By W.H. Berger, L.D. Labeyrie
` Authors of the papers are very recognized, such a lot exotic experts on the planet from many branches of average sciences. due to this, clinical point of papers, the quantity and personality of provided info is particularly efficient and entire. '
`... a important and particular addition in every one climatological library.'
M. Sadowski in PAGEOPH, Vol. one hundred thirty No. 1, 1989.
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Extra resources for Abrupt Climatic Change: Evidence and Implications
Hilankovitch and Climate, Part 2, D. Reidel, Dordrecht, p. 671686. , Esmay, A. , 1980. Evidence bearing on the mechanism of rapid deglaciation, Climatic Change, 3: 65-87. , Erlenkeuser, H. , 1982. Termination I: the response of continental climate in the subtropics as recorded in deep-sea sediments, Bulletin de l'Institut Geologique du Bassin d'Aquitaine, 31: 393-407. S. ) 1966. C. Royal Meteorological Society, London, 229pp. , 1976. The Genesis Strategy, Plenum Press, New York, 4l9pp. M. , 1987.
Greenland ice core: geophysics, geochemistry, and the environment, Amer. Geophys. Union Geophys. Monogr. 33, l18pp. M. E. ), 1980. Studies in the Lateglacial of North-West Europe. Pergamon Press, Oxford. C. M. (eds) 1986a. Projecting the climatic effects of increasing carbon dioxide. S. Dept. S. Govt. , 38lpp. C. M. (eds) 1986b. Detecting the climatic effects of increasing carbon dioxide. S. Dept. S. Govt. , 198pp. E. , 1974. Quaternary stratigraphy of Norden, a proposal for terminology and classification, Boreas, 3: 109-128.
Due to the long residence time of C02 in the atmosphere (about 4 years), the distribution of C02 over the globe is rather uniform (cf. , 1985, Fig. 20). H20, however, stays only 9 days in the atmosphere before raining out. In the tropics the speed of the vertically integrated transport vector is only of the order of 250km/d (estimated from Peixoto and Oort, 1983) with a component towards the Intertropical Convergence Zone, so that little additional water vapour in the tropics can escape into higher latitudes.