From Wikipedia, the free encyclopedia
Weather forecasting is the application of science and technology to predict the conditions of the
atmosphere for a given location and time. People have attempted to predict the
weather informally for
millennia and formally since the
19th century. Weather forecasts are made by collecting quantitative
data about the current state of the atmosphere at a given place and using
meteorology to project how the atmosphere will change.
Once calculated by hand based mainly upon changes in
barometric pressure, current weather conditions, and sky condition or
cloud cover, weather forecasting now relies on
computer-based models that take many atmospheric factors into account.
Human input is still required to pick the best possible forecast model
to base the forecast upon, which involves pattern recognition skills,
teleconnections, knowledge of model performance, and knowledge of model biases. The inaccuracy of forecasting is due to the
chaotic
nature of the atmosphere, the massive computational power required to
solve the equations that describe the atmosphere, the error involved in
measuring the initial conditions, and an incomplete understanding of
atmospheric processes. Hence, forecasts become less accurate as the
difference between current time and the time for which the forecast is
being made (the
range of the forecast) increases. The use of ensembles and model consensus help narrow the error and pick the most likely outcome.
There are a variety of end uses to weather forecasts. Weather
warnings are important forecasts because they are used to protect life
and property. Forecasts based on
temperature and
precipitation are important to
agriculture,
and therefore to traders within commodity markets. Temperature
forecasts are used by utility companies to estimate demand over coming
days. On an everyday basis, people use weather forecasts to determine
what to wear on a given day. Since outdoor activities are severely
curtailed by heavy rain, snow and
wind chill,
forecasts can be used to plan activities around these events, and to
plan ahead and survive them. In 2009, the US spent $5.1 billion on
weather forecasting.
History
Ancient forecasting
For millennia people have tried to forecast the weather. In 650 BC, the
Babylonians predicted the weather from cloud patterns as well as
astrology. In about 350 BC,
Aristotle described weather patterns in
Meteorologica. Later,
Theophrastus compiled a book on weather forecasting, called the
Book of Signs.
Chinese weather prediction lore extends at least as far back as 300 BC, which was also around the same time ancient
Indian astronomers developed weather-prediction methods.
In New Testament times, Christ himself referred to deciphering and
understanding local weather patterns, by saying, "When evening comes,
you say, 'It will be fair weather, for the sky is red', and in the
morning, 'Today it will be stormy, for the sky is red and overcast.' You
know how to interpret the appearance of the sky, but you cannot
interpret the signs of the times."
In 904 AD,
Ibn Wahshiyya's
Nabatean Agriculture, translated into Arabic from an earlier
Aramaic work,
discussed the weather forecasting of atmospheric changes and signs from
the planetary astral alterations; signs of rain based on observation of
the
lunar phases; and weather forecasts based on the movement of winds.
Ancient weather forecasting methods usually relied on observed
patterns of events, also termed pattern recognition. For example, it
might be observed that if the sunset was particularly red, the following
day often brought fair weather. This experience accumulated over the
generations to produce
weather lore. However, not all of these predictions prove reliable, and many of them have since been found not to stand up to rigorous statistical testing.
Modern methods
The Royal Charter sank in an 1859 storm, stimulating the establishment of modern weather forecasting.
It was not until the invention of the
electric telegraph in 1835 that the modern age of weather forecasting began.
Before that, the fastest that distant weather reports could travel was
around 100 miles per day (160 km/d), but was more typically 40–75 miles
per day (60–120 km/day) (whether by land or by sea). By the late 1840s, the telegraph allowed reports of weather conditions from a wide area to be received almost instantaneously, allowing forecasts to be made from knowledge of weather conditions further
upwind.
The two men credited with the birth of forecasting as a science were an officer of the
Royal Navy Francis Beaufort and his
protégé Robert FitzRoy. Both were influential men in
British
naval and governmental circles, and though ridiculed in the press at
the time, their work gained scientific credence, was accepted by the
Royal Navy, and formed the basis for all of today's weather forecasting knowledge.
Beaufort developed the
Wind Force Scale
and Weather Notation coding, which he was to use in his journals for
the remainder of his life. He also promoted the development of reliable
tide tables around British shores, and with his friend
William Whewell, expanded weather record-keeping at 200 British
Coast guard stations.
Robert FitzRoy was appointed in 1854 as chief of a new department within the
Board of Trade to deal with the collection of weather data at sea as a service to
mariners. This was the forerunner of the modern
Meteorological Office.
All ship captains were tasked with collating data on the weather and
computing it, with the use of tested instruments that were loaned for
this purpose.
Weather map of Europe, December 10, 1887.
A storm in 1859 that caused the loss of the
Royal Charter inspired FitzRoy to develop charts to allow predictions to be made, which he called
"forecasting the weather", thus coining the term "weather forecast". Fifteen land stations were established to use the
telegraph
to transmit to him daily reports of weather at set times leading to the
first gale warning service. His warning service for shipping was
initiated in February 1861, with the use of
telegraph communications. The first daily weather forecasts were published in
The Times in 1861. In the following year a system was introduced of hoisting storm warning cones at the principal ports when a gale was expected. The
"Weather Book" which FitzRoy published in 1863 was far in advance of the scientific opinion of the time.
As the electric telegraph network expanded, allowing for the more
rapid dissemination of warnings, a national observational network was
developed, which could then be used to provide synoptic analyses.
Instruments to continuously record variations in meteorological
parameters using
photography were supplied to the observing stations from
Kew Observatory – these cameras had been invented by
Francis Ronalds in 1845 and his
barograph had earlier been used by FitzRoy.
To convey accurate information, it soon became necessary to have a
standard vocabulary describing clouds; this was achieved by means of a
series of classifications first achieved by
Luke Howard in 1802, and standardized in the
International Cloud Atlas of 1896.
Numerical prediction
It was not until the 20th century that advances in the understanding of atmospheric physics led to the foundation of modern
numerical weather prediction. In 1922, English scientist
Lewis Fry Richardson published "Weather Prediction By Numerical Process",
after finding notes and derivations he worked on as an ambulance driver
in World War I. He described therein how small terms in the prognostic
fluid dynamics equations governing atmospheric flow could be neglected,
and a finite differencing scheme in time and space could be devised, to
allow numerical prediction solutions to be found.
Richardson envisioned a large auditorium of thousands of people
performing the calculations and passing them to others. However, the
sheer number of calculations required was too large to be completed
without the use of computers, and the size of the grid and time steps
led to unrealistic results in deepening systems. It was later found,
through numerical analysis, that this was due to
numerical instability. The first computerised weather forecast was performed by a team composed of American meteorologists
Jule Charney, Philip Thompson, Larry Gates, and Norwegian meteorologist
Ragnar Fjørtoft, applied mathematician
John von Neumann, and
ENIAC programmer
Klara Dan von Neumann. Practical use of numerical weather prediction began in 1955, spurred by the development of programmable electronic
computers.
Broadcasts
The first ever daily weather forecasts were published in
The Times on August 1, 1861, and the first
weather maps were produced later in the same year. In 1911, the
Met Office
began issuing the first marine weather forecasts via radio
transmission. These included gale and storm warnings for areas around
Great Britain. In the United States, the first public radio forecasts were made in 1925 by Edward B. "E.B." Rideout, on
WEEI, the Edison Electric Illuminating station in Boston. Rideout came from the
U.S. Weather Bureau, as did
WBZ weather forecaster G. Harold Noyes in 1931.
How models create forecasts
The basic idea of numerical weather prediction is to sample the state of the fluid at a given time and use the equations of
fluid dynamics and
thermodynamics
to estimate the state of the fluid at some time in the future. The main
inputs from country-based weather services are surface observations
from automated
weather stations at ground level over land and from weather buoys at sea. The
World Meteorological Organization
acts to standardize the instrumentation, observing practices and timing
of these observations worldwide. Stations either report hourly in
METAR reports, or every six hours in
SYNOP reports. Sites launch
radiosondes, which rise through the depth of the
troposphere and well into the
stratosphere. Data from
weather satellites are used in areas where traditional data sources are not available.
Compared with similar data from radiosondes, the satellite data has the
advantage of global coverage, however at a lower accuracy and
resolution.
Meteorological radar
provide information on precipitation location and intensity, which can
be used to estimate precipitation accumulations over time. Additionally, if a
pulse Doppler weather radar is used then wind speed and direction can be determined.
Modern weather predictions aid in timely evacuations and potentially save lives and prevent property damage
Commerce provides
pilot reports along aircraft routes, and ship reports along shipping routes. Research flights using
reconnaissance aircraft fly in and around weather systems of interest such as
tropical cyclones.
Reconnaissance aircraft are also flown over the open oceans during the
cold season into systems that cause significant uncertainty in forecast
guidance, or are expected to be of high impact 3–7 days into the future
over the downstream continent.
Models are
initialized using this observed data. The irregularly spaced observations are processed by
data assimilation
and objective analysis methods, which perform quality control and
obtain values at locations usable by the model's mathematical algorithms
(usually an evenly spaced grid). The data are then used in the model as
the starting point for a forecast. Commonly, the set of equations used to predict the known as the physics and dynamics of the atmosphere are called
primitive equations.
These equations are initialized from the analysis data and rates of
change are determined. The rates of change predict the state of the
atmosphere a short time into the future. The equations are then applied
to this new atmospheric state to find new rates of change, and these new
rates of change predict the atmosphere at a yet further time into the
future. This
time stepping procedure is continually repeated until the solution reaches the desired forecast time.
The length of the time step chosen within the model is related to
the distance between the points on the computational grid, and is
chosen to maintain
numerical stability. Time steps for global models are on the order of tens of minutes, while time steps for regional models are between one and four minutes. The global models are run at varying times into the future. The
Met Office's
Unified Model is run six days into the future, the
European Centre for Medium-Range Weather Forecasts model is run out to 10 days into the future, while the
Global Forecast System model run by the
Environmental Modeling Center is run 16 days into the future. The visual output produced by a model solution is known as a
prognostic chart, or
prog.
The raw output is often modified before being presented as the
forecast. This can be in the form of statistical techniques to remove
known
biases in the model, or of adjustment to take into account consensus among other numerical weather forecasts.
MOS or model output statistics is a technique used to interpret
numerical model output and produce site-specific guidance. This guidance
is presented in coded numerical form, and can be obtained for nearly
all National Weather Service reporting stations in the United States. As
proposed by
Edward Lorenz
in 1963, long range forecasts, those made at a range of two weeks or
more, are impossible to definitively predict the state of the
atmosphere, owing to the
chaotic nature of the
fluid dynamics
equations involved. In numerical models, extremely small errors in
initial values double roughly every five days for variables such as
temperature and wind velocity.
Essentially, a model is a computer program that produces
meteorological
information for future times at given locations and altitudes. Within
any modern model is a set of equations, known as the primitive
equations, used to predict the future state of the atmosphere. These equations—along with the
ideal gas law—are used to evolve the
density,
pressure, and
potential temperature scalar fields and the
velocity vector field of the atmosphere through time. Additional transport equations for pollutants and other
aerosols are included in some primitive-equation mesoscale models as well. The equations used are
nonlinear partial differential equations, which are impossible to solve exactly through analytical methods, with the exception of a few idealized cases.
Therefore, numerical methods obtain approximate solutions. Different
models use different solution methods: some global models use
spectral methods for the horizontal dimensions and
finite difference methods
for the vertical dimension, while regional models and other global
models usually use finite-difference methods in all three dimensions.
Techniques
Persistence
The
simplest method of forecasting the weather, persistence, relies upon
today's conditions to forecast the conditions tomorrow. This can be a
valid way of forecasting the weather when it is in a steady state, such
as during the summer season in the tropics. This method of forecasting
strongly depends upon the presence of a stagnant weather pattern.
Therefore, when in a fluctuating weather pattern, this method of
forecasting becomes inaccurate. It can be useful in both short range
forecasts and
long range forecasts.
Use of a barometer
Measurements
of barometric pressure and the pressure tendency (the change of
pressure over time) have been used in forecasting since the late 19th
century. The larger the change in pressure, especially if more than 3.5
hPa (2.6
mmHg), the larger the change in weather can be expected. If the pressure drop is rapid, a
low pressure system is approaching, and there is a greater chance of rain.
Rapid pressure rises are associated with improving weather conditions, such as clearing skies.
Looking at the sky
Marestail shows moisture at high altitude, signalling the later arrival of wet weather.
Along with pressure tendency, the condition of the sky is one of the
more important parameters used to forecast weather in mountainous areas.
Thickening of
cloud cover or the invasion of a higher cloud deck is indicative of rain in the near future. High thin
cirrostratus clouds can create
halos around the
sun or
moon, which indicates an approach of a
warm front and its associated
rain. Morning
fog
portends fair conditions, as rainy conditions are preceded by wind or
clouds that prevent fog formation. The approach of a line of
thunderstorms could indicate the approach of a
cold front. Cloud-free skies are indicative of fair weather for the near future. A
bar can indicate a coming tropical cyclone. The use of sky cover in weather prediction has led to various
weather lore over the centuries.
Nowcasting
The forecasting of the weather within the next six hours is often referred to as
nowcasting.
In this time range it is possible to forecast smaller features such as
individual showers and thunderstorms with reasonable accuracy, as well
as other features too small to be resolved by a computer model. A human
given the latest radar, satellite and observational data will be able to
make a better analysis of the small scale features present and so will
be able to make a more accurate forecast for the following few hours. However, there are now
expert systems using those data and mesoscale numerical model to make better extrapolation, including evolution of those features in time.
Use of forecast models
In the past, the human forecaster was responsible for generating the entire weather forecast based upon available observations. Today, human input is generally confined to choosing a model based on various parameters, such as model biases and performance. Using a consensus of forecast models, as well as ensemble members of the various models, can help reduce forecast error.
However, regardless how small the average error becomes with any
individual system, large errors within any particular piece of guidance
are still possible on any given model run.
Humans are required to interpret the model data into weather forecasts
that are understandable to the end user. Humans can use knowledge of
local effects that may be too small in size to be resolved by the model
to add information to the forecast. While increasing accuracy of
forecast models implies that humans may no longer be needed in the
forecast process at some point in the future, there is currently still a
need for human intervention.
Analog technique
The
analog technique is a complex way of making a forecast, requiring the
forecaster to remember a previous weather event that is expected to be
mimicked by an upcoming event. What makes it a difficult technique to
use is that there is rarely a perfect analog for an event in the future.
Some call this type of forecasting pattern recognition. It remains a
useful method of observing rainfall over data voids such as oceans,
as well as the forecasting of precipitation amounts and distribution in
the future. A similar technique is used in medium range forecasting,
which is known as teleconnections, when systems in other locations are
used to help pin down the location of another system within the
surrounding regime. An example of teleconnections are by using
El Niño-Southern Oscillation (ENSO) related phenomena.
Communicating forecasts to the public
An example of a two-day weather forecast in the visual style that an American newspaper might use. Temperatures are given in Fahrenheit.
Most end users of forecasts are members of the general public. Thunderstorms can create strong winds and dangerous
lightning strikes that can lead to deaths, power outages, and widespread hail damage. Heavy snow or rain can bring transportation and commerce to a stand-still, as well as cause flooding in low-lying areas. Excessive
heat or
cold waves can sicken or kill those with inadequate utilities, and
droughts can impact water usage and destroy vegetation.
Several countries employ government agencies to provide forecasts
and watches/warnings/advisories to the public in order to protect life
and property and maintain commercial interests. Knowledge of what the
end user needs from a weather forecast must be taken into account to
present the information in a useful and understandable way. Examples
include the
National Oceanic and Atmospheric Administration's
National Weather Service (NWS) and
Environment Canada's
Meteorological Service (MSC).
Traditionally, newspaper, television, and radio have been the primary
outlets for presenting weather forecast information to the public. In
addition, some cities had
weather beacons. Increasingly, the internet is being used due to the vast amount of specific information that can be found. In all cases, these outlets update their forecasts on a regular basis.
Severe weather alerts and advisories
A
major part of modern weather forecasting is the severe weather alerts
and advisories that the national weather services issue in the case that
severe or hazardous weather is expected. This is done to protect life
and property. Some of the most commonly known of severe weather advisories are the
severe thunderstorm and
tornado warning, as well as the
severe thunderstorm and
tornado watch. Other forms of these advisories include winter weather, high wind,
flood,
tropical cyclone, and fog. Severe weather advisories and alerts are broadcast through the media, including radio, using emergency systems as the
Emergency Alert System, which break into regular programming.
Low temperature forecast
The low temperature forecast for the current day is calculated using the lowest temperature found between 7 pm that evening through 7 am the following morning. So, in short, today's forecasted low is most likely tomorrow's low temperature.
Specialist forecasting
There
are a number of sectors with their own specific needs for weather
forecasts and specialist services are provided to these users.
Air traffic
Because the aviation industry is especially sensitive to the weather,
accurate weather forecasting is essential. Fog or exceptionally low
ceilings can prevent many aircraft from landing and taking off.
Turbulence and
icing are also significant in-flight hazards. Thunderstorms are a problem for all aircraft because of severe turbulence due to their
updrafts and
outflow boundaries, icing due to the heavy precipitation, as well as large
hail, strong winds, and lightning, all of which can cause severe damage to an aircraft in flight.
Volcanic ash is also a significant problem for aviation, as aircraft can lose engine power within ash clouds. On a day-to-day basis airliners are routed to take advantage of the
jet stream tailwind to improve fuel efficiency. Aircrews are briefed prior to
takeoff on the conditions to expect en route and at their destination. Additionally, airports often change which
runway is being used to take advantage of a
headwind. This reduces the distance required for takeoff, and eliminates potential
crosswinds.
Marine
Commercial and recreational use of waterways can be limited significantly by wind direction and speed,
wave
periodicity and heights, tides, and precipitation. These factors can
each influence the safety of marine transit. Consequently, a variety of
codes have been established to efficiently transmit detailed marine
weather forecasts to vessel pilots via radio, for example the
MAFOR (marine forecast). Typical weather forecasts can be received at sea through the use of
RTTY,
Navtex and
Radiofax.
Agriculture
Farmers rely on weather forecasts to decide what work to do on any particular day. For example, drying
hay is only feasible in dry weather. Prolonged periods of dryness can ruin
cotton,
wheat, and
corn crops. While corn crops can be ruined by drought, their dried remains can be used as a cattle feed substitute in the form of
silage.
Frosts and freezes play havoc with crops both during the spring and fall. For example,
peach trees in full bloom can have their potential peach crop decimated by a spring freeze.
Orange groves can suffer significant damage during frosts and freezes, regardless of their timing.
Forestry
Weather forecasting of wind, precipitations and humidity is essential for preventing and controlling
wildfires. Different indices, like the
Forest fire weather index and the
Haines Index,
have been developed to predict the areas more at risk to experience
fire from natural or human causes. Conditions for the development of
harmful insects can be predicted by forecasting the evolution of
weather, too.
Utility companies
An air handling unit is used for the heating and cooling of air in a central location (click on image for legend).
Electricity and gas companies rely on weather forecasts to anticipate
demand, which can be strongly affected by the weather. They use the
quantity termed the degree day to determine how strong of a use there
will be for heating (
heating degree day)
or cooling (cooling degree day). These quantities are based on a daily
average temperature of 65 °F (18 °C). Cooler temperatures force heating
degree days (one per degree Fahrenheit), while warmer temperatures force
cooling degree days. In winter, severe cold weather can cause a surge in demand as people turn up their heating. Similarly, in summer a surge in demand can be linked with the increased use of
air conditioning systems in hot weather.
By anticipating a surge in demand, utility companies can purchase
additional supplies of power or natural gas before the price increases,
or in some circumstances, supplies are restricted through the use of
brownouts and
blackouts.
Other commercial companies
Increasingly,
private companies pay for weather forecasts tailored to their needs so
that they can increase their profits or avoid large losses.
For example, supermarket chains may change the stocks on their shelves
in anticipation of different consumer spending habits in different
weather conditions. Weather forecasts can be used to invest in the
commodity market, such as futures in oranges, corn, soybeans, and oil.
Military applications
United Kingdom Armed Forces
Royal Navy
The UK
Royal Navy, working with the UK
Met Office,
has its own specialist branch of weather observers and forecasters, as
part of the Hydrographic and Meteorological (HM) specialisation, who
monitor and forecast operational conditions across the globe, to provide
accurate and timely weather and oceanographic information to
submarines, ships and
Fleet Air Arm aircraft.
Royal Air Force
A mobile unit in the
RAF, working with the UK
Met Office, forecasts the weather for regions in which British, allied servicemen and women are deployed. A group based at
Camp Bastion provides forecasts for the British armed forces in
Afghanistan.
United States Armed Forces
US Navy
Emblem of JTWC Joint Typhoon Warning Center
Similar to the private sector, military weather forecasters present
weather conditions to the war fighter community. Military weather
forecasters provide pre-flight and in-flight weather briefs to pilots
and provide real time resource protection services for military
installations. Naval forecasters cover the waters and ship weather
forecasts. The
United States Navy
provides a special service to both themselves and the rest of the
federal government by issuing forecasts for tropical cyclones across the
Pacific and Indian Oceans through their
Joint Typhoon Warning Center.
US Air Force
Within the United States, Air Force Weather provides weather forecasting for the Air Force and the Army.
Air Force forecasters cover air operations in both wartime and peacetime operations and provide
Army support;
United States Coast Guard marine science technicians provide ship forecasts for ice breakers and other various operations within their realm; and Marine forecasters provide support for ground- and air-based
United States Marine Corps operations. All four military branches take their initial enlisted meteorology technical training at
Keesler Air Force Base. Military and civilian forecasters actively cooperate in analyzing, creating and critiquing weather forecast products.