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The upward and downward flux at various levels in the atmosphere and ocean is calculated by a Monte Carlo method which includes all orders of multiple scattering. A realistic model of the atmosphere-o...
The degree and direction of polarization, the ellipticity, and the radiance of the radiation at various levels in the atmosphere and ocean are calculated by a Monte Carlo method which includes all ord...
Observations of the motions of drifter clusters were made in the western Caribbean Sea during the summer of 1971. By two independent analyses of the relative motions of a cluster, two time series of h...
Periods and structures of several normal modes of Lake Michigan (including Green Bay) are calculated theoretically, taking into account the Lake's topography and the earth's rotation. The calculations...
Conservation expressions for a fluid property i* (e.g., salt, heat) and mass are derived for a semi-enclosed, stratified region as functions of a concentration j (e.g., salinity, temperature) and time...
model eddy is represented by an isolated three-dimensional patch characterized by anomalous potential vorticity, and its evolution is governed by stratified, f-plane quasigeostrophic dynamics. Guided ...
The scattering of internal gravity waves at finite topography is studied theoretically and numerically for a two-dimensional finite-depth ocean. In Part I a single incident plane wave was considered. ...
We developed an absorption-based primary production model that includes the effects of phytoplankton community size structure for the continental margin and adjoining Gulf Stream waters of the Middle ...

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