Last edited by Tuzragore
Wednesday, August 5, 2020 | History

2 edition of Numerical prediction of the mean wind over water waves found in the catalog.

Numerical prediction of the mean wind over water waves

by Kenneth G. Dunning

  • 386 Want to read
  • 4 Currently reading

Published by Naval Postgraduate School in Monterey, California .
Written in English

    Subjects:
  • Meteorology

  • ID Numbers
    Open LibraryOL25326527M

    Liu, Yi Yang, Di Guo, Xin and Shen, Lian Numerical study of pressure forcing of wind on dynamically evolving water s of Fluids, Vol. 22, Issue. 4, p. Section - Wave Predictions Based on Wind Statistics. _ "M/S FAMITA was a rescue vessel lying stand by in the North Sea from the middle of the 50's to the late 70's. The position was 57deg 30' North and 3deg 00' East. The vessel reported wind and wave .

      Statistics over the urban pixels in Table 2 (the corresponding area is represented in Fig. 3, and is identified with an urban fraction of 10% or more, a water fraction of 10% or less, and a valid remotely sensed surface temperature) confirm that the mean bias over urban pixels is negative and almost similar (− K for URB and − K for Cited by: Wind waves, with periods of a few seconds, and the tides, with periods of twelve hours or more, are really two examples of the same physical phe-nomenon. They di er only in the source of their energy. For the shortest-period waves|periods of, say, one to four seconds|the connection between the wind and the waves is obvious.

    Numerical weather prediction (NWP) uses mathematical models of the atmosphere and oceans to predict the weather based on current weather conditions. Though first attempted in the s, it was not until the advent of computer simulation in the s that numerical weather predictions produced realistic results. A number of global and regional forecast models are run in different countries. Just like the random waves, wind blowing over the deck structure is also random having a mean speed superimposed on it. This wind spectrum may be important to consider for certain types of offshore structures. There are several wind spectrum models available. Here we have adopted the expression of the wind frequency spectrum according to the.


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Numerical prediction of the mean wind over water waves by Kenneth G. Dunning Download PDF EPUB FB2

Search the history of over billion web pages on the Internet. search Search the Wayback Machine. Featured texts All Books All Texts latest This Just In Smithsonian Libraries FEDLINK (US) Genealogy Lincoln Collection. National Emergency Library.

Top American Libraries Canadian. NumericalPredictionoftheMeanWind OverWaterWaves by g Lieutenant,UnitedStatesNavy B.S.,HumboldtStateCollege, Submittedinpartialfulfillmentofthe. A numerical model for wind-wave prediction in deep water [Resio, Donald T.] on *FREE* shipping on qualifying offers.

A numerical model for wind-wave prediction in deep water on orders over $ shipped by Amazon or get Fast, Free Shipping with Author: Donald T. Resio. Through numerical solutions it was possible to determine that: 1) mean wind velocities at lower levels closely approximate the initial mean velocity profile for large wave numbers (k >/- m(-1)) or small wave amplitudes, 2) mean wind velocities at lower levels fluctuate more from the initial mean velocity profile as the wave number decreased or the wave amplitude increases, 3) solutions were very Author: Kenneth G.

Dunning. 1 FIELD MEASUREMENTS AND NUMERICAL MODELING OF WIND-WAVES IN LAKE BIEL: A BASIC TOOL FOR SHORE PROTECTION PROJECTS SAYAH S.M.1, MAI S.2, BOILLAT J-L.3, and SCHLEISS A.J.4 1) Ecole Polytechnique Fédérale de Lausanne (EPFL), Laboratory of Hydraulic Constructions (LCH), CH Lausanne, Switzerland.

applications of numerical wind wave models are shown, aimed to study both the wind wave. physics and global wind-wave variability at the climate scale, including mechanical energy.

exchange between wind, waves, and upper water layer. Parameterization of the wind‐water‐waves interaction is a key problem of the air Numerical algorithm and DNS results of a turbulent wind flow over water surface Comparison of the DNS results with t Cited by: turbulent wind flow over surface waves for Reynolds num-ber (based on the bulk wind flow velocity, surface wave-length l, and air molecular viscosity) Re = and wave steepness ka = (where k is the wave number and a is the wave amplitude).

Later Yang and Shen [] employed DNS to study the turbulent wind flow over waves withCited by: In the present paper we discuss numerical algorithm and results of DNS of a turbulent wind flow over a wavy water surface.

Waves with maximum steepness of ka =wave age 0. Advances in numerical weather prediction represent a quiet revolution because they have resulted from a steady accumulation of scientific knowledge and technological advances over many years that, with only a few exceptions, have not been associated with the aura of fundamental physics.

As an alternative, we consider direct numerical simulations (DNS). In the present paper we discuss numerical algorithm and results of DNS of a turbulent wind flow over a wavy water surface. Waves with maximum steepness of ka =wave age 0, and Reynolds number Re = 15, are considered.

The present paper is an attempt to predict (for comparison) the wave conditions that would have been encountered by the moving ship from analysis of the oceanwide weather records and the use of a high-speed digital computer process for forecasting waves in moving, variable wind systems.

The wave prediction technique is dependent on generalizations of emprical laws derived Cited by: Numerical predictions of ocean wave characteristics are now provided by the WAVEWATCH III model, originally developed by NOAA in the US and implemented operationally by CAWCR and NMOC.

This model replaces the Bureau's WAM model, and is run on global, regional and Australia domains as used in ACCESS. Nevertheless, the wave breaking effect has to be considered for a reasonable prediction of the evolution of water waves.

In addition, modeling the wind forcing effect is necessary for nonlinear waves under wind action which transfers energy to waves, induces wave growth, and Cited by: 2) the effect of wind waves in the second event on two kind of fluxes is strong, too. and its moving from west to east follows the cold front.

It causes stronger active fluxes at south part than at north part of the yellow sea. (4) The wind waves motivate more air-sea momentum flux and heat Size: 3MB. The book gives the user all the necessary elements to build a numerical model. An Introduction to Numerical Weather Prediction Techniques is rich in illustrations, especially tables showing outputs from each individual algorithm presented.

Selected figures using actual meteorological data are also by: What is NWP. • A quantitative future forecast of weather (or climate) based on a model or a set of model or a set of model solutions to predict temperature, wind, rain, snow, hail, etc.

over a prescribed domain • Forecast is created from a set of PDE’s and other process equations that describe the dynamic and thermodynamic processes in the earths atmosphere. Although the Charnock parameter has been related to ocean wave age, as functions of the ratio of the wave phase speed at the peak of the spectrum and either the friction velocity or the m neutral wind speed U 10N (Drennan et al.

; Donelan ), Fairall et al. () pointed out that there is still a lack of consensus on the relationship Cited by: 2. forecast than deterministic (or control) forecast after a short lead-time ( days) for the global model application.

There is about a day improvement in the forecast skill when using ensemble mean instead of a single forecast for longer lead-time. The skillful forecast (65% and above of an anomaly correlation) could be extended to File Size: KB.

Over the ocean, turbulent pressure fluctuations in the air initiate small ripples on the water surface 9 that further grow and develop into wind-driven waves through a. Wave predictions are necessary for the design of offshore wind turbine. The waters around Japan, large swells are caused by waves propagated over Pacific ocean.

Furthermore, not only large swells but also wind waves are induced by tropical cyclones. In the conventional studies, different wave models and wind fields for wave simulations have.Wind- and Density-Driven Water Circulation 31 1.

Introduction One of the first problems one has to deal with when applying a numerical model to an analysis of hydrodynamic processes in a real water basin is the choice of spatial and time resolution of the model. The choice is usually a compromise between available.An investigation of the turbulent flow structure over a progressive water wave, as well as the structure of the wave-induced flow field in a transformed wave-following frame, is reported.

Experimental results are given for a free-stream velocity of 24 m s−1 over Cited by: