Jeremy:
You
have given a nice, succinct example of the bias that can occur
depending on the time of day that the clock resets. This can
happen at any time, though probably some times have larger bias due to
this than others. Something similar of course happens with Tmin,
esp. if the clock is reset around local sunrise.
I think
putting this output in the SRF file, and at 3 hour intervals is a good
idea, and then users can decide for themselves what matches their obs.
sources best or other needs. It also takes advantage of the
existing output file structure for RegCM. For multi-model
comparisons, esp. in extratropical domains that stretch over several
time zones, it will probably be best to stick to 00 UTC.
I have
the nearly same question as Anji - is the "2-m" temperature
computed relative to the zero-plane displacement level for the
vegetation under consideration? The zero-plane displacement
level is not the top of the vegetation, but it is a function typically
of the vegetation's roughness length.
I must
have lost a factor of 10 somewhere in my estimate of the lowest
level's midpoint - thanks for the correction.
Bill
At 10:42 AM +0100 2005.11.17, Jeremy Pal wrote:
Hi Bill,
If it is OK for others, I agree that we should use 00UTC. But, I
foresee potential problems with this approach. For example, if
you have a day that is very hot followed by a cooler day, you may end
up counting the maximum temperature twice for the hot day depending on
locally what time 00UTC is. A similar scenario could be thought
of for minimum temperature. For this reason, I suggested the
max/min of the SRF output interval, so that the user could decide at
the postprocessing stage what time to use. Anyway, if you think
that these potential problems are negligible, we can use 00UTC.
Regarding the 2m temperature, do you think there is a need to rethink
our approach for computing it in the presence of tall vegetation?
If so, do you have any suggestions?
A small clarification... In the default version, I pretty sure
that the midpoint of the lowest model level generally about 35 to 40
meters.
Thanks for the comments. It is nice to see so much interaction
for so many different RegCNETers!
Jeremy
Wm. J. Gutowski wrote:
Re: [RegCNET] tmax and tmin
Lara:
I'm not
sure that using the lowest ATM level is the best choice, although we
do want an air temperature. What most models that I know about
typically do is use the near-surface air temperature that the
land-surface model determines, perhaps in conjunction with the PBL
model This is the temperature that corresponds to what the
observing stations are measuring. The lowest ATM level may be
many meters above the surface. For example, RegCM's lowest
layer's delta sigma = 0.05 implies a lowest-layer thickness of about
500 m, that the nominal middle of the layer is at about 250
m.
There
may be a further issue here though (and I need help from the ICTP
people on this!): is the near-surface air temperature computed
in RegCM3 at 2 m? I thought some observation stations
used
other heights above the
surface.
Also,
how well do we know that Tmin/Tmax stations adhere to WMO standards?
I know if the U.S. they don't, simply because of the disparate reset
times used. If that is the case elsewhere, then I suggest doing
the reset at a default time of 00 UTC (so that the values are for the
calendar day ending at that time). This could be a parameter
that the user can change in the input files, though that might cause
confusion about what day to associate the values with.
(Arguably, that potential for confusion will always be there relative
to the local clock.)
Bill
At 11:02 AM -0800 05.11.16, Lara Kueppers
wrote:
Jeremy-
A couple of things:
* Mark and I were discussing that it would be best if Tmin and Tmax
were calculated from air temperature (lowest ATM level) so that they
are consistent with the average T values. If you output this in the
SRF file, that's fine, just so it's clear we're talking atmospheric
min and max.
* Also, calculating min and max from 00
to 00 UTC seems the most workable option. Unless there is some
argument for having sub-daily min and max (as opposed to average)
temperature, we'd say limit the file size!
One other thought... Would anyone else find it useful to have the
combined surface albedo values available from BATS? (i.e. the total
vis and ir albedos calculated from veg, soil, snow etc.) This would be
helpful for interpreting seasonal cycle results from land cover change
experiments. Of course this would increase the file size...
Lara
Jeremy Pal wrote:
Hi,
Having it done based on local time may be a bit tricky to code up.
As an alternative, we could consider storing the max/min temperature
and wind for every output interval (e.g. 3 hours). This way, the
user can decide the reset time at the postproc stage... Of course,
this increases the SRF output file size by about 15% as opposed to
just a couple percent.
What do you think of this idea?
Jeremy
Tomá" Halenka wrote:
Dear All,
Not bad hearing Tmax and Tmin will be included properly in new
edition
of RegCM. But I would recommend to use WMO definition and reset
time,
moreover, keep in mind it has to be done in local time as my
opinion.
Best regards,
Tomas
*************************************************
RNDr. Tomas Halenka, CSc.
Charles University in Prague,
Faculty of Mathematics and Physics,
Department of Meteorology and Environment Protection,
V Holesovickach 2, 180 00 Prague 8,
Prague, Czech Republic,
Phone: +420 2 21912514
Fax: +420 2 21912533
E-mail: tomas.halenka@mff.cuni.cz
*************************************************
-----Original Message-----
From: regcnet-bounces@lists.ictp.it
[mailto:regcnet-bounces@lists.ictp.it] On Behalf Of BI
XUNQIANG
Sent: Wednesday, November 16, 2005 9:48 AM
To: Wm. J. Gutowski
Cc: Gao Xuejie; regcnet@lists.ictp.it
Subject: Re: [RegCNET] tmax and tmin
Dear Bill, Lara, and Gao:
In the next public released RegCM3 version, we will add Tmax, Tmin
and vertital velocity (for pressure level) as the standard output.
We will calculated Tmax and Tmin as the way Bill suggested (for
every land surface step, and reset at 00 UTC).
Any other fields are also necessary to be included ?
Thanks and best regards,
On Tue, 15 Nov 2005, Wm. J. Gutowski wrote:
Dear Lara:
I am not the expert on
this, but I am pretty sure that observed
Tmin
and Tmax are obtained primarily from
min/max thermometers, which
record the
highest and lowest temperature attained
since the last time they were
reset.
They are almost always reset every 24
hours, though they don't all get
reset
at the same time. That is,
different stations, even in the same
country (or
in the US, the same state) may reset
their thermometers at different
times of
the day. This can induce a small
bias in one station's climatological
averages compared to what it would get if
it reset at another time.
This is
documented in the literature somewhere,
though I don't have the
reference
myself.
Using the 3-hourly output will tend to reduce the
diurnal
temperature
range you get because that is probably
not sampling the extremes of
the day,
though I have not seen this reduction
tabulated by anyone, and it
probably
depends on location and season.
Including a computation of the true
daily
min/max temperature would be just a few
lines of code, and some of us RegCNETers have undoubtedly done it for
their version of the code - we
really
should have it as part of the standard
model, I think. There would
still be
the question of what time of day to
"reset the thermometer", but in
model
intercomparisons I've been part of, we
typically agree to go from 00
UTC - 00
UTC.
Bill
At 11:32 AM -0800 05.11.14, Lara Kueppers wrote:
Hi-
Awhile back I asked how Tmin and Tmax in the SRF output file were
calculated. Here is Nellie's recent reply, in case anyone else is
interested.:
"Hi Lara,
I just verified this with Bi...Tmin and Tmax are calculated from
the
BATS
output, so if you have the model output
to the SRF file every 3
hours, then
that is what the min and max are
calculated from. Bi thinks this is
a
better way to do it since min and max
temp observations are generally
taken
from 3 or 6 hourly obs. You can
increase the frequency of the srf
output
variables (in the regcm.in file) to see
how much of difference it
would
make in the diurnal temp range.
"
--
~*~*~*~*~*~*~*~*~*~*~*~*~*~*~*~*~*
Lara M. Kueppers, PhD
Postgraduate Researcher
Department of Earth Sciences
University of California, Santa Cruz
1156 High Street
Santa Cruz, CA 95064
USA
831.459.3504 ph
831.459.3074 fax
kueppers@pmc.ucsc.edu
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RegCNET mailing list
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--
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
William J. Gutowski, Jr.
3021 Agronomy Hall
Dept. of Geological and
Atmospheric Sciences
Iowa State University
Dept. of Agronomy
Ames, Iowa 50011-1010
gutowski@iastate.edu
Tel:1-515-294-5632
Fax:1-515-294-2619
http://www.ge-at.iastate.edu/
http://rcmlab.agron.iastate.edu/
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
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~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
~ Dr. Xunqiang Bi
email:bixq@ictp.it ~ ~
Physics of Weather and Climate
Group ~
~ The Abdus Salam
ICTP ~
~ Strada Costiera,
11 ~
~ P.O. BOX 586, 34100 Trieste,
ITALY ~
~ Tel: +39-040-2240302 Fax: +39-040-2240449 ~
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Phone: +39 040 2240579; Fax: +39 040 2240449
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RegCNET mailing list
RegCNET@lists.ictp.it
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--
~*~*~*~*~*~*~*~*~*~*~*~*~*~*~*~*~*
Lara M. Kueppers, PhD
Postgraduate Researcher
Department of Earth Sciences
University of California, Santa Cruz
1156 High Street
Santa Cruz, CA 95064
USA
831.459.3504 ph
831.459.3074 fax
kueppers@pmc.ucsc.edu
_______________________________________________
RegCNET mailing list
RegCNET@lists.ictp.it
https://lists.ictp.it/mailman/listinfo/regcnet
--
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
William J. Gutowski, Jr.
3021 Agronomy Hall
Dept. of Geological and
Atmospheric Sciences
Iowa State University
Dept. of
Agronomy
Ames, Iowa 50011-1010
gutowski@iastate.edu
Tel:1-515-294-5632
Fax:1-515-294-2619
http://www.ge-at.iastate.edu/
http://rcmlab.agron.iastate.edu/
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
--
The Abdus Salam International Centre for Theoretical Physics
Strada Costiera 11; 34100 Trieste, ITALY
Phone: +39 040 2240579; Fax: +39 040
2240449
--
*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*
William J.
Gutowski
3021
Agronomy
Dept. of Geological
and
Atmospheric Sciences
gutowski@iastate.edu
Dept. of Agronomy
Tel:
+1-515-294-5632
Iowa State
University Fax:
+1-515-294-2619
Ames, Iowa
50011-1010
http://www.ge-at.iastate.edu
http://rcmlab.agron.iastate.edu/
*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*-*