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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
  • Evolution
    ...It takes into account the Ekman spiral, provided the model is forced with wind stress at the surface, or with friction at the bottom.
    880 bytes (124 words) - 11:27, 3 December 2008
  • Fetch
    ...nd on the surface of the water, between this point and the point where the wind effect started to take place. ...g several directions, each one with a different weight. Thus, for the same wind direction, a point with more obstacles in the near directions has assigned
    1 KB (197 words) - 11:27, 3 December 2008
  • How to configure a 2D model forced with tide with MOHID
    The module atmosphere configures the atmospheric forcing such as wind, solar radiation, latent and sensible heat sea-air exchange, infrared radia
    14 KB (2,266 words) - 18:13, 26 December 2011
  • Hydrolight
    ...the state of the sea surface, we will have to provide Hydrolight with the wind speed. In order to calculate the surface radiation , we will have to define
    32 KB (5,216 words) - 11:27, 3 December 2008
  • Meteo
    === GFS wind files === #*Daily 1 day wind forecasts(from 0h00 to 21h00) from GFS model covering the North Atlantic
    4 KB (690 words) - 11:27, 3 December 2008
  • Module Atmosphere
    ...compute processes occurring at the water-air interface, such as computing wind shear stress, radiation balances, latent and sensible heat fluxes. ...ntends to help the user to couple atmosphere to water, activating in MOHID wind forcing, heat fluxes and mass fluxes between this interface.
    5 KB (640 words) - 15:05, 26 June 2015
  • Module FillMatrix
    ...out all MOHID modules, two-dimensional (e.g. water elevation, wave height, wind velocity, bottom roughness length, etc.) and three-dimensional (e.g. temper ...perty values will remain constant throughout the simulation (e.g. constant wind speed and direction in a scenario simulation).
    9 KB (1,162 words) - 11:05, 22 April 2014
  • Module Basin
    :u<sub>2</sub> = average hourly wind speed at 2m hight [m s-1].
    14 KB (1,941 words) - 12:49, 20 July 2017
  • Eutrofização Albufeiras
    ...s_Eutrofizacao\ComoFazer\1.PreparaInputs\1.Dados\Meteorologia\meteo_files. Wind effect on surface water may be dependent on events and not represented by m WIND = Wind Speed (m/s - Use the original for now)
    32 KB (5,188 words) - 16:16, 2 November 2011
  • GFS
    *U - U-Component of Wind 10 m above ground [m/s] *V - V-Component of Wind 10 m above ground [m/s]
    5 KB (811 words) - 11:49, 29 February 2012
  • Light extinction
    ...Manual|processes occurring at the water-air interface]], such as computing wind shear stress, radiation balances, latent and sensible heat fluxes.
    39 KB (5,326 words) - 18:06, 22 February 2012
  • Mohid Bibliography
    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
    261 KB (37,509 words) - 23:24, 1 April 2024
  • Operational Modelling
    wind velocity X wind velocity Y
    18 KB (2,094 words) - 14:14, 1 June 2011
  • Module SedimentQuality
    wind - km/day
    8 KB (928 words) - 20:46, 8 December 2013
  • Mohid Swan
    The Swan model would need of wind, tide and deep-Ocean swell as boundary conditions. == Wind ==
    15 KB (2,233 words) - 16:07, 28 June 2011
  • Run SWAT Model - ArcView Interface
    This file points to weather stations that will create climate variables (wind, humidity, etc..) so you should check which is closer to your watershed usi
    19 KB (3,238 words) - 15:56, 2 November 2011
  • Geostrophic Initialization
    WIND : 1
    2 KB (209 words) - 12:05, 31 January 2012
  • Calibration/Validation in Mohid Land
    ...alidate other meteorology data (temperature, relative humidity, radiation, wind velocity) important for reference evapotranspiration. For other variables as radiation, relative humidity, temperature, wind velocity that interfere for instance on reference evapotranspiration comput
    14 KB (2,283 words) - 16:50, 1 July 2013
  • SNIRH Meteorological Stations
    ...ny stations with historical data available, at least for precipitation and wind speed, but sometimes for solar radiation, humidity and air temperature can
    770 bytes (128 words) - 15:40, 28 November 2012
  • Mohid Ocean Downscalling
    NAME : wind velocity X NAME : wind velocity Y
    38 KB (4,047 words) - 14:36, 23 May 2017
  • New: MOHID Water Vectorial and Angle Properties
    ...OHID in ModuleAtmosphere and ModuleWaves have nautical referential (0º is wind or wave from N towards S, 90º is from East towards West and so on). This an example of wind velocity X and wind velocity Y in Atmosphere_X.dat file until now:
    9 KB (1,209 words) - 15:32, 25 February 2016
  • Keyword list
    |1D vertical model of the water column. Only coriolis and wind stress. Neuman conditions of horizontal null gradient are imposed for veloc | rowspan="3" |WIND
    177 KB (22,102 words) - 14:20, 19 April 2023
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