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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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樓主: 減輕
31#
發(fā)表于 2025-3-27 00:45:52 | 只看該作者
32#
發(fā)表于 2025-3-27 01:16:01 | 只看該作者
33#
發(fā)表于 2025-3-27 09:15:25 | 只看該作者
34#
發(fā)表于 2025-3-27 11:34:57 | 只看該作者
Holocene Climate Evolution of the North Atlantic Ocean and the Nordic Seas — a Synthesis of New Resu cooling trend there is also a higher frequency (albeit subtle) variability of multi-decadal and centennial time scales in the ocean. The magnitude of this variability is in the order of a few degrees. At the moment the underlying mechanisms for this variability remains as a topic of debate.
35#
發(fā)表于 2025-3-27 17:02:57 | 只看該作者
36#
發(fā)表于 2025-3-27 19:53:46 | 只看該作者
https://doi.org/10.1007/978-3-322-86067-5ng paleoceanographic evidence for ~1400–1500-y climate oscillations during the Holocene is questionable. Instead we suggest that deep-sea records from the North Atlantic may be reconciled with 900-y climate oscillations during this period.
37#
發(fā)表于 2025-3-28 00:10:01 | 只看該作者
Das Projekt Spallations-Neutronenquelle,. The original Brückner cycle of 35 years is here suggested to be of tidal origin (twice the lunar perigee period). Likewise, the 1470-y Greenland cycle is proposed to be tidal in nature (as a beat between nodal and perigee cycles, effective during the summer season).
38#
發(fā)表于 2025-3-28 03:54:57 | 只看該作者
Holocene Climate Variability on Centennial-to-Millennial Time Scales: 1. Climate Records from the Nong paleoceanographic evidence for ~1400–1500-y climate oscillations during the Holocene is questionable. Instead we suggest that deep-sea records from the North Atlantic may be reconciled with 900-y climate oscillations during this period.
39#
發(fā)表于 2025-3-28 09:03:52 | 只看該作者
40#
發(fā)表于 2025-3-28 13:08:24 | 只看該作者
oader audience.Includes interdisciplinary papers.RecommendatThe global environment is changing rapidly under the impact of human activities, and an important element of this change is related to global c1imate modification. Can the study of c1imate and history help in devising strategies for coping
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