小隔间
发表于 2025-3-23 13:12:11
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朴素
发表于 2025-3-23 15:27:07
Das Kuratorium Unteilbares Deutschlandts. These gases, when dissolved in water droplets, modify the chemistry of the droplet phase and, then during precipitation, can be transferred to the oceans. This process is in addition to the direct transfer of the trace gases from the air to the ocean, described in this volume by Broecker and Lis
EWER
发表于 2025-3-23 19:29:57
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BARK
发表于 2025-3-24 02:02:59
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PON
发表于 2025-3-24 03:51:27
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observatory
发表于 2025-3-24 08:14:41
Das Kuratorium Unteilbares Deutschlande two cycles of particulate matter are coupled by the physical, chemical, and biological processes that take place at the air-sea interface and in the surface waters of the ocean. This geochemical coupling is particularly strong for trace metals. Within a few years at most, atmospheric inputs of tra
exorbitant
发表于 2025-3-24 12:11:11
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archenemy
发表于 2025-3-24 18:23:16
Introductory Physical Oceanography,l, and this is in fact so, but important deviations occur. Both horizontal and vertical circulations have vital roles to play, as we shall see. The principal driving forces for the ocean are solar heating, the winds, and the attraction of the moon.
挑剔为人
发表于 2025-3-24 19:20:01
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Cirrhosis
发表于 2025-3-25 02:17:46
Gas Transfer: Experiments and Geochemical Implications,roecker and Peng, 1974 Liss and Slater, 1976; Slinn et al.,l978). Basically, any net gas flux (F) across the interface must be driven by a concentration difference (ΔC) between air and surface water; the magnitude and direction of the flux being proportional to the numerical value and sign of ΔC, i.e.,