A simple two-layer model and its extension / Liao Tung-Hsien.
A two-layer model applicable both to graphical integration and numerical computation is proposed. Using this model, the height of the 500-mb surface and the thickness between this and some chosen isobaric surface in the vicinity of the top of the friction layer can be derived. An extended model invo...
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| Format: | Government Document Book |
| Language: | English |
| Published: |
L.G. Hanscom Field, Bedford, Massachusetts :
Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force,
1968.
|
| Series: | AFCRL ;
68-276. Translations (Air Force Cambridge Research Laboratories (U.S.)) ; no. 4. |
| Subjects: |
MARC
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| 100 | 1 | |a Liao, Tung-Hsien, |e author. | |
| 245 | 1 | 2 | |a A simple two-layer model and its extension / |c Liao Tung-Hsien. |
| 264 | 1 | |a L.G. Hanscom Field, Bedford, Massachusetts : |b Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, |c 1968. | |
| 300 | |a v, 22 pages : |b illustrations ; |c 28 cm. | ||
| 336 | |a text |b txt |2 rdacontent. | ||
| 337 | |a unmediated |b n |2 rdamedia. | ||
| 338 | |a volume |b nc |2 rdacarrier. | ||
| 490 | 1 | |a AFCRL ; |v 68-0276. | |
| 490 | 1 | |a Translation ; |v No. 4. | |
| 500 | |a "May 1968." | ||
| 500 | |a AD0675137 (from http://www.dtic.mil) | ||
| 500 | |a AFCRL Research Library Project 8604. | ||
| 500 | |a Translation supported by the Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, L.G. Hanscom Field, Bedford, Massachusetts. | ||
| 500 | |a Translated from Acta Meteorologica Sinica, volume 29, number 3, pp. 162-175, August 1958. | ||
| 500 | |a Translated by the Oriental Science Research Library of Emmanuel College, Boston, Mass. under Contract AF19(628)-5073. | ||
| 504 | |a Includes bibliographical references (pages 21-22) | ||
| 520 | |a A two-layer model applicable both to graphical integration and numerical computation is proposed. Using this model, the height of the 500-mb surface and the thickness between this and some chosen isobaric surface in the vicinity of the top of the friction layer can be derived. An extended model involving three layers is also designed. Unlike Sawyer and others, in designing these models, the distribution of the vertical velocity with height is not prescribed. Finally, the steadiness of the space mean velocity field and the selection of lateral boundary conditions are discussed. | ||
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