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By J. P. Rozelot (auth.), A. Ghazi, R. Fantechi (eds.)

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Additional resources for Current Issues in Climate Research: Proceedings of the EC Climatology Programme Symposium, Sophia Antipolis, France, 2–5 October 1984

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The accuracy of this complex evolution has been lent considerable credence by a detailed sedimentological study and by analysis of a large number of levels corresponding to the climatic transition. Observations similar to those obtained at Les Echets can also be made from diagram X of La Grande Pile (16), fom those of Sulzberg Baden in the Bernese Oberland (17) and of Odderade in Schleswig Holstein {lS). Without doubting the very cold nature of the brief episode which ended the Eemian interglacial palynological observations indicate a complex process of climatic deterioration that was therefore also relatively long (covering a period of several centuries).

O ~. -r--'-I (Q ~ -!? 44° 53 1 N • 03° 18 1 W • 3298 m. ~ cD Q: z J: GLACIAL BOLLING ALLEROD Y. z Variations in the isotopic composition of foraminarera, of surface water temperatures and of pollens in the SUBl-47 core extracted in the Bay of Biscay. S ISO +3 ,, Figure 6 lli... 9.!!.. ~ _°_1 w o a. I- J: o E SU 8147 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18 19. , KUKLA, G , arrl SALTZMAN, B. (1984). Milankovitch arrl climate. D. Reidel Publishing Company. , DECPE,M. and PESTIEAUX, P.

Deep hole measurements The deep hole at Dye 3 was drilled by GISP in 1979-81 (6). 6 m long, and 130 mm in diameter. The hole is filled with a fluid to counteract the outside pressure. In 1983, three independent borehole surveys were made using different tools to measure the temperature profile along the hole (Fig. 6); the inclination, azimuth and diameter of the hole; and the pressure in the fluid (18) . - 51 - a DYE3 Temp. 00 Fig. 6. Temperature profile measured along the deep hole in 1983. The minimum at 200 m depth is a remain of the little ice age.

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