Statistics and Dynamics of Aircraft Encounters of Turbulence over Greenland

Historical records of aviation turbulence encounters above Greenland are examined for the period from 2000 to 2006. These data identify an important flow regime that contributes to the occurrence of aircraft turbulence encounters, associated with the passage of surface cyclones that direct easterly...

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Main Authors: Lane, Todd P., Doyle, James D., Sharman, Robert D., Shapiro, Melvyn A., Watson, Campbell D.
Other Authors: NAVAL RESEARCH LAB MONTEREY CA
Format: Text
Language:English
Published: 2009
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA513026
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA513026
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spelling ftdtic:ADA513026 2023-05-15T16:26:44+02:00 Statistics and Dynamics of Aircraft Encounters of Turbulence over Greenland Lane, Todd P. Doyle, James D. Sharman, Robert D. Shapiro, Melvyn A. Watson, Campbell D. NAVAL RESEARCH LAB MONTEREY CA 2009-08 text/html http://www.dtic.mil/docs/citations/ADA513026 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA513026 en eng http://www.dtic.mil/docs/citations/ADA513026 Approved for public release; distribution is unlimited. DTIC Aircraft Meteorology Fluid Mechanics *AIRCRAFT *TURBULENCE *CYCLONES *FLOW *GREENLAND TERRAIN AERONAUTICS MOUNTAINS HISTORY WIND SHEAR WAVES DIRECTIONAL FORECASTING DYNAMICS MODELS REPRINTS DATA BASES SIMULATION AIRCRAFT TURBULENCE PE0601153N Text 2009 ftdtic 2016-02-22T22:59:16Z Historical records of aviation turbulence encounters above Greenland are examined for the period from 2000 to 2006. These data identify an important flow regime that contributes to the occurrence of aircraft turbulence encounters, associated with the passage of surface cyclones that direct easterly or southeasterly flow over Greenland's imposing terrain. The result of this incident flow is the generation of mountain waves that may become unstable through interactions with the background directional wind shear. It is shown that this regime accounted for approximately 40% of the significant turbulent events identified in the 7-yr database. In addition, two specific cases from the database are examined in more detail using a high-resolution mesoscale model. The model simulations highlight the important role of three-dimensional gravity wave-critical level interactions and demonstrate the utility of high-resolution forecasts in the prediction of such events. Published in the Monthly Weather Review, v137 p2687-2702 Aug 2009. Text Greenland Defense Technical Information Center: DTIC Technical Reports database Greenland
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Aircraft
Meteorology
Fluid Mechanics
*AIRCRAFT
*TURBULENCE
*CYCLONES
*FLOW
*GREENLAND
TERRAIN
AERONAUTICS
MOUNTAINS
HISTORY
WIND SHEAR
WAVES
DIRECTIONAL
FORECASTING
DYNAMICS
MODELS
REPRINTS
DATA BASES
SIMULATION
AIRCRAFT TURBULENCE
PE0601153N
spellingShingle Aircraft
Meteorology
Fluid Mechanics
*AIRCRAFT
*TURBULENCE
*CYCLONES
*FLOW
*GREENLAND
TERRAIN
AERONAUTICS
MOUNTAINS
HISTORY
WIND SHEAR
WAVES
DIRECTIONAL
FORECASTING
DYNAMICS
MODELS
REPRINTS
DATA BASES
SIMULATION
AIRCRAFT TURBULENCE
PE0601153N
Lane, Todd P.
Doyle, James D.
Sharman, Robert D.
Shapiro, Melvyn A.
Watson, Campbell D.
Statistics and Dynamics of Aircraft Encounters of Turbulence over Greenland
topic_facet Aircraft
Meteorology
Fluid Mechanics
*AIRCRAFT
*TURBULENCE
*CYCLONES
*FLOW
*GREENLAND
TERRAIN
AERONAUTICS
MOUNTAINS
HISTORY
WIND SHEAR
WAVES
DIRECTIONAL
FORECASTING
DYNAMICS
MODELS
REPRINTS
DATA BASES
SIMULATION
AIRCRAFT TURBULENCE
PE0601153N
description Historical records of aviation turbulence encounters above Greenland are examined for the period from 2000 to 2006. These data identify an important flow regime that contributes to the occurrence of aircraft turbulence encounters, associated with the passage of surface cyclones that direct easterly or southeasterly flow over Greenland's imposing terrain. The result of this incident flow is the generation of mountain waves that may become unstable through interactions with the background directional wind shear. It is shown that this regime accounted for approximately 40% of the significant turbulent events identified in the 7-yr database. In addition, two specific cases from the database are examined in more detail using a high-resolution mesoscale model. The model simulations highlight the important role of three-dimensional gravity wave-critical level interactions and demonstrate the utility of high-resolution forecasts in the prediction of such events. Published in the Monthly Weather Review, v137 p2687-2702 Aug 2009.
author2 NAVAL RESEARCH LAB MONTEREY CA
format Text
author Lane, Todd P.
Doyle, James D.
Sharman, Robert D.
Shapiro, Melvyn A.
Watson, Campbell D.
author_facet Lane, Todd P.
Doyle, James D.
Sharman, Robert D.
Shapiro, Melvyn A.
Watson, Campbell D.
author_sort Lane, Todd P.
title Statistics and Dynamics of Aircraft Encounters of Turbulence over Greenland
title_short Statistics and Dynamics of Aircraft Encounters of Turbulence over Greenland
title_full Statistics and Dynamics of Aircraft Encounters of Turbulence over Greenland
title_fullStr Statistics and Dynamics of Aircraft Encounters of Turbulence over Greenland
title_full_unstemmed Statistics and Dynamics of Aircraft Encounters of Turbulence over Greenland
title_sort statistics and dynamics of aircraft encounters of turbulence over greenland
publishDate 2009
url http://www.dtic.mil/docs/citations/ADA513026
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA513026
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA513026
op_rights Approved for public release; distribution is unlimited.
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