For general information, see the ADCIRC site, ADCIRC FAQ, or the ADCIRC Wikipedia page. For model documentation not yet available on the wiki, see the ADCIRC site. New content is being continuously added to the ADCIRCWiki, and material from the main ADCIRC site will be gradually transitioned over to the wiki.
When wind blows over the water, it exerts a shear stress at the water surface that transfers horizontal momentum vertically downward across the air–sea interface, driving circulation. In ADCIRC, wind stress is an input forcing term, with several different formats provided. See the
NWS parameter for available formats. In most cases, the exact wind stress to be applied to the model is not provided, therefore ADCIRC must determine how to convert a given wind speed to the actual stress applied at the ocean surface. This page covers the various aspects of this process, as well as the options available to the user.
Definition of Winds
The characteristics of wind forcing are often broken down in three ways:
- Whether the winds are considered to be over-water (termed "marine exposure") or over-land
- The elevation above the sea (or ground) surface of the winds
- The time-averaging (if any) that has been applied
ADCIRC generally expects 10-meter, 10-minute winds at their actual exposure, although the exact expectations vary depending on the input type. For instance, when Holland-type wind inputs are provided (e.g.
NWS=20), the wind speed is expected to be the 1-minute maximum sustained wind at 10 meters elevation. If marine-exposure winds are provided, then surface roughness reductions may be needed
. If winds are provided with a different averaging time, then an appropriate correction may be needed, though winds with averaging times of 10 to 60 minutes are generally considered to be quite similar; this is the so-called mesoscale gap. For recommendations on wind time-scale conversions not handled internally by ADCIRC, for tropical cyclones, see the WMO guidelines of Harper et al.
for marine roughness length and reduced ("land") roughness length . Wind speed is then reduced as,
for x- and y- wind vector components and . The marine roughness length is,
for drag coefficient and acceleration due to gravity . The wind drag coefficient is addressed below in this section. As previously noted, the reduced ("land") roughness length is specified by the user via the surface roughness nodal attribute. The fraction is bounded on , meaning the winds cannot be increased, nor change direction.
|ADCIRC version:||< 54|
Note that before version 54, there was a bug in this calculation. The mistake and its effects are addressed in this PDF document: ADD A LINK TO A PDF HERE YOOOOO.
Converting Wind Speed to Wind Stress
In ADCIRC, four formulations are available to convert wind speeds to the wind stresses applied in the momentum equations. The default is the linear Garratt formulation,  An alternative for use with tropical cyclones is the Powell formulation,  which varies drag by the sector of the tropical cyclone. When ice coverage is included in the model, a wind drag formulation that accounts for this effect should be used. By default, if ice coverage input data are supplied, ADCIRC uses a cubic function of ice coverage, termed the "IceCube" drag formulation. Lastly, the "swell" drag law option allows users to utilize SWAN's drag formulation when employing the coupled model.
Garratt Drag Formulation
This is the default wind drag formulation in ADCIRC. From Garratt (1977), the formula is,
By default, ADCIRC puts an upper bound on the drag coefficient of . This upper bound
WindDragLimit can be changed via the metControl fort.15 namelist.
Powell Drag Formulation
IceCube Drag Formulation
- Simiu, E., Scanlan, R.H., 1996. Wind effects on structures: fundamentals and applications to design, 3rd ed. ed. John Wiley, New York.
- Simiu, E., Yeo, D., 2018. Wind effects on structures: modern structural design for wind, Fourth edition. ed. John Wiley & Sons, Hoboken, NJ.
- Harper, B., Kepert, J., Ginger, J., 2010. Guidelines for converting between various wind averaging periods in tropical cyclone conditions (No. WMO/TD-No. 1555). WMO, Geneva, Switzerland.
- Garratt, J.R., 1977. Review of Drag Coefficients over Oceans and Continents. Mon. Wea. Rev. 105, 915–929. https://doi.org/10.1175/1520-0493(1977)105<0915:RODCOO>2.0.CO;2
- Powell, M.D., Vickery, P.J., Reinhold, T.A., 2003. Reduced drag coefficient for high wind speeds in tropical cyclones. Nature 422, 279–283. https://doi.org/10.1038/nature01481