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• Wind surface stress
  Wind stress is calculated according to a quadratic friction law: ...>\rho_{a}</math> is air density and <math>\overrightarrow{W}</math> is the wind speed at a height of 10 m over the sea surface.
  407 bytes (68 words) - 11:39, 3 December 2008

Page text matches

• Module Hydrodynamic
  Diffusive flux of momentum is imposed explicitly by means of a [[wind surface stress]], <math> \tau_{ w}</math>:
  15 KB (2,263 words) - 13:33, 9 February 2022
• Module InterfaceWaterAir
  ...urring at the water-air interface, such as computing [[wind surface stress|wind shear stress]], radiation balances, latent and sensible heat fluxes. This m ...ntends to help the user to couple atmosphere to water, activating in MOHID wind forcing, heat fluxes and mass fluxes between this interface.
  8 KB (1,212 words) - 18:01, 1 June 2018
• Module Lagrangian
  ...n be influenced by the velocity field from the hydrodynamic module, by the wind from the surface module, by the spreading velocity from oil dispersion modu
  6 KB (765 words) - 14:54, 3 October 2019
• Module Oil
  ...n be influenced by the velocity field from the hydrodynamic module, by the wind from the surface module, by the spreading velocity from oil module and by r
  3 KB (365 words) - 11:38, 3 December 2008
• Module Waves
  The water-air interface module provides wind velocity, direction and shear stresses, receiving from the surface wave mod ...ocean) and ii) one approach for shalow restricted fetch areas dependent on wind velocity and direction (fetch lengths) and depth.
  24 KB (3,329 words) - 17:13, 2 December 2013
• Mohid GIS
  ...ation added to (iii) must have an X and a Y component (e.g. flow velocity, wind velocity). Information added to (iv) is the one produced by the lagrangian
  32 KB (5,286 words) - 16:54, 16 September 2009
• Notepadplus
  ...ON VELTANGENTIALBOUNDARY VELNORMALBOUNDARY NULL_BOUND_HORADV TIDEPOTENTIAL WIND ATM_PRESSURE SURFACEWATERFLUX HMIN_CHEZY VMIN_CHEZY DATA_ASSIMILATION IMPLI
  12 KB (1,314 words) - 11:38, 3 December 2008
• Op Mer MH Por v1
  *Evaporation due to radiation and wind action ???
  3 KB (436 words) - 11:38, 3 December 2008
• Properties names
  |wind angle||Char_WindAngle||WindAngle_|| |wind direction||Char_WindDirection||WindDirection_||
  18 KB (2,218 words) - 20:35, 15 February 2010
• Time Series
  ...certain column with the name of the property (e.g. temperature, salinity, wind speed, etc), a header line must be present on the line just above the '''<B '''wind direction''' is wrong
  3 KB (509 words) - 13:25, 18 January 2013
• Upwelling
  ...the Western Iberian coast. This corresponds to the zonal component of the wind. ...l flow integrated over depth. Thus, assuming a steady state constant zonal wind stress <math>\tau</math>
  3 KB (551 words) - 11:39, 3 December 2008
• Wind surface stress
  Wind stress is calculated according to a quadratic friction law: ...>\rho_{a}</math> is air density and <math>\overrightarrow{W}</math> is the wind speed at a height of 10 m over the sea surface.
  407 bytes (68 words) - 11:39, 3 December 2008
• ATM PRESSURE
  [[WIND]] : 2 *[[WIND]]
  3 KB (304 words) - 11:26, 3 December 2008
• ATM PRESSURE TYPE
  [[WIND]] : 2 *[[WIND]]
  3 KB (338 words) - 11:26, 3 December 2008
• Applications
  deCastro M, Gómez-Gesteira M, Prego R, Neves R. Wind influence on water exchange between the ria of Ferrol (NW Spain) and the sh Janeiro J, Fernandes E, Martins F, Fernandes R. Wind and freshwater influence over hydrocarbon dispersal on Patos Lagoon, Brazil
  14 KB (2,039 words) - 18:20, 26 November 2010
• Atmospheric boundary condition
  Zonal wind velocity NAME : wind velocity X
  8 KB (767 words) - 15:05, 30 July 2017
• Blumberg-Kantha radiation scheme
  ...scheme provides acceptable results in a 2D barotrophic model with tide and wind.
  4 KB (693 words) - 13:50, 28 February 2012
• Continuous
  ...n using a ramp period for wind forcing change from '''WIND : 2''' to '''WIND : 1''' and remove keyword [[WIND_SMOOTH_PERIOD]] from the data file.
  4 KB (551 words) - 11:27, 3 December 2008
• ConvertToHDF5
  p10u wind velocity X p10v wind velocity Y
  61 KB (7,931 words) - 19:29, 26 October 2015
• Coupling Water-Atmosphere User Manual
  ...tries to answer to three main processes in what atmosphere takes part: i) wind forcing; ii) heat fluxes between air and water; iii) mass fluxes between ai ...water warming and cooling processes and thermal stratification formation. Wind can play an important role on surface stress and on mixture depth control,
  17 KB (2,142 words) - 17:14, 16 June 2017

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