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Application of Land Surface Data Assimilation to Simulations of Sea Breeze CirculationsA technique has been developed for assimilating GOES-derived skin temperature tendencies and insolation into the surface energy budget equation of a mesoscale model so that the simulated rate of temperature change closely agrees with the satellite observations. A critical assumption of the technique is that the availability of moisture (either from the soil or vegetation) is the least known term in the model's surface energy budget. Therefore, the simulated latent heat flux, which is a function of surface moisture availability, is adjusted based upon differences between the modeled and satellite- observed skin temperature tendencies. An advantage of this technique is that satellite temperature tendencies are assimilated in an energetically consistent manner that avoids energy imbalances and surface stability problems that arise from direct assimilation of surface shelter temperatures. The fact that the rate of change of the satellite skin temperature is used rather than the absolute temperature means that sensor calibration is not as critical. The sea/land breeze is a well-documented mesoscale circulation that affects many coastal areas of the world including the northern Gulf Coast of the United States. The focus of this paper is to examine how the satellite assimilation technique impacts the simulation of a sea breeze circulation observed along the Mississippi/Alabama coast in the spring of 2001. The technique is implemented within the PSUNCAR MM5 V3-5 and applied at spatial resolutions of 12- and 4-km. It is recognized that even 4-km grid spacing is too coarse to explicitly resolve the detailed, mesoscale structure of sea breezes. Nevertheless, the model can forecast certain characteristics of the observed sea breeze including a thermally direct circulation that results from differential low-level heating across the land-sea interface. Our intent is to determine the sensitivity of the circulation to the differential land surface forcing produced via the assimilation of GOES skin temperature tendencies. Results will be quantified through statistical verification techniques.
Document ID
20030054436
Acquisition Source
Marshall Space Flight Center
Document Type
Conference Paper
Authors
Mackaro, Scott
(Alabama Univ. Huntsville, AL, United States)
Lapenta, William M.
(NASA Marshall Space Flight Center Huntsville, AL, United States)
Blackwell, Keith
(University of South Alabama Mobile, AL, United States)
Suggs, Ron
(NASA Marshall Space Flight Center Huntsville, AL, United States)
McNider, Richard T.
(Universities Space Research Association United States)
Jedlovec, Gary
(NASA Marshall Space Flight Center Huntsville, AL, United States)
Kimball, Sytske
(University of South Alabama Mobile, AL, United States)
Date Acquired
August 21, 2013
Publication Date
January 1, 2003
Subject Category
Earth Resources And Remote Sensing
Meeting Information
Meeting: AMS Conference on Interactions of the Sea and Atmosphere
Location: Long Beach, CA
Country: United States
Start Date: February 9, 2003
End Date: February 13, 2003
Sponsors: American Meteorological Society
Distribution Limits
Public
Copyright
Other

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