1 edition of Wind profiler study of the central California sea/land breeze // found in the catalog.
1996 by Naval Postgraduate School, Available from National Technical Information Service in Monterey, Calif, Springfield, Va .
Written in English
Sea/land-breeze events on the Monterey Bay are examined using data from the 915-MHz wind profiler and RASS systems. These sensors were deployed during Jun-Aug 1994 in conjunction with the REINAS Project conducted by various scientific institutions in the region. Data analyzed are continuous radar and virtual temperature returns located at four sites strategically positioned around the bay. This relatively new remote sensing device provides information on maximum and minimum sea/land breeze heights, onset and cessation times, virtual temperature distribution with height, and the effect of mountainous coastal topography on the sea and land breeze system.
|Statement||Jeffrey D. Stec|
|The Physical Object|
|Pagination||xii, 102 p. ;|
|Number of Pages||102|
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Wind profiler study of the central California sea/land breeze\ Item Preview Wind profiler study of the central California sea/land breeze\ by Stec, Jeffrey D. Publication date Some content may be lost due to the binding of the book.
Addeddate Call number o CameraPages: To compensate, the wind will blow from the higher pressure over the ocean to lower pressure over the land, which is called sea breeze.
Wind profiler study of the central California sea/land breeze // book A similar effect can occur near big lakes, where the wind is referred to as a lake breeze.
The sea breeze strength will vary depending on the temperature difference between the land and the ocean. AbstractOzone is one of the six “criteria” pollutants identified by the U.S. Clean Air Act Amendment of as particularly harmful to human health. Concentrations have decreased markedly across t.
The chosen period 24–25 April favoured sea breeze development and simultaneously allowed a comparison of the large-scale wind influence (north-westerly wind versus south-easterly wind) and.
The effects of basic flow and topography on the development of the sea breeze over a complex coastal environment Article in Quarterly Journal of the Royal Meteorological Society () - Zhong, S., J. Fast, and X. Bian, A case study of the Great Plains low-level jet using wind profiler network data and a high resolution mesoscale model.
Monthly Weather Review,temperature structure in California’s Central Valley. Journal of Applied Meteorology, A case study of the Great Plains low-level jet using wind profiler network data and a high resolution mesoscale model. Monthly Weather The effects of large-scale winds on the sea/Land -breeze circulations in an area of complex coastal File Size: KB.
for the study of the coastal lower atmosphere (e.g., Ko-racˇin and Dorman Bielli et al. Our purpose in this study is to compare scatterometer and model estimates of wind and wind stress over the coastal ocean in order to improve understanding of the coastal wind ﬁelds that drive coastal ocean circulation, and of the.
Atmospheric science wind anemometer cup anemometer wind vane propeller anemometer hot-wire anemometer radiosonde pibal dropsonde pitot tube radar lidar sodar wind profiler ultrasonic anemometer sonic anemometer LLWSAS low level wind shear alert system en-US text/html textual visual Higher Education Educator and learner Instructional Material.
Small-scale features of the thermally-driven wind field produced by the coupling between the lake breeze and the up-valley circulation into a unified mesoscale flow were revealed by RK-interpolated potential temperature 3D fields; the development of a lake-breeze front structure was captured in the shoreline area, while up-valley sections.
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Nearshore data measurements were collected through a field experiment carried out at Poetto beach (Southern Sardinia, Italy) during spring In addition to coastal observations, we use intermediate and deep water Cited by: 2.
Chia, L. A., Ed., A study of the urban climate of Singapore. The Biophysical Environment of Singapore and Its Neighbouring Countries. Geography Teachers Association of Singapore, Singapore Meteorological Services, pp. Book of Abstracts International Coastal Symposium Book of Abstracts Plymouth University, 8 – 12 April Editors Professor P.E.
Russell and Professor ink ICS, Plymouth University, United Kingdom Book of Abstracts Contents Oral Presentations 2 Poster Presentations. Flows up heated slopes are an elementary component of thermally-driven flows in complex terrain and play a fundamental role in the transport of air pollutants.
Our understanding of upslope flows is still incomplete because of the difficulty of carrying out field measurements in complex terrain, the sensitivity of upslope flows to external disturbances, and the difficulty of resolving Cited by: 7. PROFILER - A device for measuring the winds speeds and directions aloft.
Also called a VAD or Velocity Azimuth Display. A VAD wind profiler or VWP is a combination of the wind profiler instrument, similar to a vertical clear-air doppler radar, and the VAD display.
PROG - Short name for. Wilczak, J. and Coauthors, Contamination of wind profiler data by migrating birds: Characteristics of corrupted data and potential solutions.
Atmos. Filled with twists, Freak is an interesting character study as readers will understand who the monster is. Toxin Paul Martin Midden Millennial Mind Publishing $ The study investigates the sensitivity of the high-resolution mesoscale atmospheric model in the model reproduction of the combined large-scale wind and thermally induced local wind (i.e.
sea breeze) on the moist convection development. Issuu is a digital publishing platform that makes it simple to publish magazines, catalogs, newspapers, books, and more online. Easily share your publications and get them in front of Issuu’s.
On the interplay between sea-land breezes and Etesian winds over the Adriatic. // Journal of Marine Systems. 78 (), Suppl. 1; ss (članak, znanstveni). Grubišić Vanda; Stiperski, Ivana. Lee wave resonances over double bell-shaped obstacles.
// Journal of the atmospheric sciences. 66 (), 5; (članak, znanstveni. Wind indirectly affects coastal Physiographic setting and geology.
geomorphology as wind stress upon a water body causes the formation of waves and oceanic circulation. Tidal prism. EM 31 Jan Figure Energy-based classification of shorelines (from Hayes ()). NRL Review - Free ebook download as PDF File .pdf), Text File .txt) or read book online for free.
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An analysis of surface and wind profiler observations from the CCOS field experiment indicates a number of important low-level flows in the Central Valley: 1) the incoming low-level marine airflow through the Carquinez Strait into the Sacramento River delta, 2) the diurnal cycle of upslope?downslope flows, 3) the up- and down-valley flow in the.
First, days before the wind weakens near Pt. Conception, the wind weakens or reverses off Oregon and northern California. Second, the upwelling-favorable wind intensifies along central California. Third, the wind relaxes at Pt. Conception, and the area of weakened winds extends poleward to northern California over days.
Ozone, air pollution, and respiratory health. PubMed Central. Beckett, W. Of the outdoor air pollutants regulated by the Clean Air Act of (and recently revised in ), ozone has been the one pollutant most difficult to control within the federal standards.
The known human health effects are all on the respiratory system. At concentrations of ozone which occur during.
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Numerical model simulation of the largeamplitude mesoscale gravity wave event of 15 December in the central United States. Mon. Wea. Rev.,– Ralph, F. M., C. Mazaudier, M. Crochet, and S. Venkateswaran, Doppler sodar and radar wind-profiler observations of gravity-wave activity associated with a gravity current.
Mon. Specific phenomena of interest for air quality studies are examined. All model configurations are biased toward higher wind speeds than observed. The diurnal cycle of wind direction and speed (land–sea-breeze cycle) as modeled and observed by a wind profiler at. The Rossby number is defined as U/fL, where U is the basic wind speed and L the horizontal scale of the disturbance associated with the phenomenon.
The study concerned with the analysis and prediction of large- scale weather phenomena, based on the use of meteorological data obtained simultan- eously over the standard observational network, is. Res. %R /JD %V 32 %D %P %L pubs %X Various nonatmospheric signals contaminate radar wind profiler data, introducing bias into the moments and wind velocity estimation.
This study applies a fuzzy logic?based method to Doppler velocity spectra to identify and eliminate the clutter echoes.
European 15 — The European Conference on Marine Science and Ocean Technology Vol. I: Marine processes, ecosystems and interactions L Luxembourg EurOCEAN KI-NAEN-C OFFICE FOR OFFICIAL PUBLICATIONS OF THE EUROPEAN COMMUNITIES Commission Community Research Project synopses EurOCEAN The European Conference on Marine.
The book is especially suitable for self-study, as the author frequently provides ample explanation not only of what he is proving, but also of how and why he is proving it. As a reference work for the specialist or a text for the student, the book is highly recommended.'. Lagrangian R o Phenomenon Time scale (o/f 2p/fT) Tropical cyclone 2pR/V T V T /fR Inertia-gravity waves 2p/N to 2p/f N/f to 1 Sea/land breezes 2p/f 1 Thunderstorms and cumulus clouds 2p/N w N w /f KelvinHelmholtz waves 2p/N N/f PBL turbulence 2ph/U * U * /fh Tornadoes 2pR/V T V T /fR where: R radius of maximum wind scale, o frequency, T time 5/5(1).
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