Box 13
Container
Contains 51 Results:
(2 documents) 1. The integral invariants of two-dimensional inviscid flow and their role in the theory of two-dimensional turbulance. 2. A simple stastical treatment of highly turbulent couette flow, undated
File — Box: 13, Folder: 21
Identifier: - 06 PDT 4 Box 13 Folder 21
Dates:
undated
The integrals of motion of two-dimensional flows and the properties of four-mode representations, 1960s
File — Box: 13, Folder: 22
Identifier: - 06 PDT 4 Box 13 Folder 22
Dates:
1960s
On integration of the quasi-geostrophic w-equation, April, 1981
File — Box: 13, Folder: 23
Identifier: - 06 PDT 4 Box 13 Folder 23
Dates:
April, 1981
On the interface between two fluids in contact with a horizontal solid surface, undated
File — Box: 13, Folder: 24
Identifier: - 06 PDT 4 Box 13 Folder 24
Dates:
undated
Internal dynamical structure. Molecular viscosity not important, undated
File — Box: 13, Folder: 25
Identifier: - 06 PDT 4 Box 13 Folder 25
Dates:
undated
Intimations of irreversibility in two-dimensional nonviscous flow, 1969
File — Box: 13, Folder: 26
Identifier: - 06 PDT 4 Box 13 Folder 26
Dates:
1969
An introduction to numerical weather prediction, undated
File — Box: 13, Folder: 27
Identifier: - 06 PDT 4 Box 13 Folder 27
Dates:
undated
Technical Memorandum No. 5. Joint Numerical Weather Prediction Unit. An interative method for solving an elliptic equation with variable coefficients and its convergwence criterion, March 8, 1955
File — Box: 13, Folder: 28
Identifier: - 06 PDT 4 Box 13 Folder 28
Dates:
March 8, 1955
The kinetic energy spectrum of large- and meso-scale turbulent motions of the oceans and atmosphere, June 1975
File — Box: 13, Folder: 29
Identifier: - 06 PDT 4 Box 13 Folder 29
Dates:
June 1975
A langrangian scheme of short-range numerical weather prediction, undated
File — Box: 13, Folder: 30
Identifier: - 06 PDT 4 Box 13 Folder 30
Dates:
undated