Titlebook: Climate Development and History of the North Atlantic Realm; Gerold Wefer,Wolfgang H. Berger,Eystein Jansen Book 2002 Springer-Verlag Berl

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https://doi.org/10.1007/978-3-322-86067-5l-to-millennial time scales in this realm may well be caused by fluctuations in the associated heat transport. The sensitivity of the meridional circulation is determined by a number of feedbacks in the climate system, which can also interact to sustain internal oscillations. Another source of clima

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Alfred Fettweis,Martin Weber,Eckart Knellereters. Reliable specification of the true extent of Sun-climate connections requires continuous solar monitoring with sufficiently high stability to specify long-term solar irradiance variability and to characterize spectral irradiance variability at all wavelengths. A suite of cavity-type electrica

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Alfred Fettweis,Martin Weber,Eckart Knellereriods of high sunspot activity, results in increased strength of winds in the North Atlantic. Changes in wind strength and mixing in the North Atlantic should affect coral growth on Bermuda. We test this proposition with an 800-year record of . from this island, comparing the cycles found within th

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Das Projekt Spallations-Neutronenquelle, climate state as well as future climate variability about the mean, resulting from the interference between natural climate variability and anthropogenic perturbations of the climate system. Natural climate variability originates from interactions between components of the climate systems and from

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https://doi.org/10.1007/978-3-322-85650-0rn Hemisphere insolation during the Holocene. This is manifested by the early Holocene optimum temperatures and the general cooling trend of the surface ocean since then. However, the duration of this optimum decreased both towards the north and towards the margins of the Nordic Seas suggesting that

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capsaicin

Zusammenbruch und Wiederaufstieg, lake records from Europe show that there are regionally-coherent patterns of change in lake status (a qualitative index of changes in water depth, area or volume) through the Holocene, reflecting climatically-induced changes in regional water budgets. Rapid changes in lake status occur in many regi

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