Titlebook: Estuarine Circulation; Bruce J. Neilson,Albert Kuo,John Brubaker Book 1989 The Humana Press Inc. 1989 Coast.Ocean.geomorphology.marine.tra

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書目名稱Estuarine Circulation影響因子(影響力)




書目名稱Estuarine Circulation影響因子(影響力)學(xué)科排名




書目名稱Estuarine Circulation網(wǎng)絡(luò)公開度




書目名稱Estuarine Circulation網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Estuarine Circulation被引頻次




書目名稱Estuarine Circulation被引頻次學(xué)科排名




書目名稱Estuarine Circulation年度引用




書目名稱Estuarine Circulation年度引用學(xué)科排名




書目名稱Estuarine Circulation讀者反饋




書目名稱Estuarine Circulation讀者反饋學(xué)科排名

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Estuarine Flow Interaction with Topography Lateral and Longitudinal Effects,waves. Though secondary currents are fairly well understood in rivers, in estuaries there is a paucity of field information, and tidally-averaged secondary flow patterns proposed in 1977 still remain largely unverified. Lee waves, on the other hand, are produced when stratified water flows over bed

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Headland Eddies in a Tidal Estuary,mensional, horizontally-circulating eddies produced by both flood and ebb currents around the two headlands at the north and the south ends of the cove. Due to stronger ebb currents, eddies generated by the ebb currents were dominant and produced a persistent residual circulation covering the entire

褻瀆

Residual Currents in the Peconic Bays Estuary,mple spectral techniques. Results suggest that for periods shorter than approximately five days currents at all moorings respond to coastal sea level fluctuations which are presumably meteorologically forced. Analysis of current fluctuations at longer periods suggest that tidal rectification contrib

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The Response of Estuarine Circulation to Local Wind Events,e distinct response conditions of non-tidal circulation to wind were observed. These conditions exhibited significant temporal and spatial variability. The first was typified by a positive two layer flow response to wind that was significant in the middle section of the York during the first six day

lethal

lethal

On Inter-Tidal Transport Equation,estuaries. The characteristic time scales for most estuarine biological and chemical processes are on the order of several tidal cycles or longer. To address the long-term transport mechanism meaningfully, the formulation of an inter-tidal conservation equation is the main subject of this paper. The

凈禮

Excitation-Response Analysis of Estuarine Circulation,tions. The system excitations include deterministic tidal forcings, stochastic buoyancy forcings and stochastic local and nonlocal atmospheric forcings having time scales ranging from daily to seasonal. The estuarine system represented by the momentum, continuity and mass transport equations in a to

清洗

A Tale of Two Estuaries: Columbia Bay, Alaska, and San Francisco Bay, California,amics are dominated by subglacial freshwater flows; San Francisco Bay is a shallow estuary dominated by tides and to a lesser extent by freshwater inflow. These different forcing mechanisms in conjunction with the dissimilar geometries, lead to different circulation patterns. These two particular es

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