[Date Prev][Date Next][Thread Prev][Thread Next][Date Index][Thread Index]
[IDV #WYC-198714]: IDV 4.1u1: Vertical cross section plots conforming to variable surface elevation
- Subject: [IDV #WYC-198714]: IDV 4.1u1: Vertical cross section plots conforming to variable surface elevation
- Date: Wed, 04 Dec 2013 11:55:18 -0700
>
> On Dec 2, 2013, at 2:14 PM, Unidata IDV Support
> <address@hidden<mailto:address@hidden>>
> wrote:
>
> IDV support,
>
> I’m using IDV v4.1u1 (latest nightly build) to plot vertical cross sections
> of WRF-ARW model output. This output is on sigma coordinate surface (and
> hence terrain following at the surface), but when I plot data (such as
> vertical velocity, which is defined on grid surfaces that include the terrain
> surface itself), the bottom edge of the plot does not conform to the
> superimposed terrain elevation plot—rather, it seems to cut off at a fixed
> elevation, around 190 meters (which intersects the terrain profile).
>
> Dave,
> I discussed your model result with one WRF support people at MMM, she said
> the gap between data and the terrain is normal. If you want to make the gap
> smaller, you can change the sigma level to 1, 0.997, .... instead of 1,
> 0.993..., some software does interpolate the data to make it looks better. I
> am not sure if this is the case for the ncl.
>
> Yuan,
>
> Since the plot I'm talking about is a vertical cross section, it presumably
> uses data from "All levels", not any particular sigma level, and that's what
> I specify when I create the plot. Specifying a particular level doesn't
> change anything, as far as I can tell. (The IDV is smart enough to ignore the
> inconsistency between specifying a vertical cross section plot and a
> particular level at the same time.)
>
> Using data from all sigma levels should include data from the lowest sigma
> level (in the case of vertical velocity, that's sigma = 1, which is the
> terrain surface itself). Hence, ideally the bottom edge of the vertical cross
> section plot should conform to the terrain profile and not intersect it,
> assuming that the terrain profile and the vertical cross section are plotted
> on the same vertical scale.
>
> However, although the bottom of my vertical cross section plot comes close to
> conforming to the terrain profile at the highest terrain elevations, it
> doesn't come very close where the terrain elevation is lower. (The bottom
> edge of the plot is not smooth but seems to outline the model's rectangular
> grid cells, at least where the plot skirts the highest terrain elevations.)
>
> One question is, what does the IDV use to determine the vertical coordinate
> of each grid point in the field that it is contouring? If it is the value of
> sigma (between 0 and 1, with 1 at the bottom and 0 at the top of the domain),
> then where does sigma = 1 begin on the plot's vertical scale? (Should it be
> same as z = 0 for the topographic profile?) And why wouldn't the bottom edge
> of the plot be a straight, horizontal line (corresponding to the same value
> of sigma)? (In my plot, the bottom of the vertical cross section is mostly a
> straight, horizontal line, but it indents upward in distinct, rectangular
> steps to stay above the highest terrain.)
>
Dave,
In the IDV, the sigma levels are transferred to pressure coordinate. I
have the feeling that only base state pressure being counted in the transfer
process. This might be the reason for the gap.
By the way, I will be in the AGU next week. Likely, I will spend a lot of
time in the UCAR booth and I will like to meet you if you are around. Send me
email offline.
Yuan
> On the other hand, if the IDV uses height above sea level (rather than sigma)
> of each grid point in the cross section to plot contours, then why doesn't
> the bottom of the contour plot more closely conform to the terrain profile,
> which is also based on height above sea level? (To use height above sea level
> of each grid point in the cross section, the IDV would have to be smart
> enough to construct that height by adding the perturbation geopotential to
> the base-state geopotential, which are the only two pieces of information the
> height of 3-D grid points in the WRF-ARW model output file, but I'd be
> surprised if it would do that. The same issue would arise if it used pressure
> as its "height" information.)
>
> I've attached a screen shot to show the discrepancy--I don't think I did that
> last time. The white line is a terrain profile aligned with the vertical
> cross section of vertical velocity (a color-fill contour plot). The lowest
> grid level for vertical velocity is the terrain surface.
>
> -- Dave
>
> [cid:663FABB8-AFB3-4A31-B9F1-420D9A0BC092]
>
>
> Yuan
>
> Is there a way to get the bottom of the plot to conform to the underlying
> terrain? (I know this is possible using NCAR graphics, for example). And what
> determines the apparent elevation of the bottom of the plot?
>
> I’ve included an IDV bundle to illustrate the point. It shows (among other
> things) a vertical cross section plot of vertical velocity with horizontal
> wind speed contours superimposed, along with a terrain profile. The data come
> from a NetCDF file located at
> http:://virga.sfsu.edu/data/wrf/<http://virga.sfsu.edu/data/wrf/><http://virga.sfsu.edu/data/wrf/>wrfout_2013-11-21_12_GFS_CenCal_BayArea_EastBay.1.nc
>
> — Dave
>
>
> ****************************************************************
> * | __ __ \|/ *
> * Dr. Dave Dempsey | ) ^ /|| ||\ --0-- *
> * Dept. of Earth & Climate Sciences |) ) ^ / ||_|| \ /|\ *
> * San Francisco State University | ) ) / | _ | \ *
> * 1600 Holloway Ave. |) )/ || || \ *
> * San Francisco, CA 94132 | ) ) ||_|| \ *
> * |) ) ) | _ | \ *
> * Phone: (415) 338-7716 | ) ) || || \ *
> * FAX: (415) 338-7705 |) ) )~~~~~~~~~~~~~~~*
> * Email: address@hidden<mailto:address@hidden><mailto:address@hidden>
> | ) ) ) ~ ~ ~ ~ *
> * |) ) ) ) ~ ~ ~ *
> ****************************************************************
>
>
>
>
>
> Ticket Details
> ===================
> Ticket ID: WYC-198714
> Department: Support IDV
> Priority: High
> Status: Closed
>
>
>
> ***************************************************************
> * Dr. Dave Dempsey | ^ ___ \|/
> *
> * Dept. of Earth & Climate Sciences | ) ^ /||_||\ --0-- *
> * San Francisco State University | ) ) / ||_|| \ /|\ *
> * 1600 Holloway Ave. | ) ) / ||_|| \
> *
> * San Francisco, CA 94132 | ) ) / ||_|| \ ^ *
> * | ) ) )
> ||_|| \ *
> * Phone: (415) 338-7716 | ) ) )~||~||~~~~ \~~*
> * FAX: (415) 338-7705 | ) ) ) ) ~ ~ ~ ~ ~ ~*
> * Email: address@hidden<mailto:address@hidden> | ) ) ) )
> ) ~ ~ ~ ~ *
> ***************************************************************
>
>
>
>
>
>
Ticket Details
===================
Ticket ID: WYC-198714
Department: Support IDV
Priority: High
Status: Open