Skip to main content

Currently Skimming:

3: Lagrangian and Eulerian Data and Models
Pages 23-26

The Chapter Skim interface presents what we've algorithmically identified as the most significant single chunk of text within every page in the chapter.
Select key terms on the right to highlight them within pages of the chapter.


From page 23...
... An appropriate statistical description of ocean circulation includes two main parts. One is the statistics of the velocity field, and the other is the statistical description of the transport mechanisms.
From page 24...
... . In particular, comparing diffusivity maps and maps of mean flow or velocity variance provides a way to test simple theories of turbulence, and eventually indicates how to improve them.
From page 25...
... Stationarity can be relaxed fairly realistically provided the ocean is characterized by slowly varying fluctuations so that time averages, even though not constant, are representative of the particular ocean climate present during the measurements. Inhomogeneity could in principle be reduced inside each box by increasing the resolution, i.e., by decreasing L, the scale of the boxes.
From page 26...
... ; 2. Filtering and parameter estimation for random fields governed by randomly perturbed ordinary and partial differential equations, with emphasis on numerical methods for nonlinear fiItenug, spectral methods, and others; 3.


This material may be derived from roughly machine-read images, and so is provided only to facilitate research.
More information on Chapter Skim is available.