


Hurricane Jeanne
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Weather stations |
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http://ww2010.atmos.uiuc.edu/(Gh)/guides/maps/sfcobs/home.rxml
http://www.hpc.ncep.noaa.gov/html/stationplot.shtml
For wind speed:
1knot = 1.9km/h (so essentially double to get to km/h)
For temperature (Tf to Tc):
Tc = (5/9)*(Tf-32)
eg. 98.6 degrees F --> degrees Celsius: (98.6-32)*5/9) = 37 degrees Celsius.

Mount Everest has been shown to be 29,028 feet high. The summit of Mount Everest has an average pressure around 300 mb. This picture shows Hillary's camp set at about 20 000 feet looking up to the summit.
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What to look at when making a forecast |
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A. Synoptic chart
Pressure systems and their related weather conditions (synoptic types)
Isobars (wind speed and direction)
Station data
Check the upper air situation to gauge the intensity of the systems
When forecasting on a station scale you need to know topography and what effect this may have on the local weather eg. the influence of a water mass, temperature drop with altitude (especially if wind is blowing), modified wind flow and speed.
The characteristics of a system will be different in different seasons.
B. Satellite photo
Clouds and temperature
C. Radar
1. For short time scale forecast (0.5 – 1.5 hours); precipitation
Example
1: Reading the synoptic map
What
sort of weather would you expect in the following places on this day
based on the 06Z (08:00 am SAST) synoptic map? Please give estimates
of
1. wind direction and speed
2. maximum temperature
3. relative humidity
4. cloud cover
This
is low-tech using blunt tools, so don't panic, just try and give a
rough estimate of the weather.....
Cape Town
Bloemfontein
Durban
What
was observed (lets use the METAR code)?
METAR
is a METerological Aerodrome Report, required for landing and taking
off of all commercial airlines
The
latest METARS are posted at: http://weather.noaa.gov/mgetmetar.php
Useful interpretation site: http://weather.gladstonefamily.net/site/FACT
The code is: SSSS DDHHMM Z DDVVVKT cloud TT/TD Q PPPP, where
SSSS = the four letter station identity
DD = day of month
HH = 24-hour
MM = minute
DD = wind bearing (tens of degrees)
VVV = wind speed (in knots)
TT = air temperature
TD = dew point
PPPP = air pressure in hPa or mb
CAVOK = clouds and visibility OK (for aviation)
The
METARs for the above synoptic state were:
Cape Town: FACT 071230Z 18004KT CAVOK 20/11 Q1023
Bloemfontein: FABL 071200Z 27006KT 250V310 CAVOK 24/M02 Q1029
Variable wind direction betw 250 and 310 deg; M=minus
Durban: FADN 071230Z 13006KT 9999 FEW015 21/13 Q1029
9999 - visibility >er 9999 meters; FEW015 - Few clouds at 1500 feet.
Other examples of METARs:
METAR
FADN 130430Z 29003KT 9000 SKC 11/08 Q1024
NOSIG=
Explanation:
Location
Durban(FADN), 13th at 04:30 utc, wind direction 290 degrees at 3
knots,
visibly 9000m, clear skies(SKC), temperature 11 degrees /
dewpoint temperature
8 degrees, QNH 1024 Hpa(mB), no significant
change expected(NOSIG),
end of bulletin(=).
METAR
FAJS 170530Z 35007KT 0500 R/21R0150 R/03L0300V0700 FG
OVC000 FEW///CB
T07/07 Q1025 FM0535 TL0615 0100 RMK
THUNDER=
Explanation:
Location
Johannesburg Int. Airport(FAJS), 17th at 05:30 utc, wind 350
degrees
at 7 knots, visibility 500m, designator on runway 21 right
- visibility 150m, at
designator 03 left visibility 300m with a
tendency to increase to 700m, fog,
overcast cloud at 0ft, few
Cumulonimbus cloud of which the observer is unable
to determine
the cloud base(///), temperature 7 degrees / dewpoint temperature
7
degrees, QNH 1025 Hpa. Here the observation ends and the trend
forecast
begins, from 05:35 until 06:15 the visibility is expected
to be 100m. RMK signifies
the end of the trend forecast and the
observer remarks that thunder was heard
at the time of
observation.
What is significant about the remark in this case
is, if the observer had heard
no thunder during the time of
observation, the term FEW///CB would not have
been included
in the METAR.
Click here
(SAWS) if you want more on METARS.... and TAFs (Terminal Aerodrome
Forecasts)
Example 2: Using GCM forecast maps
Discuss the sort of weather expected in the following regions based on these maps...
Western Cape
Eastern Cape
Limpopo Province

What can we expect? (Subjective is good - remember man-machine mix)
First what are the main features on these maps:
The season is winter (see table below for temperature definitions)
Well-developed mid-latitude cyclone at the surface (40S 10E), close enough to Cape Town for impact! Pressure gradients are tight so wind should be strong
The 500hPa heights are not showing a strong trough, the system is driven largely at the surface. This may limit the amount of snow on the mountains
Winds are off-shore along the east coast, but backward trajectories indicate that this is not a true berg-wind situation. The air may be dry but not hot.
Further north the pressure gradients are slack in the anticyclone belt, not much happening there.
1)
Western Cape: Cloudy and cold with rain, wind strong northwesterly
(possibly gale-force).
2) Eastern
Cape: Partly cloudy and mild with showers later in the west as front
moves in. Wind strong north-westerly to westerly
3)
Limpopo: Find and mild
Note: temperature forecasts are just a guess at this point, we obviously need observations and 24-hour changes to do a good job of it, but returning to climatology and the basic elements of the synoptic situation we can give a reasonable estimate. Temperature categories as used operationally by the SA Weather Service are given in the table below:
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Maximum temperature |
Summer |
Winter |
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Very Cold |
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< 7 |
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Cold |
< 15 |
7 - 12 |
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Cool |
15 - 20 |
12 - 17 |
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Mild |
20 - 25 |
17 - 22 |
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Warm |
25 - 30 |
22 - 27 |
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Hot |
30 - 35 |
> 27 |
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Very Hot |
> 35 |
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Some more charts
Your weekend weather according to EGS_312!!
For Saturday, Sunday and Monday give a forecast for the following regions for 6am and 2pm.
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Temp |
Pressure |
Wind speed |
Wind dir. |
Cloud cover |
Precip |
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Durban |
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Cape Town |
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Johannesburg |
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PE |
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UCT |
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Weather Forecasting - Summary |
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Need to know 2 things:
1. The state of the atmosphere
2. The laws that govern that state
A. Forecast methods:
Objective method – computers do the work numerically
Subjective method – Synoptic archetypes, extrapolation/interpolation, analogue systems, climatology, local weather knowledge
B. Observations
Measurements
Class 1 - in situ measurements, thermometer, barometer, anomometer etc
Class 2 - remote using EM, eg radar, aircraft and satellite
Class 3 – wind velocities (balloon tracking, satellite cloud tracking and scatterometer)
Error
Natural error – instrument error and error of representativeness
Gross error – calibration, telecommunication, coding
Data observation
Surface -land synop, marine and satellite
Radiosondes – vertical profile; wind speed and dir., temperature and dew point temperature, humidity
Aircraft – wind and temperature
Satellites – wind, temperature
C. Check data quality
Objectively – filtering rules written to check data
Subjectively – Eyeballing the data
D. Dissemination of data to
organizations using it
World Meteorological Organization
World Weather Watch
E. Analysis
Subjective – synoptic charts, weather stations, etc...
Objective –
|-----------------------------------Initialization-----------------------------------|
Previous forecast --> + checked observed data --> analysis increment --> new forecast --> + obs data --> analysis increment --> new forecast etc...
Observations at 00Z and 12Z for initialization
F. Forecast clients
Aviation, shipping, agriculture, government, commercial, public
Finally:
Forecasting combines objective numerical forecasts with subjective human experience to get a best forecast.