During the last decade, it became clear that the
chemical composition of the atmosphere
changed globally. Moreover, human activities are partly
responsible for this evolution. This is why experiments
conducted on the Space Pole are integrated in international
programs like the one called Global Change. For a better
understanding of the phenomena, which influence the
Earth’s atmosphere and climate, the programs study
atmospheric mechanisms on a global scale.
With this goal, the experimental programs at the
Belgian Institute for Space Aeronomy
use a broad variety of means: observations and measurements
are carried out from Earth observatories, stratospheric
balloons, rocket probes on board of spacecrafts like
space shuttles and satellites. More and more, space
research depends on measurements in the laboratory.
Furthermore, theoretical research is important because
the theoretical modelling is necessary for the interpretation
of experimental data. These models map the past, the
present and the future atmospheric conditions.
The atmospheric environment studies imply measures
on particles coming from various sources such urban
pollution and volcanic plumes to the atmosphere as a
whole. The observations have to be spread over a longer
period. This permits the distinction between long term
tendencies and natural changes that are related to seasonal
or other cyclic phenomena like the activity of the Sun.
The combination of different kinds of techniques and
measuring platforms (ground stations, airplane, balloon,
rocket, spacecraft, satellite) permits to obtain good
results. The experiments on the ground (picture
1) or carried out in a balloon or in an airplane
are preferable because of their accuracy in the studies
of physical chemical processes. The satellite instruments (video 1), make it possible
to extrapolate these studies to a worldwide scale. They
provide constant world cartography of the most important
atmospheric elements and parameters. To obtain a total
vision, scientists integrate the different processes
into mathematical computer models of the atmosphere.
Concerning meteorological forecast (picture
2), it is essential to precisely visualize the
present state of the weather. That implies the construction
of a graphic model on a broad scale, from the surface
and upward.
To build such a graphic model, the
Royal Meteorological Institute, through a network
of observation stations, collect parameters like atmospheric
pressure, air temperature, direction and intensity of
the wind, cloudiness, atmospheric humidity and the amount
of rainfall, every three hours. These observations are
carried out all over the world at the same time in a
standardized way.
In addition to the observations at the surface, other
observations on the level of the atmosphere must be
carried out to elaborate a 3D meteorology graphical
model. On different places in the world aerological
probes are carried out. In Belgium, the RMI performs
this kind of (picture 3)
modelling four times per day. A balloon filled with
hydrogen and transporting a radio probe, will gather
weather data up to thirty kilometers. The measurements
are then sent back to a receiving station located at
Ukkel.
Besides the classical observations, as described above,
satellite observations try to fill the shortages since
the sixties. Meteorological satellites in an orbit
around the Earth deliver on regular points in time images
of parts of the atmosphere. Thanks to these, we can
see the cloud animations, during the weather reports
on television. Moreover, the original images coming
from the satellite have an enormous scientific value.
Radar images have gained of importance in the last
decade. These images make it possible to follow the
displacement of rainfall in almost real time. By a system
called SAFIR, the
Royal Meteorological Institute
can follow the evolution of storms
by recording the discharges of thunders, and then emit
warnings useful for the population.
Because of enormous progress in the space research,
we are now able to study every part of the radiations
balance on an international scale. Certain instruments,
like the radiometers, developed in Ukkel, become an
international reference. The obtained data are interesting
for the whole scientific community interested in the
changes of the climatologic balance.
Following and understanding the water cycle to contribute
to a durable development and respect for indispensable
resources is a task that passions certain scientists.
Measuring the amount of rainfall (picture
4) is less simple than one would think. For a
correct evaluation of what a hydrologic basin receives,
one has to choose measuring instruments in function
of the type of rain (rain showers, frontal rain…).
The measurements of water vapor
is an important parameter, by either direct measurement,
or indirect starting from different parameters. The
development of new means on board of satellites (video
2) or on the ground therefore demands hydrologists,
specialized in the atmospheric part of the water cycle,
bending over new challenges.
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