Figure 5 A. The high-water situation in a part of
the Porttipahta reservoir in northern Finland. The
symbol I displays surrounding dry areas while other
symbols indicate aquatic areas. B. Lower littoral
areas 2.3 m below the water level of Fig. 5A are
displayed with white pixels. C. Upper littoral
areas up to 5 m above the water level are indicated
with various dark pixels (Jantunen and Raitala 1984).
5. DISCUSSION
The continuity of the Landsat program from 1972
until now has been very promising with respect to
long-term studies. During the last 14 years the
main focus of research has been to develop methods
and approaches for practical applications of
monitoring remote sensing. The latest satellite in
this series, Landsat 5, is expected to stop trans
mitting data before replacement. This in itself in
creases expectations for the French SPOT satellite
remote sensing, but there will still be abundant
need of information especially on environmental
changes over the last decade, and this need can be
met only by using the old Landsat MSS data.
The use of previous Landsat data should not be
diminished merely because of the availability of new
satellite data with better spectral and ground re
solution. Although remote sensing science itself
will gain advantages with the increased accuracy of
the radiation recordings many more practical demands
of other natural and environmental sciences will
derive advantage from the time perspective offered
by the Landsat data. This is especially evident
within the spheres of aquatic research and inves
tigation because these repeated registrations may
often constitute the only possibility of tracing the
more original situation before the changes, appear
ing almost daily, have taken place.
There is no denying the charm of novelty with
respect to new and ever-better satellite data. But
we should also maximize the continued use of all
satellite information and share the evident benefits
of multitemporal satellite data with all possible
diversified users, including scientists, decision
makers and ordinary people interested in the state
of the environment.
REFERENCES
Arkimaa, H. and J. Raitala 1981. Landsat example of
small lake classification. Aqua Fennica 11: 55-
60.
Arkimaa, H. and J. Raitala 1984. Landsat classifi
cation of the coastal water areas of the Bothnian
Bay off Oulu. Finnish Marine Research 250: 45-51.
Beardsley, T. 1986. Remote sensing. Nature 319: 4.
Hammack, J.C. 1977. Landsat goes to sea. Photo-
gramm. Eng. Remote Sensing 43: 683-691.
Jantunen, H. and J. Raitala 1984. Locating shore
line changes in the Porttipahta (Finland) water
reservoir by using multitemporal Landsat data.
Photogrammetria 39: 1-12.
Lindell, T. 1980. Calibration of Landsat data for
mapping of water quality in Malaren, Sweden.
Statens naturvardsverk PM 1266, Uppsala, Sweden.
Raitala, J. and H. Jantunen and S. Hellsten 1984a.
A Landsat-assisted study of the aquatic areas of
the Lake Kemijarvi region, Northern Finland.
Earth, Moon, and Planets 31: 183-216.
Raitala, J. and H. Jantunen and V. Myllymaa 1984b.
Developments in the evaluation of small lake water
quality from digital Landsat MSS data, Kuusamo,
Northeast Finland. Earth, Moon, and Planets 31:
249-264.
Raitala, J. and J. Siira and H. Arkimaa 1984c.
Landsat classification of the hydrolittoral areas
of the Bay of Liminka (Gulf of Bothnia, Finland).
Aquilo Ser. Bot. 20: 14-23.
Raitala, J. and J. Lampinen 1985. A Landsat study
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Acknowledgement: The writing of this paper was per
formed while the author held a NRC - NASA Resident
Research Associateship at the Jet Propulsion Labora
tory, Calif. Institute of Technology.
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