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An interpolation method of randomly distributed atmospheric data in the height-time domain

✍ Scribed by F. Trombetti; F. Tampieri


Publisher
Springer
Year
1983
Tongue
English
Weight
720 KB
Volume
25
Category
Article
ISSN
0006-8314

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✦ Synopsis


A numerical method for objective interpolation of boundary-layer data in the height-time domain is presented. The method is based on a diffusive transport hypothesis and allows for the determination of the optima1 ratio between the height and time scales to be used for non-dimensionalising the independent variables z and t. This ratio, with dimensions of a velocity, may be related to the vertical transfer properties of the atmosphere. A few cases during springtime with different stability conditions are discussed, showing that this ratio varies by at least one order of magnitude between day and night.


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