AWIPS LAPS runs using NOAAPORT (nationally distributed) and LDAD (locally
distributed) data that has generally been translated into NetCDF on the
AWIPS platform for use by the LAPS ingest processes.
An overall description of raw data. and ingest processes. is in our README file.
The data paths for surface data are specified in 'obs_driver.nl'. There are three separate paths for METAR, LDAD, and Maritime files. Surface observations are now used from a time window between 15 minutes before and 15 minutes after the top of the hour.
In the past there have been some questions about bulls-eyes in various surface analyses, particularly the CAPE field. The CAPE is very sensitive to dewpoint and temperature, so some bulls-eyes are normally to be expected. The key is to look at and assess the dewpoint and temperature inputs to the CAPE. Some problems in the dewpoint/temperature have been related to the spline routine and erroneous observations making it past the QC. We have replaced the spline with a more robust "Bratsethian" style of Barnes successive correction. We are also improving the QC procedures and thresholds. More details are listed below for each AWIPS build.
In terms of the analyses, the IR image data feeds into the cloud analysis as well as the surface temperature analysis. The VIS and 3.9u data (used in clouds and snow cover) is currently being developed over the next few builds (see below).
LAPS Satellite ingest processes the image closest to the top of the hour, up to a range of H-15 to H+15 minutes.
The radar reflectivity data is utilized by the cloud analyses and QPE precipitation analysis.
We are currently utilizing low-level radar reflectivity data (Level-III RPG) for input into LAPS. The strategy is to process low-level reflectivity data in polar form into a NetCDF file that is readable by the LAPS ingest program 'remap_polar_netcdf.exe'. Ideally we prefer full volume (or layer composite) radar data for LAPS, though LAPS can function to a degree with the two-dimensional, single-radar input.
LAPS uses the low-level tilt scanned closest to the top of the hour, up to a range of H-20 to H+20 minutes.
In the future we hope to use multiple radars. Towards this end a mosaicing program is being implemented as part of the LAPS AWIPS suite to combine individual 'vrc' files generated for each radar using 'remap_polar_netcdf.exe' into a composite 'vrc'.
To improve ground clutter rejection, we hope to use either the DHS (Digital Hybrid Scan), or multiple low-level tilts.
In the more distant future, wideband (Level-II) reflectivity and velocity data would be attractive for use in AWIPS/LAPS. The additon of Doppler velocity data would improve the quality of the wind analysis (3-D and surface).
For additional information, see our README file in the section on "deriv.exe". The README document discusses the newest version of helicity, while the paper on the LAPS Wind Analysis mentioned therein discusses an older version.
For OB3 we are changing the LAPS storm motion algorithm to use the Bunkers et. al. method to help ensure consistency with other helicity calculations in AWIPS. This has a better accounting for right-moving storms, especially since we previously had the shear term turned off and were using a simple mean-wind vector.
There are two LI selections on the workstation. LAPS LI is a regular LAPS product (in the LAPS big file). It is computed from a surface parcel taken from the LAPS T and Td sfc analyses. Surface (terrain following) pressure and 500mb temps are also taken from LAPS.
Computed LI is an intrinsic on the fly workstation function that calculates LI from the state LAPS variables.
Updated 7/14/2004