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  2. LazPaint - Wikipedia

    en.wikipedia.org/wiki/LazPaint

    Added brush and clone tool, palette, docking of toolbox, rain rendering, when saving show preview and choice of bit depth [29] 7.0 beta 17 August 2019 Vector layers, edit shape tool, shape alignment, wave displacement filter, non-lossy transform of layers, zoom layer tool, edit frame of ICO / CUR / GIF, Lab colorspace support when reading TIFF [30]

  3. Douglas sea scale - Wikipedia

    en.wikipedia.org/wiki/Douglas_sea_scale

    The Douglas sea scale is a scale which measures the height of the waves and also measures the swell of the sea. The scale is very simple to follow and is expressed in one of 10 degrees. The scale is very simple to follow and is expressed in one of 10 degrees.

  4. Dispersion (water waves) - Wikipedia

    en.wikipedia.org/wiki/Dispersion_(water_waves)

    Dispersion of gravity waves on a fluid surface. Phase and group velocity divided by shallow-water phase velocity √ gh as a function of relative depth h / λ. Blue lines (A): phase velocity; Red lines (B): group velocity; Black dashed line (C): phase and group velocity √ gh valid in shallow water.

  5. Category:Water waves - Wikipedia

    en.wikipedia.org/wiki/Category:Water_waves

    Wave base; Wave height; Wave radar; Wave setup; Wave shoaling; Wave tank; Wave turbulence; Wave–current interaction; Wave-making resistance; Wave-piercing hull; Waves and shallow water; Whitham equation; Wind setup; Wind wave model; Wind-wave dissipation

  6. ANUGA Hydro - Wikipedia

    en.wikipedia.org/wiki/ANUGA_Hydro

    The mathematical model is the 2D shallow water wave equation. As such it cannot resolve vertical convection and consequently not breaking waves or 3D turbulence (e.g. vorticity). All spatial coordinates are assumed to be UTM (meters). As such, ANUGA is unsuitable for modelling flows in areas larger than one and half UTM zones (9 degrees wide).

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  8. Shallow water equations - Wikipedia

    en.wikipedia.org/wiki/Shallow_water_equations

    Shallow-water equations can be used to model Rossby and Kelvin waves in the atmosphere, rivers, lakes and oceans as well as gravity waves in a smaller domain (e.g. surface waves in a bath). In order for shallow-water equations to be valid, the wavelength of the phenomenon they are supposed to model has to be much larger than the depth of the ...

  9. 5 Tips to Make the Best Alcohol-Free Cocktails, According to ...

    www.aol.com/5-tips-best-alcohol-free-182900197.html

    Gone are the days of the sad mocktail — the cranberry cocktail topped with a bit of seltzer or a blend of every juice behind the bar. A growing number of bartenders are paying just as much ...