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The Transmission and Decay of Barotropic Topographic Rossby Waves Incident on a Continental Shelf
Barotropic Topographic Rossby Waves Continental Shelf
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2009/3/7
We know that long-period (>1 day) and long-wavelength (>100 km) topographical Rossby waves can be generated by a wind acting directly on a continental shelf (Adams and Buchwald, 1969). Here we examine...
Spectra of Reciprocal Transmission：Generalization to Saturated Regions
Reciprocal Transmission Saturated Regions
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2009/2/9
The results of Munk et al. (1981), relating spectra of ocean sound-speed and water-particle velocity to observable acoustic spectra are applicable only in the geometrical optics region. It is shown th...
Energy Transmission by Barotropic Rossby Waves across Large-Scale Topography
Energy Transmission Large-Scale Topography Barotropic Rossby Waves
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2009/1/19
An analytical study investigates the energy transmission by free, barotropic, linear Rossby waves across a large scale bottom topography when topographic and beta-effects have the same order of magnit...
Australia-Bermuda Sound Transmission Experiment（1960）Revisited
Australia-Bermuda Sound Transmission Experiment Bermuda hydrophones
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2009/1/6
Detonations at the depth of the sound channel axis off Perth, Australia were recorded on Bermuda hydrophones at a 178°.2 range (180° is antipodal). The analysis by Shockley et al. of this 1960 transmi...
Transmission of a Two-Layer Coastal Kelvin Wave over a Ridge
Two-Layer Coastal Kelvin Wave topographic ridge
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2009/1/4
We consider the problem of a low-frequency, two-layer, coastal Kelvin wave which impinges on a topographic ridge or valley at some angle to the coastline, with the aim of bounding the transmission of ...
Topographic Filtering and Reflectionless Transmission of Long Waves
Topographic Filtering Reflectionless Transmission Long Waves
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2008/11/11
The equation governing the passage of linear monochromatic, long waves over variable topography can be transformed into a Schrödinger equation. There are several transformations accomplishing thi...
The Transmission and Transformation of Baroclinic Rossby Waves by Topography
Transmission Transformation Baroclinic Rossby Waves Topography
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2008/7/4
The transmission of westward propagating baroclinic Rossby waves incident on a gappy meridional barrier is studied in the context of the two-layer, quasigeostrophic model. The meridional barrier model...
Ocean Radiant Heating. Part II: Parameterizing Solar Radiation Transmission through the Upper Ocean
Ocean Radiant Heating Parameterizing Solar Radiation Transmission Upper Ocean
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2008/7/2
Accurate determination of sea surface temperature (SST) is critical to the success of coupled ocean–atmosphere models and the understanding of global climate. To accurately predict SST, both the quant...
The Transmission of Rossby Waves through Basin Barriers
Rossby Waves Basin Barriers
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2008/6/30
The response of a basin with a topographic barrier to spatially localized and time periodic forcing is considered. The barrier, which almost completely divides the full basin into two adjacent subbasi...
Transmission of oxygen concentration fluctuations through the diffusive boundary layer overlying aquatic sediments
oxygen concentration fluctuations diffusive boundary layer aquatic sediments
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2014/5/14
Even though the O2 concentration in the diffusive boundary layer overlying natural aquatic sediments usually varies over time, microprofiles with little or no error bars are abundant in the literature...
Colored dissolved organic matter and dissolved organic carbon exclusion from lake ice: Implications for irradiance transmission and carbon cycling
Colored dissolved organic matter dissolved organic carbon exclusion lake ice irradiance transmission carbon cycling
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2014/5/26
Thick ice cover is a feature of cold-temperate, polar, and alpine lakes and rivers throughout much of the year. Our observations from Canadian lakes and rivers across the latitudinal gradient 46-80°N ...