Changes in the carbon cycle during the last deglaciation as indicated by the comparison of 10Be and 14C records

By R. Muscheler, J. Beer, G. Wagner, C. Laj, C. Kissel, G. Raisbeck, F. Yiou, P. Kubik. 2004

210 citations recorded by the source corpus.

Subfields: Atmospheric Science, Molecular Biology, Paleontology

View Paper: https://www.semanticscholar.org/paper/53fc81a4f31b11fed2f39b33ce50d9ca14d00821

How researchers see this paper

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

In Atmospheric Science

1. I. Usoskin
2. R. Muscheler
3. M. Vonmoos
4. Hans Renssen
5. R. Holme
6. Hugues Goosse
7. J. Beer
8. Monika Korte

In Molecular Biology

1. I. Usoskin
2. R. Muscheler
3. M. Vonmoos
4. R. Holme
5. J. Beer
6. Monika Korte
7. N. Suttie
8. M. Hill

In Paleontology

1. Hans Renssen
2. Hugues Goosse
3. I. Usoskin

Citations in the corpus

• Radiocarbon simulations for the glacial ocean: The effects of wind stress, Southern Ocean sea ice and Heinrich events (2005, background): “02 atoms cm 2 s 1 [42]) and for the LGM (about 30% higher than the present (14)C production [43]).”
• Reconstructing Holocene geomagnetic field variation: new methods, models and implications (2014, methodology): “To estimate variations in the dipole moment we used 10Be flux data from the GRIP ice core (Muscheler et al. 2004; Vonmoos et al. 2006), which were first low-pass filtered with a cut-off frequency of 1/3000 yr−1 to remove solar activity induced production variations (Muscheler et al. 2005).”
• Large variations in Holocene solar activity: Constraints from 10Be in the Greenland Ice Core Project ice core (2006, methodology): “Greenland Ice Core Project (GRIP) ice core (Summit, Central Greenland) covering several hundred thousand years [Baumgartner et al., 1997b; Muscheler et al., 2004; Wagner et al., 2001; Yiou et al., 1997].”
• Solar activity during the last 1000 yr inferred from radionuclide records (2007, methodology): “Panel a shows data from Camp Century (Beer et al., 1988), panel b from GRIP ( Muscheler et al., 2004b; Yiou et al., 1997), panel c from Milcent (Beer et al., 1991), panel d from Dye3 (Beer et al., 1990), panel e from Dome Concordia (Beer et al., 1991) and panel f from the South Pole (Raisbeck et al”
• Coupled climate model simulation of Holocene cooling events: oceanic feedback amplifies solar forcing (2006, background): “Especially on the decadal to centennial time scales, which are of interest in our analysis, the potential for carbon cycle induced changes in 14 C is not very large (e.g., Muscheler et al., 2004b).”
• Tree rings and ice cores reveal C-14 calibration uncertainties during the Younger Dryas (2008, unknown): “Long-term differences between 10 Be and 14 C records still remain unresolve”