An evaluation of the Naval Oceanic Vertical Aerosol Model during Key90

  • 54 Pages
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Naval Postgraduate School, Available from the National Technical Information Service , Monterey, Calif, Springfield, Va
ContributionsDavidson, Kenneth L.
The Physical Object
Pagination54 p. ;
ID Numbers
Open LibraryOL25519366M

Calhoun: The NPS Institutional Archive Theses and Dissertations Thesis Collection An evaluation of the Naval Oceanic Vertical Aerosol Model during Key   An illustration of an open book. Books. An illustration of two cells of a film strip. Video An illustration of an audio speaker. An evaluation of the Naval Oceanic Vertical Aerosol Model during Key Item Preview remove-circle An evaluation of the Naval Oceanic Vertical Aerosol Model during Key by Cecere, Thomas H.;Davidson, Kenneth : An Evaluation of the Naval Oceanic Vertical Aerosol Model During Key90 by Thomas H.

Cecere Lieutenant, United States Navy B.S., State University of New York at Stony Brook, Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE IN METEOROLOGY AND PHYSICAL OCEANOGRAPHY from the NAVAL POSTGRADUATE SCHOOLAuthor: Thomas H. Cecere. Abstract.

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Approved for public release; distribution is unlimitedAn experiment was conducted in the Florida Keys from 2 - 19 July to test the performance of the Naval Oceanic Vertical Aerosol Model (NOVAM) in a weak-convective regime Meteorological data collected by aircraft and boat was used to generate the surface and vertical profile information files required by : Thomas H.

Cecere. Ocean aerosol measurements and models in the straits of Florida (the Key experiment) p. 2 NOVAM evaluation from aerosol and lidar measurements in a tropical marine environmentp. 14 Modeling aerosol extinction in a coastal environment p. 28 Aerosol induced loss of image resolution p.

The Naval Oceanic Vertical Aerosol Model (NOVAM) has been formulated to estimate the vertical structure of the optical and infrared extinction coefficients in the marine atmospheric boundary layer (MABL).

NOVAM was designed to predict the non-uniform and non-logarithmic extinction profiles which are often observed. It is based on a combination of empirical and physical models which describe.

The naval oceanic vertical aerosol model: progress report () Pagina-navigatie: Main; Save publication. Save as MODS; Export to Mendeley; Save as EndNote. NOVAM, the Naval Oceanic Vertical Aerosol Model, has been developed to predict the nonuniform and nonlogarithmic extinction profiles that are often observed in the marine atmospheric boundary layer.

The kernel of NOVAM is the Navy Aerosol Model (NAM) that calculates the aerosol size distribution at 10 m ASL from meteorological parameters. The aerosol profile is calculated from the surface.

NOVAM, the Naval Oceanic Vertical Aerosol Model, has been developed to predict the nonuniform and nonlogarithmic extinction profiles that are often observed in the marine atmospheric boundary layer.

The kernel of NOVAM is the Navy Aerosol Model (NAM) that calculates the aerosol size distribution at 10 m ASL from meteorological parameters. A number of models are reviewed for the atmospheric aerosols, clouds, and precipitation and their effects on the propagation of electromagnetic radiation at wavelengths from the ultraviolet.

Advanced Search >. Home > Proceedings > Volume > Proceedings > Volume NOVAM, the Naval Oceanic Vertical Aerosol Model, has been developed to predict the nonuniform and nonlogarithmic extinction profiles that are often observed in the marine atmospheric boundary layer. The development of higher resolution AGCMs and OGCMs is one of the most active areas of study in the model development field.

At the Institute of Atmospheric Physics (IAP), Chinese Academy of Sciences (CAS), over 30 years have passed since the IAP’s AGCM was first designed induring which time the model has been continually developed.

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The data set collected during 11–16 September was analysed in terms of aerosol transport (HYbrid Single-Particle Lagrangian Integrated Trajectory model (HYSPLIT)), aerosol load model simulations (Copernicus Atmosphere Monitoring Service (CAMS), Navy Aerosol Analysis and Prediction System (NAAPS), Global Environmental Multiscale-Air.

Visibility reduction Atmospheric visibility is defined by the ability of our eyes to distinguish an object from the surrounding background. Scattering of solar radiation by aerosols is the main process limiting visibility in the troposphere ().In the absence of aerosols our visual range would be approximately km, limited by scattering by air molecules.

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Knowledge in naval architecture is used to. cal model can extend the extinction prediction to higher altitudes. A Naval Oceanic Vertical Aerosol Model (NOVAM) is being developed to provide the vertical variation of the optical/IR properties of the marine atmosphere (Gathman, ; de Leeuw et al., a, b; Davidson et.

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high horizontal and vertical resolution are needed to depict the 3D structure with accuracy superior to climatology and/or persistence (i.e., a forecast of no change). The existing two-model operational system, run daily at the Naval Oceanographic Office (NAV-OCEANO), is based on the 1/32° Navy.

Graham Feingold (National Oceanic and Atmospheric Administration) has collaborated on using large eddy simulation to study aerosol effects in the marine atmosphere. Haflidi Jonsson at the Naval Postgraduate School is instrumental in the aircraft operations and the data management, which is.

marine atmosphere over a broad range of spatial and temporal scales. The work during the last year included the following tasks: • Characterize and conduct airborne measurements with a state-of-the-art instrument to quantify aerosol-water interactions, termed the differential aerosol sizing and hygroscopicity spectrometer probe (DASH-SP).

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