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The best definition I know of "moving average" is: http://mathworld.wolfram.com/MovingAverage.html In Meteorology, the "one pass Cressman" (which applies a distance-based, non-linear weight to all observation points within a "circle of influence") demonstrates this -- it is essentially an inverse distance-weighted average of all the data points where the weight is > 0. A more sophisticated extension was introduce by Barnes, and involves multiple passes through the data (see Barnes 1994 article in Journal of Atmos and Oceanic Technology). tom On Tue, 8 Jan 2002, gaoming fu wrote: > > Hello, All > > Recently some one told me that Moving average is another good way for > interpolation. But I have no idea about it. Does VisAD suppor it? > > For example, for an area of 10 by 10 m, I have some irregular points (with x, > y, > and z). > Now I want to draw the surface using a grid with cell size of 1 m. First I > have to > interpolate > these grid points to get the z values (this can be easily done using > WEIGHTED_AVERAGE > and NEAREST_NEIGHBOR methods in VisAD), then draw those grid points. Now I > want to > try the so called "Moving average" approach. The purpose is to get a smooth > surface so that it is very close to the real topography visually. > > Any help will be highly apprecaited. > > Gaoming Fu > > > > > > _________________________________________________________________________________________ > Chat with friends online, try MSN Messenger: Click Here > > -- Tom Whittaker University of Wisconsin-Madison Space Science and Eng. Center ph: 608.262.2759
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