[ESIP-all] BESSIG meeting: Interpolation, Wed, 10/23, 4:00 PM, Outlook Hotel
anne.wilson at lasp.colorado.edu
Wed Oct 16 19:04:51 EDT 2013
Our next meeting of the Boulder Earth and Space Science Informatics
Group is next Wednesday, and if you're in Boulder please consider
joining us. Our speaker will be Alex Pletzer from Tech-X on interpolation:
"There is more to conservative interpolation--- interpolating edge and
face centered fields in the geo-sciences"
Interpolation is one of the most widely used postprocessing tasks,
according to a survey of Ultrascale Visualization Climate Data Analysis
Tools (UV-CDAT) users. Most geo-postprocessing tools (UV-CDAT, NCL,
Ferret, etc) support a choice of both bilinear and conservative
regridding with conservative interpolation guaranteeing that the total
amount of "stuff" (energy, water, etc) remains unchanged after
regridding. The SCRIP and ESMF are examples of libraries implementing
these interpolation methods.
We argue that the type of interpolation is dictated by the type of field
and that cell centered fields require conservative interpolation whereas
nodal fields require bilinear (or higher order) interpolation. Moreover,
the wind velocity fields used by finite-volume atmospheric codes, which
are neither cell-centered nor nodal but face-centered (Arakawa D
staggering), require different interpolation formulas. Interpolation
formulas of face-centered and edge-centered (Arakawa C) fields have been
known as Whittney forms since 1957 and are widely used in
electromagnetics. We present interpolation methods new to the
geo-sciences that conserve flux and line integrals for Arakawa D,
respectively Arakawa C, stagggered fields.
This talk should be of interest to anybody in need to regrid velocity
and other vector fields whose components are staggered with respect to
Complete information is available at our web site:
Come on by, hope to see you there!
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