Objective
发表于 2025-3-21 19:11:40
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orient
发表于 2025-3-21 21:51:36
Achim Hohorst,Michael Westermeier,Philipp P. Spangenbergs an active area of deep water formation not only during full interglacial conditions (isotopic stages 1 and 5e) but also during the early part of the glaciation (isotope stages 4 and 5a–5d)..As sinking of surface water to the depth is linked to its cooling during winter, the Norwegian Sea deep wate
adj忧郁的
发表于 2025-3-22 02:44:55
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Myelin
发表于 2025-3-22 06:58:48
Markus Fromm-Wittenbergccession of Pleistocene ice ages. Accurate values for the variations of these orbital element and related monthly insolations are now available for the last 2 to 3 million years. Even if recent climatic models, both qualitative and quantitative, show that the orbital parameters have modulated the cl
outset
发表于 2025-3-22 09:09:28
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Multiple
发表于 2025-3-22 16:11:13
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GULP
发表于 2025-3-22 19:01:25
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画布
发表于 2025-3-22 22:39:51
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压迫
发表于 2025-3-23 03:47:31
Mirko Twardys an active area of deep water formation not only during full interglacial conditions (isotopic stages 1 and 5e) but also during the early part of the glaciation (isotope stages 4 and 5a–5d)..As sinking of surface water to the depth is linked to its cooling during winter, the Norwegian Sea deep wate
的阐明
发表于 2025-3-23 05:39:44
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