Jennifer,
An interesting task, but not for ESRI's software. Wind magnitude and direction are components of some two-dimensional vector. You may wish to interpret it as gradient and to restore its potential function (something like atmospheric pressure that causes wind). Strictly speaking, this is incorrect theoretically (because your vector field may not be a potential field), but you have finite number of grid points, and you can use this approach to study flow convergence and divergence.
After doing so, calculate plan curvature for your new grid of this "potential" using even ESRI's software, because flowline divergence is equal to plan curvature as proven by Theorem 4 of this paper:
Shary, P.A., 1995. Land surface in gravity points classification by a complete system of curvatures. Mathematical Geology 27(3): 373-390.
Plan curvature probably will not satisfy you, because it does not sum flows, is too sensitive to errors in data, and does not take into account important depressions in your "potential" (pressure). To have much better solution, you should change this approach by another one using so-called catchment area, but this is out of ESRI's competence. To my knowledge, they use only some "alchemy" in this direction on Silicon Graphics. This is why I've mentioned that your task is not for ESRI's software. You may learn the sense of catchment area and its scale-free features in the following paper:
Shary, P.A., Sharaya, L.S., Mitusov, A.V., 2002. Fundamental quantitative methods of land surface analysis. Geoderma 107(1-2): 1-32.
Together with catchment area, you will necessarily calculate depressions in your "potential". They are of great importance in land surface (Great Lakes, large deserts,...), why not in atmospheric pressure ?
This is the solution to your task, as I see it. You may wish to see map images at my website http://members.fortunecity.com/eco4/giseco/ or download free full-featured DEMO http://www.rockware.com/catalog/pages/giseco.html that performs what you are interesting in.
By the way, you're trying to study divergence, why not rotor? Its effects are essential in atmosphere. I'm doing this, it doesn't matter for which surface: land, human skin, pressure.
Hope this helps.
Peter ************************ Peter A. Shary, scientific researcher and GIS developer Institute of physical, chemical and biological problems of soil science of the Russian Academy of Sciences 142290 Poushchino Moscow region Russian Federation Phone: +7 0967 733604 Fax: +7 0967 790595 ************************
>From: "Jennifer Horsman" <jenh@gust.sr.unh.edu> >Reply-To: "Jennifer Horsman" <jenh@gust.sr.unh.edu> >To: "GISlist" <gislist@geocomm.com> >Subject: GISList: flow convergence and grids >Date: Thu, 3 Apr 2003 13:55:44 -0500 > >Does anyone know of a utility which allows calculation of flow convergence >and/or divergence from a grid with azimuth (angle of direction) and >magnitude of flow values at each cell (I am working with wind data)? I have >ESRI ArcGIS. > >Thanks, >Jennifer > > > > > >To unsubscribe, write to gislist-unsubscribe@geocomm.com >________________________________________________________________________ >GeoCommunity GeoBids - less than $1 per day! >Get Access to the latest GIS & Geospatial Industry RFPs and bids >http://www.geobids.com > >Online Archive of GISList (and numerous others) available at: >http://spatialnews.geocomm.com/community/lists/ > >Setup a GeoCommunity Account and have access to >the GISDataDepot DRG & DOQQ Catalog >http://www.geocomm.com/login.php >
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