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METEOROLOGY

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Title: METEOROLOGY


1
METEOROLOGY
  • GEL-1370

2
Chapter Nine
  • Weather Forecasting

3
Goal for this Chapter
  • We are going to learn answers to the following
    questions
  • Is weather prediction an exact science? If not,
    why not?
  • What are the different methods of data
    collection?
  • How does weather watch differs from weather
    warning?
  • What is a prog and how does it differ from
    analysis?
  • How are computer-generated weather forecasts
    prepared?
  • What is ensemble forecasting?
  • What are the different methods used to predict
    movement of a surface mid-latitude cyclonic
    storm?

4
Acquisition of weather information
  • Weather forecasting is not an exact science
  • Over 10,000 land-based stations and hundreds of
    ships provide surface weather info 4 times/day
    major airports conditions hourly
  • WMO World Meteorological Organization over 130
    nations responsible for the international
    exchange of weather data
  • NCEPNational Center for Environmental Prediction
    (NCEP) formerly called National Meteorological
    Center, in Camp Springs, MD all meteorological
    data is analyzed, prepare weather maps and charts
    and prediction of weather on a global and
    national scale begins (this transmitted to
    private public agencies)

5
Weather Information forecasting tools
  • Watches, Warning and Advisories NCEP issues
    advisories in the form of watches warnings
    issued to the public of hazardous driving
    conditions caused by wind, dust, fog, snow, sleet
    or freezing rain
  • Watch Indicates that atmospheric conditions
    favor hazardous weather occurring during a
    specified time period
  • Warning Indicates hazardous weather is either
    imminent or actually occurring within the
    specified forecast area
  • Key Warnings Wind advisory, Wind-chill advisory,
    flash-flood watch and warning, severe
    thunderstorm watch and warning, tornado watch and
    warning, hurricane watch and warning, snow
    advisory, Winter storm warning, blizzard warning,
    dense fog advisory

6
Watches, warnings Advisories
  • Wind Advisory Issued when sustained winds reach
    25 to 39 mi/hr or when wind gusts are up to 57
    mi/hr
  • High wind warning Sustained winds are gt40 mi/hr
    or wind gusts gt57 mi/hr
  • Wind-chill advisory When wind-chill temp lt -30
    to -35F
  • Flash-flood watch warning May result in flash
    flooding (warning) is occurring or is imminent
    in the specified area (watch)
  • Severe thunderstorm watch warning winds gt57
    mi/hr and/or hail gt3/4 inch diameter have been
    visually sighted or indicated by radar

7
Watches, warnings advisories contd.
  • Tornado watch warning May develop has been
    spotted either visually or by radar take shelter
    immediately
  • Snow advisory Expect Snowfall of 2 inch or more
    in 12 hours or 3 inch or more in 24 hrs expected
  • Winter storm warning (or heavy snow warning)
    Expect Snowfall of 4 inch or more in 12 hours or
    6 inch or more in 24 hrs expected
  • Blizzard warning When falling or blowing snow
    winds of gt35 mi/hr restricts visibility to lt1/4
    mile
  • Dense fog advisory visibility lt ¼ mile
  • Storm warning Winds gt 54 mi/hr expected
  • Hurricane watch and warning When a tropical
    storm or hurricane becomes a threat to a coastal
    area when it appears that the storm will strike
    an area within 24 hrs with wind speeds gt 74 mi/hr

8
Flags indicating advisories and warnings in
maritime areas
9
Computer and Weather Forecasting Numerical
weather prediction
  • Analysis The drawing interpretation of the
    pattern of various weather elements on a surface
    or upper-air chart
  • Numerical weather prediction Daily forecasting
    of weather based upon the solutions of
    mathematical equations by high-speed computers
  • Atmospheric models Simulation of the
    atmospheres behavior by mathematical equations
    or by physical models
  • Method of solution dozens of equations describe
    how atmospheric parameters (temp, pressure,
    humidity, wind speed direction) change with
    time ---each equation is solved a future Dt for
    a large number of locations grid points ---
    Each equation is solved for many (50) levels in
    the atmosphere calculated values are put back in
    to those equations and calculated for the next
    interval of time and so on for 12, 24, 36, 48,
    120 hours so on.

10
Computer Weather forecasting contd.
  • Prognostic Chart (Prog) A chart showing expected
    or forecasted atmospheric conditions (pressure
    patterns, frontal positions, and so on)
    forecasters use prog as a guide to predict the
    weather
  • Variability in weather prediction Variety of
    models, each produce slightly different
    interpretation of the weather mainly due to the
    way the models are used, what model is used,
    distance of grid points, etc. Some models are
    better than others for a specific task (such as
    predicting the position of the trough on
    upper-level chart, position of surface lows, etc)

11
Why sometimes forecasts dont work??
  • Factors that affect the prediction of weather
    (such as surface temp, winds, precipitation)
    forecasts
  • 1) Each models idealize the atmosphere and the
    assumptions made about the atmosphere may be on
    target on some times, but not all the times
  • 2) Many models are not global in their coverage
    and thus, the models assumed boundaries could
    lead to errors (e.g., air masses entering from
    western Pacific in to North America, if the
    boundary is set as the west coast not including
    the western Pacific) global model would involve
    longer computation time
  • 3) Sparness of data Data from oceans and high
    latitudes are sparse data from satellites have
    helped computers forecast is as good as the
    data fed in to it

12
Why sometimes forecasts dont work?? contd.
  • 4) Inadequate representation of many pertinent
    processes (e.g., interactions of water, ice
    local terrain on weather systems, such as
    radiation budget locally, etc.)
  • Some models take large geographic features
    (oceans, mountain chains) neglecting small scale
    features (hills and lakes) and could have a
    marked influence on local weather
  • 5) Inherent chaotic behavior within the
    atmosphere Several small, unpredictable
    atmospheric fluctuations and disturbances (and
    the uncertainties) get amplified with time in
    projecting the weather farther into the future

13
500-mb progs for 7 PM EST, May 4, 1999 48 hrs
in to the future Prog (a) MRF Model Prog (b)
ETA Model solid lines height contours 552
5520 m
14
Tools for Forecasting the Weather
  • High-speed data modeling systems are used
  • AWIPS (Advanced Weather Interactive Processing
    System) processes information received from the
    Doppler radar system and the Automated Surface
    Observing System (ASOS) operated in airports
    ASOS systems provide continuous information on
    wind, temp, pressure, cloud-base height, runway
    visibility
  • Soundings A two-dimensional vertical profile of
    temperature, dew point winds
  • Several meteorological indexes can aid in
    determining the likelihood of thunderstorms,
    tornadoes hail

15
The AWIPS work station provides various weather
maps
16
Doppler Radar data during a severe hailstorm in
Orlando, FL 100 probability that thunderstorm
was producing hail algorithm estimated hail size
gt 3
17
Satellites Weather Forecasting
  • Satellites provide photographs of areas where
    there are no ground-based observations
  • Geostationary Satellites (Geosynchronous
    satellites) Orbit the equator at the same rate
    as the earth spins (remains at 36,000 km above a
    fixed spot on earths surface) allows continuous
    monitoring of a specific region
  • Pictures received from Geostationary satellites
    to determine the cloud movement, dissipation, or
    development associated with weather fronts
    storms --- useful to forecast the progress of
    large weather systems
  • Polar-orbiting satellites Pass over the north
    and south polar regions on each revolution
    provide sharp pictures in polar regions circle
    the earth at 850 km above the earth provides
    detailed photographic information about violent
    storms cloud systems

18
Geostationary satellite monitors one area
constantly, as it remains stationary with respect
to an observer on earths surface
19
Polar Orbiting satellites scan from north to
south
20
Satellites contd.
  • Satellites use radiometers to observe clouds both
    day night (by detecting radiation from top of
    the clouds)
  • Imager Advanced radiometer that satellite
    pictures with much better resolution
  • Sounder Advanced radiometer that provides a more
    accurate profile of temp, moisture at different
    levels in the atmosphere
  • Infrared satellite picture can distinguish warm,
    low clouds from cold, high clouds (warm objects
    radiate more energy than cold objects)

21
Infrared satellite picture can distinguish warm,
low (Gray) clouds from cold, high (white) clouds
22
A visible image (left) and an infrared image
(right) of the eastern Pacific taken at the same
time
23
Satellites contd.
  • Clouds appear white in the visible image in the
    IR image, clouds appear to have many shades of
    gray
  • Along the elongated band of clouds associated
    with the occluded front, the clouds appear white
    and bright in both pictures, indicating thick
    heavy clouds
  • Time-series photographs provide info on the
    movement of the clouds and hence are useful to
    predict arrival of clouds and storms and the
    passage of weather fronts
  • Other Forecasting Methods
  • Persistent Forecast A prediction that future
    weather will be the same as present weather
  • Steady-state or trend method Surface weather
    systems tend to move in the same direction and at
    the same speed as they have been moving

24
Other forecasting methods contd.
  • Nowcasting Extension of trend method from
    minutes to a few hours
  • Analog Method Existing features on a weather
    chart may strongly resemble features that
    produced certain weather conditions
  • Weather types can be used to long-range weather
    forecasting do not adequately predict specific
    weather elements
  • Ensemble forecasting A technique based on
    running several forecast models (or different
    versions of a single model), each beginning with
    slightly different weather info to reflect errors
    in the measurements agreement forecasters can
    place a high degree of confidence in the
    forecast low degree of confidence means that the
    models do not agree

25
Forecasting contd.
  • Climatological Forecast Forecast based on the
    climatology of a particular region e.g., in LA,
    rainfall amounts more than a trace occur once in
    90 days (1 of the time) we can predict with
    99 confidence of what can happen!
  • What does it mean 70 chance of rainfall?
  • 60 of the forecast area, it will rain??
  • 60 chance it will rain within the forecast
    area??
  • 60 chance that any random place in the forecast
    area will receive measurable rainfall

26
Forecasting words used by the National Weather
Service (precipitation gt 0.01)
probability of preci. Forecast wording for steady precipi. Forecast wording for showery precipi.
20 Slight chance of precipitation Widely scattered showers
30 to 50 Chance of precipitation Scattered showers
60 to 70 Precipitation likely Numerous showers
gt80 Precipitation, rain, snow Showers
  • .

27
Probability of a white christmas one inch or
more snow on the ground (30 yr average)
28
Accuracy and skill in weather forecasting
  • Forecasts made for 12-24 hrs are usually accurate
  • 1-3 day forecasts are reasonably good not
    perfect better than 50
  • With longer time, the accuracy decreases and gt7
    days, accuracy falls off rapidly
  • The forecast must be better than current weather
    or the normal (climatology) weather in LA
    example
  • Teleconnection prediction Warming of the
    equatorial tropical Pacific affects weather in
    different regions of the world the interactions,
    where a warmer tropical Pacific can influence
    rainfall in CA are called teleconnections
    aids to predict seasonal changes, but not diurnal

29
Predicting weather from local signs
  • A halo around the moon portends rain Why?
  • Halo is caused by by the bending of light as it
    passes through ice crystals and that ice
    crystals-type clouds (cirrostratus) are often the
    forerunners of an approaching storm
  • Few forecasting rules that may be applied when
    making a short-range local weather forecast
  • Observation Indication Local weather forecast
  • Surface winds from Possible cool Possible
  • S or SW clouds front thunder- showers
  • Building to the west storms approaching possibly,
  • Warm (hot) humid from the west turning cooler
  • windy

30
Forecasting from weather signs
Observation Indication Local weather forecast
Winternight Clear, relatively calm with low humidity Rapid radiational cooling A very cold night
If clear, relatively calm, low humidity, snow on the ground Rapid radiational cooling A very cold night
Cloudy, relatively calm with low humidity Clouds will absorb and radiate IR to surface Not as cold when the sky is clear
Summer night Clear, hot, humid Strong absorption/emission of IR High minimum temp
  • .

31
Contd.
Observation Indication Local weather forecast
Clear and relatively dry More rapid radiational cooling Lower min temp
If surface winds are from N and become NE, then E, then SE Surface high pressure area moving to E low pressure approaching from W Increasing clouds with the possibility of precipitation within 24 hours
If surface winds are from NE then N, then NW Surface low pressure area is moving to the east, surface high press. Approaching from W Possible showers or thunderstorms with gusty winds
Afternoon cumulus clouds with flat bases, and tops at just about the same level Stable layer above the clouds Partly cloud, with no precipitation

32
Weather forecasting using surface charts
  • Thumb Rules for forecasting
  • 1) Storms fronts tend to move in the same
    direction and speed during the previous 6 hrs,
    over a short-time intervals
  • 2) Lows tend to move in a direction that
    parallels the isobars in the warm air ahead of
    the cold front
  • 3) Lows tend to move toward the region of
    greatest surface pressure drop, whereas highs
    tend to move toward the region of greatest
    surface pressure rise
  • 4) Surface pressure systems tend to move in the
    same direction as the wind at 500 mb level. Speed
    at the surface ½ the speed at aloft

33
Forecast example
  • Projection of pressure systems, fronts and
    current weather in to the future by assuming
    steady-state conditions (12- 24 hours projection)
  • The storm center over the Central Plains and
    should move northeast the 500-mb chart suggests
    that the surface low should move northeast at a
    speed of 25 knots
  • Six Cities
  • Augusta (GA), Washington D.C., Chicago, Memphis,
    Dallas, and Denver

34
Surface weather map for 600 AM Tuesday. Dashed
lines positions of weather features 6 hrs ago
shaded green precipitation
35
500-mb chart at the same time L position of the
surface low
36
Weather Forecast
  • Augusta, GA cP associated with a high pressure
    center brought freezing temp and fair weather
    southerly winds on the western side bring warmer
    moist air clear and cold in the morning,
    increasing high clouds, wind direction will be
    light barometric pressure falling slowly
  • -Reality fog was found --- temp of the ground
    was not considered warm, moist air over the cold
    surface --- fog
  • Washington D.C. Storm approaches from the west
    slowly increasing cloudiness

37
Weather prediction contd.
38
Weather prediction contd.
  • Sleet was found not predicted Why??
    Intensification of the storm influx of warmer
    air from the ocean slowly raised the surface temp
    and the sleet soon became rain
  • Chicago Major snowstorm total snowfall is 12
    inches actual snowfall is 13 inch problem
    storm system slowed as it became occluded
  • Memphis, TN Predicted thunderstorm did not
    materialize winds were not strong enough to mix
    the cold, moist air that had settled in the
    valleys with the warm air above

39
Weather prediction contd.
  • Dallas Gulf of Mexico effect
  • Denver Rocky mountain effect
  • Problems associated with the prediction

40
Surface weather map for 600 AM wednesday
41
Summary Chapter -9
  • Warning and Watch
  • Problem with modern day weather prediction
  • Prog, numerical weather prediction
  • Geosynchronous satellites
  • IR images vs visible images
  • Persistent forecast, Steady-state forecast,
    nowcasting, analogue weather prediction
  • Ensemble weather forecasting probability
    forecasting
  • Problems associated with forecasting
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