The forecasts this week here in Canberra have been well received by the
public
and can be attributed to helpful guidance from the models. The
rainfall
we got was keenly anticipated from a week prior to occurring
and
the heavy winds of Wednesday were well captured by the models. On
behalf
of this office, many thanks.
It is however, a good time to enquire as to why there remains NO
guidance
at all in this country that focuses on the 'precipitable
water'.
Neither 'Kenny' nor NMOC guidance of any kind [GASP analysis
accepted].
Is there something out there that I'm unaware of? The US
excessive
rainfall policy regularly talks about this variable in their
discussions,
and quite frankly, it is an extremely important element in
forecasting
good rainfall events, be it in a rain band like that which
we
recently had, but also from convective events as well, incl. flash
flooding
etc. I strongly recommend that something be available from LAPS
and
GASP that allows us to see this variable. I would also be
particularly
keen to see what sort of biases these models have in
relation
to the amount of moisture they predict. It could be a helpful
factor
in allowing forecasters to better use the rainfall guidance.
Also, I gave a talk in HO in June highlighting the strong correlation
between
3 hourly temperature and pressure changes in the Meso LAPS
model.
The data I showed was based on manually extracted values over
about
3 weeks. I've continued to do this and now have just over 100 days
worth
of information based on the 12Z run. They continue to strongly
support
the comments that were raised in that talk and I strongly
believe
that would be of some interest to anybody interested in
improving
the MSLP guidance from this product, which is significantly
failing
to capture the local pressure changes across the region of
interest
to us.
The following table lists the time period in which the forecasts were
valid,
the correlation co-efficient between the 3 hourly temperature and
pressure
changes, and the z-score quantifying the strength of the
correlation.
0
to +3 hrs: 15Z-12Z -0.4479 -4.797
+3
to +6 hrs: 18Z-15Z -0.2854 -2.920
+6
to +9 hrs: 21Z-18Z -0.3703 -3.869
+9
to +12 hrs: 00Z-21Z -0.7901 -8.809
+12
to +15 hrs: 03Z-00Z -0.4633 -4.990
+15
to +18 hrs: 06Z-03Z -0.3625 -3.778
+18
to +21 hrs: 09Z-06Z -0.1996 -2.013
+21
to +24 hrs: 12Z-09Z -0.5657 -6.379
+24
to +27 hrs: 15Z-12Z -0.4837 -5.252
+27
to +30 hrs: 18Z-15Z -0.3577 -3.724
+30
to +33 hrs: 21Z-18Z -0.4415 -4.717
+33
to +36 hrs: 00Z-21Z -0.8120 -11.272
With the possible exception of the +18 to +21 hr period in which the
correlation
is significantly different from zero at 4.4% the other
correlations
are extremely significant. Whilst I concede that there is
some
reason for negative correlations between temperatures and
pressures,
eg in the afternoon when rising temps coincide with falling
pressures,
to have EVERY single correlation a negative one to the extent
that
we have here is clearly not correct. The two most excessive
correlations
occur in the 3 hours to 00Z [i.e. +9 to +12 hrs and +33 to
+36
hrs], when the strongest temperature rises occur. During this time
the
model drops the pressure greater on the days in which the
temperature
rise in the most. However in this 3 hour period, strictly as
defined,
the pressure actually rises slightly. It doesn't fall. I would
be
more than happy to have some discussions about why the model does
this.
Local pressure differentials between the ranges and coast are
crucial
to a number of significant weather features across the region.
The
failure of the Meso LAPS to mimic these changes in a significant way
makes
some aspects of this guidance difficult, if not impossible, to
interpret.
Having said that, the main thing I'd like to re-affirm is the
appreciation
of the guidance we've received over the past week or so.
Thanks.
Dave.
Phil Davill
Hi Dave,
Yes there is precip
water available.
With the new 72hr
laps avalaible i have been experimenting with ADDE over some data. By reducing
the domain slightly and being selective in what I get (ie sigma levels,
height, mixing ratio, u, v mslp rain, screen temp
and precip water) the file
size is under 2 meg. Kenny on loading will calculate TD, humiditiy, divergence,
vorticity etc. One advantage of doing it this way is we get ll levels at
or below .85 as opposed to the 5 levels
that are sent to the regions.
A minor modification
to Kenny (version 10.3 I am working on) will display the Laps precip water.
Precip water is also available
on the US (NCEP) model data and possiblly the GASP data that Neil Adams
excellent web based interactive display (I am at home so can not check
that for you).
I assume you could
view the LAPS precip water on goats or using mcidas.
Phil Davill