標(biāo)題: Titlebook: Geophysical Approach to Marine Coastal Ecology; The Case of Iriomote Shinya Shimokawa,Tomokazu Murakami,Hiroyoshi Kohno Book 2020 Springer [打印本頁] 作者: 充裕 時(shí)間: 2025-3-21 18:41
書目名稱Geophysical Approach to Marine Coastal Ecology影響因子(影響力)
書目名稱Geophysical Approach to Marine Coastal Ecology影響因子(影響力)學(xué)科排名
書目名稱Geophysical Approach to Marine Coastal Ecology網(wǎng)絡(luò)公開度
書目名稱Geophysical Approach to Marine Coastal Ecology網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geophysical Approach to Marine Coastal Ecology被引頻次
書目名稱Geophysical Approach to Marine Coastal Ecology被引頻次學(xué)科排名
書目名稱Geophysical Approach to Marine Coastal Ecology年度引用
書目名稱Geophysical Approach to Marine Coastal Ecology年度引用學(xué)科排名
書目名稱Geophysical Approach to Marine Coastal Ecology讀者反饋
書目名稱Geophysical Approach to Marine Coastal Ecology讀者反饋學(xué)科排名
作者: 不容置疑 時(shí)間: 2025-3-21 21:48 作者: BLAZE 時(shí)間: 2025-3-22 03:31
Dynamical Properties of Coastal Currents in the Northwestern Part of Iriomote Island Part. 2—Funaukiconnecting channel, the seawater exchange among the bays becomes inactive. In the case of the moderate aspect ratio of the connecting channel, which is comparable with those of both bays, the seawater exchange among the bays reaches a maximum. For a larger aspect ratio (deeper or shorter) of the con作者: 未成熟 時(shí)間: 2025-3-22 04:52 作者: 牛馬之尿 時(shí)間: 2025-3-22 11:13
Transport Properties of Soil Particles in Sakiyama and Amitori Bayst and the topography are also important for them. The results are useful for assessing soil particle effects on coastal oceanic ecosystems, such as those containing reef-building coral and ., and their effective conservation in natural conservation areas of the Sakiyama and Amitori bays.作者: BIDE 時(shí)間: 2025-3-22 14:13 作者: BIDE 時(shí)間: 2025-3-22 17:40 作者: moratorium 時(shí)間: 2025-3-22 23:21 作者: countenance 時(shí)間: 2025-3-23 04:05 作者: 試驗(yàn) 時(shí)間: 2025-3-23 06:32 作者: 不再流行 時(shí)間: 2025-3-23 10:57 作者: Badger 時(shí)間: 2025-3-23 13:57
Der Betrieb elektrischer Maschinen,l coverage. Averages of the diversity index of the coral types at the mouth and inner parts of the bay are lower than the average of the whole region, but the average of diversity index at the intermediate part of the bay with the intermediate physical disturbances is higher than the average, which 作者: Incompetent 時(shí)間: 2025-3-23 20:18
https://doi.org/10.1007/978-3-662-25880-4 the mouth of Amitori Bay is about 2?km across and the length of the bay is 4?km. These suggested that the acroporid community in Amitori Bay could be maintained by recruits from within the bay and from immediately surrounding areas.作者: 供過于求 時(shí)間: 2025-3-23 23:18 作者: Presbycusis 時(shí)間: 2025-3-24 03:59
Numerical Analysis of Initial Dynamic State of Bundle of , spawning in Amitori Bay作者: Infelicity 時(shí)間: 2025-3-24 08:32
Numerical Analysis of Dispersals of , Seeds and Fruits in the Northwest Sea Area of Iriomote Island作者: 沒有貧窮 時(shí)間: 2025-3-24 12:00
https://doi.org/10.1007/978-981-15-1129-5Physical environment; Marine coastal ecosystem; Iriomote Island of Japan; Nature conservation area; Cora作者: Creditee 時(shí)間: 2025-3-24 18:46 作者: Frequency-Range 時(shí)間: 2025-3-24 22:50
Anatomische und physiologische Grundlagen,and: the geographical characteristics, Sakiyamawan–Amitoriwan Nature Conservation Area, and the meteorology, respectively. Sections?.–. describe biological aspects of Iriomote Island: Corals, Tropical sea grass ., ., respectively.作者: chuckle 時(shí)間: 2025-3-25 02:50
Magnetisch verkettete Stromkreisea 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.作者: 人工制品 時(shí)間: 2025-3-25 03:23
Iriomote Island, Japanand: the geographical characteristics, Sakiyamawan–Amitoriwan Nature Conservation Area, and the meteorology, respectively. Sections?.–. describe biological aspects of Iriomote Island: Corals, Tropical sea grass ., ., respectively.作者: Insul島 時(shí)間: 2025-3-25 10:51 作者: 歹徒 時(shí)間: 2025-3-25 11:51 作者: 歪曲道理 時(shí)間: 2025-3-25 18:20
Observational MethodObservations introduced into this book include current and wave observations mainly using WavesADCP, meteorological observation using an anemometer, and water quality observation using a portable multi-item water quality meter. This chapter presents a description of these observational methods.作者: CHOKE 時(shí)間: 2025-3-25 21:25 作者: GLADE 時(shí)間: 2025-3-26 01:08 作者: Watemelon 時(shí)間: 2025-3-26 06:23 作者: 放肆的我 時(shí)間: 2025-3-26 10:09
https://doi.org/10.1007/978-3-7091-5725-1bservational and numerical frameworks. Shirahama Bay with shallower water and Funauki Bay with deeper water in the northwestern part of Iriomote Island?are mutually connected by a channel. Tidal flows in both bays are expected to be much more complex than those of Sakiyama and Amitori bays, discusse作者: heart-murmur 時(shí)間: 2025-3-26 16:09
,F?rderung des elektrischen Schwei?ens,t techniques employing sediment traps using a polyvinyl chloride pipe to capture suspended sediment and a handheld analyzer for X-ray fluorescent analysis and a digital scanner for image analysis were employed for sediment measurement and analysis. In laboratory experiments, the sediment catch perfo作者: Judicious 時(shí)間: 2025-3-26 16:57 作者: 大火 時(shí)間: 2025-3-26 22:45
,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作者: 監(jiān)禁 時(shí)間: 2025-3-27 02:41
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作者: infringe 時(shí)間: 2025-3-27 06:18 作者: OFF 時(shí)間: 2025-3-27 12:15
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作者: GLOOM 時(shí)間: 2025-3-27 16:54 作者: 蓋他為秘密 時(shí)間: 2025-3-27 18:39
978-981-15-1131-8Springer Nature Singapore Pte Ltd. 2020作者: macabre 時(shí)間: 2025-3-27 23:00 作者: 媒介 時(shí)間: 2025-3-28 04:53 作者: OPINE 時(shí)間: 2025-3-28 06:15
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.作者: CYT 時(shí)間: 2025-3-28 11:21
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作者: 銼屑 時(shí)間: 2025-3-28 18:22
Dynamical Properties of Coastal Currents in the Northwestern Part of Iriomote Island Part. 2—Funaukibservational and numerical frameworks. Shirahama Bay with shallower water and Funauki Bay with deeper water in the northwestern part of Iriomote Island?are mutually connected by a channel. Tidal flows in both bays are expected to be much more complex than those of Sakiyama and Amitori bays, discusse作者: BARB 時(shí)間: 2025-3-28 22:13
Sediment Monitoring in Sakiyama and Amitori Bayst techniques employing sediment traps using a polyvinyl chloride pipe to capture suspended sediment and a handheld analyzer for X-ray fluorescent analysis and a digital scanner for image analysis were employed for sediment measurement and analysis. In laboratory experiments, the sediment catch perfo作者: BURSA 時(shí)間: 2025-3-29 00:34 作者: Assault 時(shí)間: 2025-3-29 05:17
Underwater Three-Dimensional Measurementsy 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作者: 策略 時(shí)間: 2025-3-29 11:04
Coral Distributions and Physical Environments in Amitori Bay 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作者: 真實(shí)的人 時(shí)間: 2025-3-29 15:24
Coral Distributions and Physical Environments in Sakiyama Baye distributions of coral coverage by the colony shapes and coral areas by the community types were investigated at 72 points around the bay. Next, physical variables such as oceanic flow and soil particle numbers were analyzed by numerical simulation under average summer and winter conditions in the作者: MAG 時(shí)間: 2025-3-29 16:54
Estimation Technique for Horizontal Distribution of Coral 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作者: HOWL 時(shí)間: 2025-3-29 19:48 作者: mendacity 時(shí)間: 2025-3-30 01:07
Der Betrieb elektrischer Maschinen,ect relation with bottom flows in the region; the bottom flows differ among coral community types. (2) Coral coverage shows an inverse relation with soil particle numbers in the region. . mainly inhabits areas with greater numbers of soil particles.作者: wall-stress 時(shí)間: 2025-3-30 08:07 作者: 我還要背著他 時(shí)間: 2025-3-30 09:49 作者: 尊敬 時(shí)間: 2025-3-30 14:33
