Malleable
发表于 2025-3-25 04:05:12
Triebfahrzeuge für Dreiphasenwechselstrom The radiant energy emitted by the sun may vary somewhat over very long periods, but a sensible idealization for most meteorological and oceanographic purposes consists in considering the solar source strength as fixed. Temporal variations in the incident radiation (and its spatial distribution) are
蒸发
发表于 2025-3-25 10:48:18
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我要沮丧
发表于 2025-3-25 12:35:16
Der Bau der Stromrichter und Hilfsapparate,ical motion and strongly affects the nature of the dynamics. It is also clear from the discussion in Section 2.9 that the vertical structure of the winds and currents is directly related to the presence and strength of horizontal density gradients by the thermal wind relation.
Hay-Fever
发表于 2025-3-25 18:40:40
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Baffle
发表于 2025-3-25 22:00:03
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友好
发表于 2025-3-26 00:33:17
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phlegm
发表于 2025-3-26 04:21:43
of the theory of the dynamics of large-scale motions of the oceans and atmosphere. Revised and updated, it includes expanded discussions of * the fundamentals of geostrophic turbulence * the theory of wave-mean flow interaction * thermocline theory * finite amplitude barocline instability.978-0-387-
Arteriography
发表于 2025-3-26 08:49:10
,Linienführung und Gleisanlage,eral pattern of the oceanic circulation began to emerge. It is clear now that a time-averaged circulation pattern exists in all oceans, although its observations may be significantly distorted by the presence of energetic fluctuations.
antenna
发表于 2025-3-26 15:08:06
Homogeneous Models of the Wind-Driven Oceanic Circulation,eral pattern of the oceanic circulation began to emerge. It is clear now that a time-averaged circulation pattern exists in all oceans, although its observations may be significantly distorted by the presence of energetic fluctuations.
sorbitol
发表于 2025-3-26 17:29:19
Textbook 19872nd editionory of the dynamics of large-scale motions of the oceans and atmosphere. Revised and updated, it includes expanded discussions of * the fundamentals of geostrophic turbulence * the theory of wave-mean flow interaction * thermocline theory * finite amplitude barocline instability.