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  • ...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
  • ...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
  • 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
  • ...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
  • === 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
  • ...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
  • ...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
  • :u<sub>2</sub> = average hourly wind speed at 2m hight [m s-1].
    14 KB (1,941 words) - 12:49, 20 July 2017
  • ...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
  • *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
  • ...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
  • 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
  • wind velocity X wind velocity Y
    18 KB (2,094 words) - 14:14, 1 June 2011
  • wind - km/day
    8 KB (928 words) - 20:46, 8 December 2013
  • 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
  • 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
  • WIND : 1
    2 KB (209 words) - 12:05, 31 January 2012
  • ...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
  • ...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
  • NAME : wind velocity X NAME : wind velocity Y
    38 KB (4,047 words) - 14:36, 23 May 2017

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