Page Last updated Thu Apr 8 14:33 BST 2010
IMPORTANT - EUROCONTROL PROPOSALS
The British Gliding Association, along with its airsports colleagues throughout Europe,
are extremely concerned about Eurocontrol’s proposals to standardise the rules of the air throughout Europe.
The proposals call for the removal of decades of appropriate and sensible national modifications and differences
to the ICAO Rules of the Air.
These national differences - as seen for example in the UK ANO and in the series
of exemptions put in place by UK CAA - are appropriate and safe
and to remove them will
seriously damage gliding in particular and airsports in general.
The BGA response is available at the BGA Consulation Page
RASPtable is the simplest interface to all Parameter Maps. See the Introduction for usage.
PLEASE CHECK THE DATE AT THE TOP OF EACH
MAP, AS THE SYSTEM IS SUBJECT TO GLITCHES.
The Status Check indicates if any run error was detected.
Please note that the Location of the LAND-SEA BOUNDARY is approximate.
Interpretation
Frequently Asked Questions (pdf format)
A link to some Webcasts on using RASP.
They have been done by some Paraglider people, and are hosted by Judith Mole.
Many Thanks to you all.
They are of general applicability, and include an excellent introduction to Soundings.
Below are some links to papers by Jean Oberson, a RASP maintainer in Switzerland.
They are, naturally, focussed on his site, but hopefully useful in the UK.
Note also that there are functional differences from RASP-UK,
for example my Sounding Locations on the map are not clickable
- but I do have "Soundings Anywhere"
For more Information about the data in the maps, see DrJack's Website
and especially the Parameter
Descriptions
BlipSpot Maker provides text parameter values for all forecast times at a location.
You can also get a Sounding. You can copy the URL and add to your Favourites list.
Track Average indicates if a task specified by BGA Trigraphs is achievable
Track Start Time
indicates the best time to start a task.
WARNING: it is very slow!
Note: Climb Rates are now in Knots
Wind Tool indicates whether Ridge Sites are expected to work
Experts may prefer a file-list interface to the Forecast Maps
from the Day links below.
Today (12Km)
Monday
Tuesday
Wednesday
Thursday
Friday
Saturday
Sunday
The schedule explains what happens each day,
and indicates when forecasts are updated.
Thanks to:
Overview
These forecasts are intended to help the
meteorology-minded pilot better evaluate soaring conditions. The
maps are particulalry useful to cross-country soaring pilots, since
they allow evaluation of conditions away from the home field.
Utilizing the forecasts can require some self-education (though that
can't be too hard since over 2000 US pilots actively use BLIPMAPs in
the US) as individualized assistance is not provided. At first
glance the website can seem intimidating since so many parameters are
forecast - but most are "supplemental" forecasts to be used as needed
and many users normally look only at the three or four they have found
to be most useful, such as the expected lift strength or the maximum
(dry) thermalling height or cloud potential/height forecasts, looking
at additional parameters only under special conditions.
How are these RASP forecasts produced ?
My traditional RUC and ETA BLIPMAP forecasts are
obtained by post-processing forecast files output from NCEP prognostic
models, so horizontal and vertical resolution is determined by that
used in those models. Here I am instead running a prognostic
model myself, so am able to specify the vertical/horizontal grid
(though of course subject to limits of practicality). A WRF
(Weather Research and Forecasting) model is being initialized and
marched forward in time at 180 second time intervals to produce
forecasts at 3 hr increments. Initial and boundary conditions
come from the larger-scale models run by NCEP, in this case from the
GFS model having a resolution of around 100km. To increase
accuracy, forecasts are produced for three different grids: a
large-domain coarse-mesh grid (36 km), a 12 km grid nested inside it,
and a small-scale fine-mesh 4km grid within that (but only results for
the latter two grids are presented). Since the data needed to
make such runs is available globally, the forecasts can be made for
anywhere in the world.
Notes and Caveats:
() One is not supposed to believe all the details of these
forecasts, particularly since the smallest-scale structure is
constantly
changing yet one a few snapshots at different times are shown.
Rather, one should be looking for patterns.
() Forecasts for points close to the boundary will be less
accurate than for those located nearer the center of the domain, due
to inevitable mis-matchings between the coarse and fine grids.
In particular, predictions of max/min BL vertical velocity are very
noisy and inaccurate near the boundary (particularly where boundary
condition problems exist). To remind users of this, a dotted
line marks the "frame" outside of which coarse-fine boundary
interaction problems are most prevalent.
() The "Explicit CloudWater Cloudbase" estimates are based on
cloud water predicted from internal model equations and problematical
since
there is no simple criterion for differentiating "mist" concentrations
from "cloud" concentrations. The criterion presently used is a
first guess.
() The "Cu Potential" and "Sfc. LCL" predictions are based on a
simple formula which considers
only water vapor at the surface
() This model does not ingest as much observational data as do
the institutional models
such as RUC and ETA, hence some effects are not included.
() The fact that these forecasts are only a snapshot in time of
a fairly noisy field should be particularly emphasized for the 4 km
resolution forecasts, as forecasts for, say, 30 minutes before or
after would look different. At this point it's difficult to
figure how much value they really add anything, but one never knows til
one tries.
() The "Vert. Velocity at 850mb (or 700mb or 500mb)" and
"Vert. Velocity Slice at Vert.Vel.Max" parameters attempt to forecast
mt. wave events, although strong vertical velocities resulting from
deep BL convergence can also be found in the plots. The first
parameter gives a plan view of vertical velocity at the 850mb level, a
height of roughly 1500 m MSL and thus often above the BL top.
The second parameter is a vertical slice taken at a point of maximum
vertical velocity (as found at a height of approximately 1500 m AGL
within a horizontal box which excludes ane outer edge of the domain;
the position of that slice is indicated by a dotted line on the plot
of the first parameter (with left-right on the slice always being
left-right on the plan view). A label above the plots gives the
location and magnitude of the found maximum value. Mt. wave
predictions are best made using resultions no larger than 4km, since a
coarser grid generally does not resolve the waves accurately.
() Time loops are provided to illustrate the variability, and
hence uncertainty,
over a 3 hour period. Unfortunately the color scales are not
identical for all maps
in the loop, but generally they are roughly comparable.