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9 MODELLING
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vertical air motions, temperature changes and moisture processes among other
variables to calculate what the atmosphere might look like. Computer models
have to include hundreds of mathematical equations to produce a weather
forecast. A lot of computing power is needed to run a computer model. It is
usual for supercomputers to be used in such activities. As we have seen, these
supercomputers are able to perform quadrillions of calculations every second!
The UK Met Office uses the Unified Model (UM) approach. This is a numerical
model of the atmosphere used for both weather and climate applications. It is a
model which is being continuously developed by the Met Office and its partners.
The Met Office uses a seamless modelling approach, whereby a single group
of related models can be used to make predictions over a number of timescales
involving short-term weather forecasts as well as long-range climate forecasts.
The models used take variables like atmospheric pressure, humidity, rainfall,
temperature, wind speed and wind direction, which are recorded all over the Earth’s
surface, into account. The model is suitable for NWP, seasonal forecasting and
climate modelling, with forecast times ranging from a few days to hundreds of years.
Furthermore, the UM approach can be used both as a global and a regional model.
For the weather forecasting aspect, atmospheric models can be used to compare
the current conditions with previous days at similar times of the year with
the same or similar conditions. This enables a reasonably accurate forecast to
be made. Maps are produced showing isobars, temperatures and wind speed.
Predictions can be made because similar weather conditions will have been
observed over very long periods of time.
Climate change
Climate can be measured using a number of variables (quantities that change)
such as rainfall, hours of sunlight, wind speed and temperature, among others.
Temperatures in most regions of our planet vary according to the time of year.
Summer in the southern hemisphere tends to be December to February, while
in the northern hemisphere it is June to August. The temperature differences
between different regions of the world cause differences in atmospheric pressure
which, in turn, lead to winds, storms and, in some cases, hurricanes. Many
scientists believe that the increasing levels of carbon dioxide in the atmosphere,
which is leading to hotter temperatures for our planet, will give rise to major
changes in our climate. Climate change is already beginning to happen in the
Arctic and Antarctic. This does not necessarily mean that all regions on the
planet will become hotter, but some will. The result will be more changeable
weather conditions, such as extremely high levels of temperature, rain- and
snowfall becoming far more frequent than they are now. Forecasting the
possible changes to the Earth’s climate, in other words the long-term patterns
of weather for the entire planet, is obviously going to be more complex than
relatively short-term weather forecasting for specific regions of the planet.
For a long time now, the Earth’s climate has been monitored and records
have been kept of the actual values of the variables involved over a number of
years. This data can be input into a computer model, which is a large and very
complex program that runs on a supercomputer. It is made up of a collection
of equations representing different parts of the climate. Each equation contains
variables like temperature, rainfall, the amount of carbon dioxide in the
atmosphere, and sea level. It shows how each of these affects the other variables.
The variables can be changed to see what effect they will have on the climate.
These equations together give an approximation of the Earth’s climate. The
model can be used to predict trends and examine the effect of increasing and