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contributor authorAlduchov, Oleg A.
contributor authorEskridge, Robert E.
date accessioned2017-06-09T14:05:42Z
date available2017-06-09T14:05:42Z
date copyright1996/04/01
date issued1996
identifier issn0894-8763
identifier otherams-12300.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147625
description abstractAlgorithms, based on Magnus's form equations, are described that minimize the difference between several relationships between temperature and water vapor pressure at saturation that are commonly used in archiving data. The work was initiated in connection with the development of a unified upper-air dataset that will use measurements gathered from the late 1930s to the present and archived in several data centers. The conversion of field measurements to archived humidity values within the databases that are being used have not been consistent and in some cases are unknown. A goal of this work was to develop a uniform and accurate method to convert these data to various humidity variables without regard to the equations used in archiving the original data. Archived temperature values are recorded to 0.1°C. This precision creates a temperature dependent range in uncertainty in saturation vapor pressure. A procedure was developed to take this into account when the error minimizing equations were derived.
publisherAmerican Meteorological Society
titleImproved Magnus Form Approximation of Saturation Vapor Pressure
typeJournal Paper
journal volume35
journal issue4
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1996)035<0601:IMFAOS>2.0.CO;2
journal fristpage601
journal lastpage609
treeJournal of Applied Meteorology:;1996:;volume( 035 ):;issue: 004
contenttypeFulltext


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