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Titlebook: Geophysical Approach to Marine Coastal Ecology; The Case of Iriomote Shinya Shimokawa,Tomokazu Murakami,Hiroyoshi Kohno Book 2020 Springer

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31#
發(fā)表于 2025-3-26 22:45:59 | 只看該作者
,Die Widerstandsschwei?verfahren,y structure from motion (SfM). The possibility of underwater SfM using a small submarine (small remotely operated vehicle, sROV) was also investigated. After we conducted underwater SfM and conventional measurements simultaneously for dendritic coral, massive coral, and seaweed . in a coral reef are
32#
發(fā)表于 2025-3-27 02:41:19 | 只看該作者
Der Betrieb elektrischer Maschinen, conducted to obtain data for the coral distribution, sea temperature, sea salinity, wind speed, and river flow rate. Then, the observed data were used in ocean and wave model numerical simulations and soil particle tracking analyses to ascertain the spatial and temporal distributions of wave height
33#
發(fā)表于 2025-3-27 06:18:06 | 只看該作者
34#
發(fā)表于 2025-3-27 12:15:29 | 只看該作者
Die Untersuchung elektrischer Maschinen, and current in spite of its small size. It also exhibits a diverse distribution of coral reefs in response. Physical data acquired through numerical analysis, although including errors from actual measurements, provide much information by being interpolated spatially and are useful for the understa
35#
發(fā)表于 2025-3-27 16:54:46 | 只看該作者
36#
發(fā)表于 2025-3-27 18:39:24 | 只看該作者
978-981-15-1131-8Springer Nature Singapore Pte Ltd. 2020
37#
發(fā)表于 2025-3-27 23:00:41 | 只看該作者
38#
發(fā)表于 2025-3-28 04:53:37 | 只看該作者
39#
發(fā)表于 2025-3-28 06:15:05 | 只看該作者
Numerical Simulation Methoda coordinate system (CCM) developed by the author and a colleague for computation of seawater flow, a wave model SWAN developed at Delft University of Technology, and the Lagrangian particle tracking model.
40#
發(fā)表于 2025-3-28 11:21:28 | 只看該作者
Dynamical Properties of Coastal Currents in the Northwestern Part of Iriomote Island Part. 1—Sakiyamussed in this chapter, based on the results of theoretical, observational, and numerical investigations. According to the tidal flow dynamics in a single channel, these bays in this region are categorized as “deep bays,” in which little difference in phase and amplitude of the tidal levels exists fr
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