5. D. Frierson
6. D. Hartmann
7. David Ferreira
8. John Marshall

In Environmental Chemistry

1. Hugues Goosse
2. Hans Renssen
3. A. Ganopolski
4. F. Joos
5. R. Roth
6. D. Roche
7. X. Crosta
8. Heikki Seppä

In Oceanography

1. Ryan Abernathey
2. David Ferreira
3. John Marshall
4. D. Hartmann
5. A. Ganopolski
6. F. Joos
7. P. Ceppi
8. Hugues Goosse

Citations in the corpus

• Extratropical Cooling, Interhemispheric Thermal Gradients, and Tropical Climate Change (2012, positive): “A recent study by Lee et al. (2011) offers such an example: Using an AGCM, they explored the hypothesis of an impact on the SH westerlies from North Atlantic cooling as suggested by Anderson et al. (2009).”
• The last deglaciation: timing the bipolar seesaw (2011, background): “…may represent a more rapid response of the near-coastal records used in the composite to the observed changes in Southern Ocean conditions (e.g. Anderson et al., 2009) and/or sea ice extent (e.g. Bianchi and Gersonde, 2004), which can cause changes in δ 18 O ice by affecting cy-clogenesis, the…”
• The Dependence of Southern Ocean Meridional Overturning on Wind Stress (2011, background): “Such wind-induced changes in the MOC could help regulate glacial–interglacial cycles by venting CO2 from the deep ocean to the atmosphere (Toggweiler and Russell 2008; Anderson et al. 2009; Marshall and Speer 2011).”
• A reconstruction of radiocarbon production and total solar irradiance from the Holocene 14 C and CO 2 records: implications of data and model uncertainties (2013, background): “…the termination as suggested by a range of proxy data (e.g.Franois et al., 1997; Adkins et al., 2002; Hodell et al., 2003; Galbraith et al., 2007; Anderson et al., 2009; Schmitt et al., 2012; Burke and Robinson, 2012) and modelling work (e.g.Tschumi et al., 2011); (iii) a range of mechanisms…”
• Glacial CO2 cycle as a succession of key physical and biogeochemical processes (2011, background): “This, in turn, is primarily related to the enhanced sea ice formation in the Southern Ocean, stronger brine rejection and an increase of the AABW salinity (Brovkin et al., 2007).”
• The relationship between the ITCZ and the Southern Hemispheric eddy‐driven jet (2013, background): “…of the ITCZ and of the eddy-driven westerlies in the context of ice age terminations, where the ITCZ shift may have been forced mainly from the Northern Hemisphere (NH) [Anderson et al., 2009; Toggweiler and 1Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA.”
• Global characterization of the Holocene Thermal Maximum (2012, background): “, 2004; Anderson et al., 2009). Denis et al. (2010) relate this latitudinal contrast to a strong sensitivity to the latitudinal temperature gradient.”