A further note on tuning the LFM gradient wind relation

O'Lenic, Edward A.

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A further note on tuning the LFM gradient wind relation

1980
By O'Lenic, Edward A.
Series: Office note (National Centers for Environmental Prediction (U.S.)) ; 225

[PDF-546.53 KB]

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Personal Author:

O'Lenic, Edward A.
Corporate Authors:

National Meteorological Center (U.S.)
NOAA Program & Office:

NWS (National Weather Service) ; NCEP (National Centers for Environmental Prediction)

NWS (National Weather Service) ; NCEP (National Centers for Environmental Prediction) Less -
Description:

"This note is intended to refine and extend the results of Office Note 222. In that paper, heights analyzed by the Hough analysis scheme and output on a 1-Bedient 65-by-65 grid were used to compute gradient winds. By varying a parameter in the gradient wind equation and repeatedly calculating winds, an optimum value of the parameter was chosen. This process is repeated in the current paper. This time, however, the calculations are done at 4 pressure levels on both the 1-Bedient 65-by-65 grid again using Hough height analyses, and on the 1/2-Bedient 53-by-57 grid using height analyses from the LFM (Cressman type analysis), and a larger number of cases than was used in the previous note"--Introduction.
Content Notes:

Edward A.. O'Lenic.

"December 1980."

"This is an unreviewed manuscript, primarily intended for informal exchange of information among NMC staff members."

System requirements: Adobe Acrobat Reader.

Includes bibliographical references.
Keywords:

[+]

Mathematical Models Numerical Analysis Numerical Weather Forecasting Wind Forecasting
Series:

Office note (National Centers for Environmental Prediction (U.S.)) ; 225
Document Type:

Office Note
Place as Subject:

United States
Rights Information:

Public Domain
Compliance:

Library
Main Document Checksum:

[+]

urn:sha256:95bdec959cb7ff4a99cfa67bc5ebfb910cf8ddbcf46976c69fc76e3c51c56860
Download URL:

https://repository.library.noaa.gov/view/noaa/12142/noaa_12142_DS1.pdf
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A further note on tuning the LFM gradient wind relation

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