LVAD360
发表于 2025-3-25 04:42:47
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Paleontology
发表于 2025-3-25 09:05:38
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改变立场
发表于 2025-3-25 14:04:32
Longitudinal Dispersion of Salt in the Volkerak Estuarydal regime and freshwater discharge for the estuary are controlled by respectively a storm surge barrier and discharge sluices. In the different experiments freshwater discharges are 25 m./s, 50 m./s and 100 m./s and the tidal ranges at the mouth are 2.70 m and 3.50 m. In the seaward part of the est
Contort
发表于 2025-3-25 19:48:33
Mixing and Trapping in Australian Tropical Coastal Watershe coastal boundary layer inhibits mixing between the nearshore and offshore water by two effects, firstly by trapping in mangrove swamps, and secondly due to frictional effects which inhibit inertial jets. Contrast was found between coastal boundary layer dynamics in the Gulf of Carpentaria, which
搜集
发表于 2025-3-25 20:41:02
Control of Estuarine Salinities by Coastal Ocean Salinityuarine salinities against Mississippi River discharge and cross-spectrum analysis do not produce a successful hindcast of the observations. Parsimonious auto-regressive, moving-average predictive models of the weekly-averaged salinity data are quite skillful in hindcasting the measurements. These mo
祖先
发表于 2025-3-26 02:05:12
Mixing Processes in a Numerical Model of the Western Dutch Wadden Seaian displacement of watermasses appears to be very sensitive to the time of release, the initial position and the initial volume of the watermass considered. The advective component of this displacement agrees with the Eulerian residual currents on relatively large scales. In a Lagrangian sense the
难理解
发表于 2025-3-26 05:45:57
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BOAST
发表于 2025-3-26 08:28:40
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Dorsal
发表于 2025-3-26 14:29:17
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支架
发表于 2025-3-26 20:40:16
Residual Currents and Long-term Transport978-1-4613-9061-9Series ISSN 0724-5890