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Multiradionuclide evidence for the solar origin of the cosmic-ray events of AD 774/5 and 993/4
Mekhaldi, F., Muscheler, R., Adolphi, F., Aldahan, A., Beer, J., McConnell, J. R., … Woodruff, T. E. (2015). Multiradionuclide evidence for the solar origin of the cosmic-ray events of AD 774/5 and 993/4. Nature Communications, 6, 8611 (8 pp.). https://doi.org/10.1038/ncomms9611
Persistent link between solar activity and Greenland climate during the Last Glacial Maximum
Adolphi, F., Muscheler, R., Svensson, A., Aldahan, A., Possnert, G., Beer, J., … Thiéblemont, R. (2014). Persistent link between solar activity and Greenland climate during the Last Glacial Maximum. Nature Geoscience, 7(9), 662-666. https://doi.org/10.1038/ngeo2225
Climate forcing reconstructions for use in PMIP simulations of the Last Millennium (v1.1)
Schmidt, G. A., Jungclaus, J. H., Ammann, C. M., Bard, E., Braconnot, P., Crowley, T. J., … Vieira, L. E. A. (2012). Climate forcing reconstructions for use in PMIP simulations of the Last Millennium (v1.1). Geoscientific Model Development, 5(1), 185-191. https://doi.org/10.5194/gmd-5-185-2012
Climate forcing reconstructions for use in PMIP simulations of the last millennium (v1.0)
Schmidt, G. A., Jungclaus, J. H., Ammann, C. M., Bard, E., Braconnot, P., Crowley, T. J., … Vieira, L. E. A. (2011). Climate forcing reconstructions for use in PMIP simulations of the last millennium (v1.0). Geoscientific Model Development, 4(1), 33-45. https://doi.org/10.5194/gmd-4-33-2011
Variable <SUP>10</SUP>Be fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record?
Ljung, K., Björck, S., Muscheler, R., Beer, J., & Kubik, P. W. (2007). Variable 10Be fluxes in lacustrine sediments from Tristan da Cunha, South Atlantic: a solar record? Quaternary Science Reviews, 26(7-8), 829-835. https://doi.org/10.1016/j.quascirev.2006.12.016
Reply to the comment by Bard et al. on "Solar activity during the last 1000 yr inferred from radionuclide records"
Muscheler, R., Snowball, I., Joos, F., Müller, S. A., Beer, J., & Vonmoos, M. (2007). Reply to the comment by Bard et al. on "Solar activity during the last 1000 yr inferred from radionuclide records". Quaternary Science Reviews, 26(17-18), 2304-2308. https://doi.org/10.1016/j.quascirev.2007.06.014
Solar activity during the last 1000 yr inferred from radionuclide records
Muscheler, R., Joos, F., Beer, J., Müller, S. A., Vonmoos, M., & Snowball, I. (2007). Solar activity during the last 1000 yr inferred from radionuclide records. Quaternary Science Reviews, 26(1-2), 82-97. https://doi.org/10.1016/j.quascirev.2006.07.012
Ancient biomolecules from deep ice cores reveal a forested Southern Greenland
Willerslev, E., Cappellini, E., Boomsma, W., Nielsen, R., Hebsgaard, M. B., Brand, T. B., … Collins, M. J. (2007). Ancient biomolecules from deep ice cores reveal a forested Southern Greenland. Science, 317(5834), 111-114. https://doi.org/10.1126/science.1141758
Solar variability over the past several millennia
Beer, J., Vonmoos, M., & Muscheler, R. (2006). Solar variability over the past several millennia. Space Science Reviews, 125(1-4), 67-79. https://doi.org/10.1007/s11214-006-9047-4
Solar forced Dansgaard/Oeschger events?
Muscheler, R., & Beer, J. (2006). Solar forced Dansgaard/Oeschger events? Geophysical Research Letters, 33(20), 1-4. https://doi.org/10.1029/2006GL026779
Large variations in Holocene solar activity: constraints from <SUP>10</SUP>Be in the Greenland Ice Core Project ice core
Vonmoos, M., Beer, J., & Muscheler, R. (2006). Large variations in Holocene solar activity: constraints from 10Be in the Greenland Ice Core Project ice core. Journal of Geophysical Research A: Space Physics, 111(A10), 1-14. https://doi.org/10.1029/2005JA011500
&lt;sup&gt;10&lt;/sup&gt;Be concentration in the ice shelf of Queen Maud Land, Antarctica
Moraal, H., Muscheler, R., du Plessis, L., Kubik, P. W., Beer, J., McCracken, K. G., & McDonald, F. B. (2005). 10Be concentration in the ice shelf of Queen Maud Land, Antarctica. South African Journal of Science, 101(5-6), 299-301.
Geomagnetic field intensity during the last 60,000 years based on <SUP>10</SUP>Be and <SUP>36</SUP>Cl from the Summit ice cores and <SUP>14</SUP>C
Muscheler, R., Beer, J., Kubik, P. W., & Synal, H. A. (2005). Geomagnetic field intensity during the last 60,000 years based on 10Be and 36Cl from the Summit ice cores and 14C. Quaternary Science Reviews, 24(16-17), 1849-1860. https://doi.org/10.1016/j.quascirev.2005.01.012
Why did a cold period follow on the heels of the last Ice Age?
Muscheler, R. (2005). Why did a cold period follow on the heels of the last Ice Age? Eawag News [engl. ed.], 58, 11-13.
Bomb-test <SUP>36</SUP>Cl measurements in Vostok snow (Antarctica) and the use of <SUP>36</SUP>Cl as a dating tool for deep ice cores
Delmas, R. J., Beer, J., Synal, H. A., Muscheler, R., Petit, J. R., & Pourchet, M. (2004). Bomb-test 36Cl measurements in Vostok snow (Antarctica) and the use of 36Cl as a dating tool for deep ice cores. Tellus, Series B: Chemical and Physical Meteorology, 56B(5), 492-498. https://doi.org/10.3402/tellusb.v56i5.16454
Causes and timing of the 8200yr BP event inferred from the comparison of the GRIP <SUP>10</SUP>Be and the tree ring Δ<SUP>14</SUP>C record
Muscheler, R., Beer, J., & Vonmoos, M. (2004). Causes and timing of the 8200yr BP event inferred from the comparison of the GRIP 10Be and the tree ring Δ14C record. Quaternary Science Reviews, 23(20-22), 2101-2111. https://doi.org/10.1016/j.quascirev.2004.08.007
Changes in the carbon cycle during the last deglaciation as indicated by the comparison of <SUP>10</SUP>Be and <SUP>14</SUP>C records
Muscheler, R., Beer, J., Wagner, G., Laj, C., Kissel, C., Raisbeck, G. M., … Kubik, P. W. (2004). Changes in the carbon cycle during the last deglaciation as indicated by the comparison of 10Be and 14C records. Earth and Planetary Sciences Letters, 219, 325-340. https://doi.org/10.1016/S0012-821X(03)00722-2
Pourquoi un soudain retour du froid à la fin de la dernière période glaciaire?
Muscheler, R. (2004). Pourquoi un soudain retour du froid à la fin de la dernière période glaciaire? Eawag News [éd. fr.], 58, 11-13.
Wieso kam es am Ende der letzten Eiszeit zu einem erneuten Kälteeinbruch?
Muscheler, R. (2004). Wieso kam es am Ende der letzten Eiszeit zu einem erneuten Kälteeinbruch? Eawag News [dtsch. Ausg.], 58, 11-13.
Co-precipitated silver-metal oxide aggregates for accelerator mass spectrometry of <SUP>10</SUP>Be and <SUP>26</SUP>Al
Stone, J., Fifield, K., Beer, J., Vonmoos, M., Obrist, C., Grajcar, M., … Caffee, M. (2004). Co-precipitated silver-metal oxide aggregates for accelerator mass spectrometry of 10Be and 26Al. Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and Atoms, 223-224, 272-277. https://doi.org/10.1016/j.nimb.2004.04.055