矿石 发表于 2025-3-26 21:49:07
Linear and two-dimensional geometry of whitecapping and foam structures,ctional coverage areas, depending on surface wind velocity, sea surface state, size of sea waves, season of observation, biological activity at the given World Ocean area, etc. Here, since the wave-breaking and subsequent whitecapping process depend on many factors of a physical, chemical, and bioloDawdle 发表于 2025-3-27 02:22:57
http://reply.papertrans.cn/20/1906/190507/190507_32.pnghazard 发表于 2025-3-27 08:46:22
http://reply.papertrans.cn/20/1906/190507/190507_33.png河流 发表于 2025-3-27 09:52:06
https://doi.org/10.1057/9780230250772 methods of studying such complicated media can be passive and active microwave remote systems (including radar systems with synthesized and real aperture and Doppler scatterometers) (Krasiuk and Rosenberg, 1970; Meischner, 1990; Sharkov, 1998, 2003; Bulatov et al., 2003; Mouche et al., 2006).Dawdle 发表于 2025-3-27 15:41:51
Electrodynamics of concentrated drop flows, methods of studying such complicated media can be passive and active microwave remote systems (including radar systems with synthesized and real aperture and Doppler scatterometers) (Krasiuk and Rosenberg, 1970; Meischner, 1990; Sharkov, 1998, 2003; Bulatov et al., 2003; Mouche et al., 2006).Enervate 发表于 2025-3-27 18:40:48
and remotely sensed reflectance and emissivity in visible, IR and microwave ranges of one of the most important elements of disturbed sea surface - sea waves breaking.978-3-642-06752-5978-3-540-29828-1解脱 发表于 2025-3-28 00:37:20
http://reply.papertrans.cn/20/1906/190507/190507_37.pngBIPED 发表于 2025-3-28 05:35:05
https://doi.org/10.1057/9780230250772o-scale radiophysical scattering model for signals with vertical polarization (in transmission-reception mode) (Moor and Fung, 1979; Alpers and Hasselmann, 1982), the results of many works indicate the urgency of organizing special experiments with the purpose of revealing the physical features of scattering signals with horizontal polarization.vasculitis 发表于 2025-3-28 08:55:29
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