NOMOGRAMS FOR CALCULATING TURBULENT HEAT EXCHANGE AND HEAT LOSS BY EVAPORATION

Calculation of turbulent heat exchange and heat loss by evaporation with empirical formulas is a rather long and work-consuming operation, requiring cumbersome computations, consisting of series of successive calculations. To facilitate such calculations it is expedient to use uncomplicated nomogram...

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Bibliographic Details
Main Author: Shamontev,V. A.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1970
Subjects:
Meteorology
Thermodynamics
(*MARINE METEOROLOGY
EVAPORATION)
(*THERMODYNAMIC CYCLES
SEA WATER)
COLD WEATHER TESTS
ARCTIC REGIONS
ANTARCTIC REGIONS
HEAT TRANSFER
ATMOSPHERIC MOTION
USSR
TRANSLATIONS
Arctic
Antarctic
Antarc*
Online Access:http://www.dtic.mil/docs/citations/AD0711916
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0711916
Description
Summary:Calculation of turbulent heat exchange and heat loss by evaporation with empirical formulas is a rather long and work-consuming operation, requiring cumbersome computations, consisting of series of successive calculations. To facilitate such calculations it is expedient to use uncomplicated nomograms, which enable us to obtain directly from them the values of heat currents resulting from turbulent heat exchange and evaporation. Such nomograms were used in calculating the heat balance components of one of the Arctic seas for the navigation period. Plotting of such nomograms, connected with the graphic solution of an equation with three unknowns, is based on the method of application of the system of Cartesian coordinates. (Author) Trans. of Problemy Arktiki i Antarktiki (USSR) n26 p39-44 1967.

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