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Atmospheric Boundary Layer Wind Data During the Period January 1, 1998 Through January 21, 1999 at the Dallas-Fort Worth Airport
Language: en
Pages: 236

Atmospheric Boundary Layer Wind Data During the Period January 1, 1998 Through January 21, 1999 at the Dallas-Fort Worth Airport

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Type: BOOK - Published: 2000 - Publisher:

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Atmospheric Boundary Layer Wind Data During the Period January 1, 1998 Through January 31, 1999 at the Dallas-Fort Worth Airport
Language: en
Pages: 24

Atmospheric Boundary Layer Wind Data During the Period January 1, 1998 Through January 31, 1999 at the Dallas-Fort Worth Airport

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Type: BOOK - Published: 2000 - Publisher:

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Atmospheric Boundary Layer Wind Data During the Period January 1, 1998 Through January 21, 1999 at the Dallas-Fort Worth Airport. Volume 2; Data and Processing
Language: en
Pages: 232

Atmospheric Boundary Layer Wind Data During the Period January 1, 1998 Through January 21, 1999 at the Dallas-Fort Worth Airport. Volume 2; Data and Processing

Authors: National Aeronautics and Space Administration (NASA)
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Type: BOOK - Published: 2018-06-27 - Publisher: Createspace Independent Publishing Platform

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The NASA Langley Research Center's Aircraft Vortex Spacing System (AVOSS) requires accurate winds and turbulence to determine aircraft wake vortex behavior near
NASA Langley Scientific and Technical Information Output 2000
Language: en
Pages: 162

NASA Langley Scientific and Technical Information Output 2000

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Type: BOOK - Published: 2001 - Publisher:

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Atmospheric Boundary Layer Wind Data During the Period January 1, 1998 Through January 31, 1999 at the Dallas-Fort Worth Airport. Volume 1; Quality Assessment
Language: en
Pages: 36

Atmospheric Boundary Layer Wind Data During the Period January 1, 1998 Through January 31, 1999 at the Dallas-Fort Worth Airport. Volume 1; Quality Assessment

Authors: National Aeronautics and Space Adm Nasa
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Type: BOOK - Published: 2018-09-27 - Publisher: Independently Published

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The quality of the Aircraft Vortex Spacing System (AVOSS) is critically dependent on representative wind profiles in the atmospheric boundary layer. These winds
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