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Pat, $GEMPAKHOME/source/gemlib/dv/dvpvor.f: C* DV_PVOR * C* * C* This subroutine computes the potential vorticity in a layer from * C* scalar (thermal and pressure) and vector (wind) fields: * C* * C* PVOR ( s, V ) = - GRAVTY * AVOR ( VLAV (V) ) * LDF ( CTA ) / * C* ( 100 * LDF ( PRES ) ) * C* * C* Where: 100 converts millibars to Pascals * C* CTA can be THTA, THTE, or THES * C* * C* PVOR works on a layer in THTA or PRES coordinates. In the case of * C* PRES, the vorticity of the layer averaged wind is corrected by * C* the addition of ( k cross partial V w.r.t. CTA ) dot grad (CTA). * C* PVOR generates a scalar grid. Steve Chiswell Unidata User Support >From: address@hidden >Organization: UCAR/Unidata >Keywords: 200010101815.e9AIFJ429846 >Steve: > >I guess what I'm asking is: Is PVOR still formulated as the k hat component >of the full equation? > >I was told that by using PVOR(THES,GEO) that this got me an EPV >of the full 3-d form > > EPV = -eta dot del(Theta_e) > >where eta is the total vorticity, and the del is a 3-d operator. > >Nowhere in my reading of the documentation does it say this. > >Has there been a contribution, perhaps that does this? > >Thanks. > >Pat > >> >> >From: address@hidden >> >Organization: UCAR/Unidata >> >Keywords: 200010091702.e99H2b428162 >> >> > >> >Hello. >> > >> >I am told that by using PVOR(THES, GEO) that this now yields a 3-d >> >value for EPV. Is this so? >> > >> >We are running GEMPAK5.4, patch level 14. >> > >> >Thanks. >> > >> >Pat >> >-- >> >======================================================================= >> >Dr. Patrick S. Market Phone: (573) 882 - 1496 >> >University of Missouri-Columbia Lab: (573) 882 - 6372 >> >Soil and Atmospheric Sciences Fax: (573) 884 - 5133 >> >203 Gentry Hall e-mail: address@hidden >> >Columbia, MO 65211 Web: http://web.missouri.edu/~marketp >> >======================================================================= >> > >> >> >> Patrick, >> >> As defined in the GEMPAK User Guide under GPARM, PVOR() is a layer quantity. >> If you are looking at a grid cross section in gdcross, then the layer >> quantities are computed automatically: >> GVCORD = pres >> GFUNC = pvor(thes,geo) >> >> If you are using a plan view such as with gdcntr, then glevel should >> represent the layer over which you want the calculation to occur. >> >> Steve Chiswell >> **************************************************************************** >> Unidata User Support UCAR Unidata Program >> (303)497-8644 P.O. Box 3000 >> address@hidden Boulder, CO 80307 >> ---------------------------------------------------------------------------- >> Unidata WWW Service http://www.unidata.ucar.edu/ >> **************************************************************************** >> > > >-- >======================================================================= >Dr. Patrick S. Market Phone: (573) 882 - 1496 >University of Missouri-Columbia Lab: (573) 882 - 6372 >Soil and Atmospheric Sciences Fax: (573) 884 - 5133 >203 Gentry Hall e-mail: address@hidden >Columbia, MO 65211 Web: http://web.missouri.edu/~marketp >======================================================================= >