A statistical model of atmospheric temperature signals.

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Authors
Kline, Edward Marvin
Subjects
thermal plume
skewness
coefficient of excess
atmospheric temperature signals
model temperature signals
micro-thermals
turbulence
Advisors
Boston, Noël
Date of Issue
1972-03
Date
March 1972
Publisher
Monterey, California. Naval Postgraduate School
Language
en_US
Abstract
The "ramp" is an often observed feature in temperature fluctuations during unstable atmospheric conditions. It is characterized by a gradual increase in temperature followed by a sudden drop to an ambient level. This ramp clearly distinguishes temperature signals from other turbulence signals such as velocity. Three different ramp-type atmospheric temperature fluctuations and their derivatives are constructed and statistically examined for the parameters skewness and coefficient of excess., These statistical values are compared with values obtained from actual signals. The "complex ramp signal" was found to represent these quite well. Skewness and coefficient of excess for this signal could be altered almost independently of each other. The complex ramp is constructed by inscribing nearly symmetrical consecutive triangles within two envelope rays of constant but different slopes such that the two envelope rays approximate a ramp function.
Type
Thesis
Description
Series/Report No
Department
Oceanography
Organization
Naval Postgraduate School (U.S.)
Identifiers
NPS Report Number
Sponsors
Funder
Format
Citation
Distribution Statement
Approved for public release; distribution is unlimited.
Rights
This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
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