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dc.contributor.authorParish, Thomas R.
dc.contributor.authorRahn, David A.
dc.contributor.authorLeon, David C.
dc.date.accessioned2017-11-22T17:06:46Z
dc.date.available2017-11-22T17:06:46Z
dc.date.issued2016-09-12
dc.identifier.citationParish, T. R., Rahn, D. A., & Leon, D. C. (2016). Aircraft Measurements and Numerical Simulations of an Expansion Fan off the California Coast. Journal of Applied Meteorology and Climatology, 55(9), 2053-2062. doi:10.1175/jamc-d-16-0101.1en_US
dc.identifier.urihttp://hdl.handle.net/1808/25450
dc.description.abstractMountains along the California coastline play a critical role in the dynamics of marine atmospheric boundary layer (MBL) airflow in the vicinity of the shoreline. Large changes in the MBL topology have been known to occur downwind of points and capes along the western coast of the United States. Large spatial gradients in wind and temperature become established that can cause anomalous electromagnetic wave propagation. Detailed airborne measurements using the University of Wyoming King Air were conducted to study the adjustment of the MBL to the Point Arguello and Point Conception headlands. Pronounced thinning of the MBL consistent with an expansion fan occurred to the south of Point Conception on 13 June 2012. A sharp cloud edge was collocated with the near collapse of the MBL. D-value cross sections derived from differential GPS altitude measurements allow assessment of the vertical profile of the horizontal pressure gradient force and hence thermal wind forcing in response to the near collapse of the MBL. The Weather Research and Forecasting Model was run with a 1-km grid spacing to examine the atmospheric adjustment around Point Conception during this period. Results from the simulations including the vertical cross sections of the horizontal pressure gradient force were consistent with the aircraft observations. Model results suggest that divergence occurs as the flow rounds Point Conception, characteristic of an expansion fan. Wind speeds in the MBL increase coincident with the decrease in MBL thickness, and subsiding flow associated with the near collapse of the MBL is responsible for the sharp cloud edge.en_US
dc.publisherAmerican Meteorological Societyen_US
dc.rights© Copyright 2016 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. All AMS journals and monograph publications are registered with the Copyright Clearance Center (http://www.copyright.com). Questions about permission to use materials for which AMS holds the copyright can also be directed to the AMS Permissions Officer at permissions@ametsoc.org. Additional details are provided in the AMS Copyright Policy statement, available on the AMS website (http://www.ametsoc.org/CopyrightInformation).en_US
dc.subjectAtm/Ocean Structure/Phenomenaen_US
dc.subjectMarine boundary layeren_US
dc.subjectObservational techniques and algorithmsen_US
dc.subjectAircraft observationsen_US
dc.subjectModels and modelingen_US
dc.subjectNumerical analysis/modelingen_US
dc.titleAircraft Measurements and Numerical Simulations of an Expansion Fan off the California Coasten_US
dc.typeArticleen_US
kusw.kuauthorRahn, David A.
kusw.kudepartmentGeography and Atmospheric Scienceen_US
dc.identifier.doi10.1175/JAMC-D-16-0101.1en_US
kusw.oaversionScholarly/refereed, publisher versionen_US
kusw.oapolicyThis item meets KU Open Access policy criteria.en_US
dc.rights.accessrightsopenAccessen_US


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