Younger dryas

Denton, G. H. and Hendy, C. H. (1994). Documentation of a Younger Dryas glacial advance in the New Zealand Alps. Science 264,1434-1437. 

Fairbanks, R. G. (1989). A 17,000-year glacio-eustatic sea level record influence of glacial melting rates on younger dryas event and deep-ocean circulation. Nature 342, 637-642. 

Fig. 18-10 (a) Accumulation rate history for Greenland (Alley et ai, 1993 Guffey and Clow, 1997), with insets focusing on the Younger Dryas cold interval and the very rapid termination of the last glaciation, with substantial change that occurred in only 3 years noted (after Alley et ai, 1993). (b) Accumulation-rate history, normalized to the modem rate, for Antarctica (Raisbeck et ah, 1987), derived from °Be analysis. 

Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice. Nature 391,141-146. 

Fig. 9.7 Isotope records of abrupt climate change at the Younger-Dryas Preboreal transition 11,600 years BP taken from Greenland ice core data. The 8lsO, 815N2, and 840Ar isotopic records are plotted from top to bottom (Reprinted from Grachev, A. M. and Severinghaus, J. P. Quat. Sci. Rev. 24, 513 (2005), copyright 2005, with permission from Elsevier)...

McElwain JC, Mayle FE, Beerling DJ (2002) Stomatal evidence for a decline in the atmospheric C02 concentration during the Younger Dryas stadial a comparison with Antarctic ice core records. J Quat Sci... 

Goldstein, B.,Joos, F., and Stocker, T. F. (2003). A modeling study of oceanic nitrous oxide during the Younger Dryas cold period. Geophys. Res. Lett. 30(2), doi 10.1029/2002GL016418. 

Figure 34.8 Plots of c5 Nbuik versus sediment age over the past 50,000 years for cores from the Mexican margin (Ganeshram et af, 1995), the Somali margin of the Arabian Sea (Ivanochko etal., 2005) and the South China Sea (Kienast, 2000). The Last Glacial Maximum (LGM) and Younger Dryas (YD) cold intervals are indicated hy the hlue shading. The offsets among the records...

Severinghaus J. P., Sowers T., Brook E. J., Alley R. B., and Bender M. L. (1998) Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice. Science 391, 141 -146. 

Fawcett P. J., Agustdottir A. M., Alley R. B., and Shuman C. A. (1997) The Younger Dryas termination and north Atlantic deepwater formation insight from climate model simulations and Greenland ice core data. Paleocanography 12, 23-38. 

Firestone J. (1995) Resolving the Younger Dryas event through borehole thermometry. J. Glacial. 41, 39-50. 

Bard E., Arnold M., Mangerud J., Pateme M., Labeyrie L., Duprat J., Melieres M.-A., Spnstegaard E., and Duplessy J.-C. (1994) The North Atlantic atmosphere-sea surface gradient during the Younger Dryas chmatic event. Earth Planet. Set Lett. 126, 275—287. 

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