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Analysing and forecasting the weather, using numerical models, requires an
impressive amount of computing and data processing power. This is why a powerful
supercomputer is needed to ingest and process all this data. The process which
leads to the production of a forecast can be seen as an endless cycle of computer
processes, which are called "operational runs". A complete operational
run can be summarized as follows:
- Data ingest:
- decoding, re-formatting and quality control of large amounts of meteorological
data from many sources worldwide.
- Data assimilation (analysis):
- derivation of an up-to-date snapshot of the state of the atmosphere. This
must be an accurate three-dimensional depiction of atmospheric winds, pressure,
moisture, and temperature.
- As a first step in the assimilation of the observational data into the forecasting
system, the analysis begins with a best guess, called a trial field, which
is a 6-hour model forecast representing our accumulated knowledge of the state
and trends of the real atmosphere. The new analysis is then obtained by using
sophisticated mathematical methods to strike a judicious balance between the
trial field and the newly-acquired observational data. The end-result is called
an objective analysis.
- Forecasting:
- prediction of the behaviour of the atmosphere for up to ten days into the
future.
- The updated objective analysis is used as the starting point in running
the GEM (Global Environmental Multiscale) atmospheric model.
- Weather models, such as GEM, use a three-dimensional mathematical grid to
represent space. Generally speaking, the tighter the grid, the more accurate
the model's representation of the atmosphere becomes. But a tight model grid
comes at a steep price in execution costs. A balance must therefore be reached
to run the model at the highest possible resolution, while attaining the best
results in terms of economy and timeliness. For this reason, the GEM model
is run on two types of operational grids: an evenly-spaced global grid, well
suited for medium-term forecasts (3-10 days), and a so-called "regional"
grid, featuring a variable-mesh grid which is tighter over North America and
adjacent waters. The regional grid's higher resolution is well suited for
short-term forecasts (up to 2 days) over the North-American region and the
adjacent Oceans
- Post-Processing:
- raw numerical results from the GEM model are fed into post-processing systems
to generate finished and semi-finished forecast products: gridded numerical
data, charts, bulletins, etc.
- The GEM model output is also used as input to other models, for the prediction
of
- ocean waves
- volcanic ash/radionucleide atmospheric transport
- air quality (smog)
- stratospheric ozone and solar UV radiation
Other refinements include the use of statistical methods to improve on the
raw numerical forecast of temperature, wind, and probability of precipitation,
for specific locations.
- Dissemination:
- large amounts of data produced by the analysis and forecasting system are
sent to offices of the Meteorological Service of Canada which, in turn, use
them as input into their local forecasts or disseminate them to the Canadian
public and other clients. In addition, data from the operational runs are
sent directly to a wide variety of outside users including federal and provincial
agencies, the Departement of National Defense, Nav Canada, and to some major
commercial clients. Data are sent out via satellite or land telecommunication
networks, as well as more and more being made available on the world-wide
web.
Recent changes to the operational
runs
Technical outline of the global
forecast system (data assimilation and operational model)
Technical outline of the regional
forecast system (data assimilation and operational model)
Technical outline of the surface
analyses
Technical outline and timetable of the main
operational runs
Timelines of Numerical Weather
Prediction in Canada
Created :
1997-02-24
Modified :
2002-12-18
Reviewed :
2002-12-18
Url of this page : http://www.msc.ec.gc.ca /cmc/op_systems/index_e.html
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