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DISCUSSION ON THE GENERAL REPORT OF SUB-COMM IV-3 163
fragt, der durch die Aufnahme bei bedecktem
Himmel erzielt werden kann, statistisch erzielt
werden kann, dann kann ich zwei Zahlen nen-
nen, die für Deutschland gelten. Wir haben, wie
Dr Härry soeben erwähnte, die Zahl von etwa
25 Tagen im Jahr, bei denen die Bewölkung ein
Achtel oder kleiner ist. Wir haben in Deutsch-
land im Durchschnitt einiger Jahre, für die wir
das genau verfolgt haben, 22 Tage festgestellt.
22 Tage im ganzen Jahr, an denen der Himmel
mit ein Achtel oder weniger Wolken bedeckt ist.
Wenn wir jetzt die Forderung stellen, dass der
Himmel zumindestens sieben Achtel mit Wolken
bedeckt sein soll, dass aber die Wolkenhöhe
natürlich nicht niedriger sein darf als die Flug-
höhe, weil wir ja durch die Wolken hindurch
nicht photographieren können, dann ergab eine
statistische Auswertung, die wir mit dem Deut-
schen Zentralamt für Wetterdienst ausgeführt
haben, dass wir für zwei, und zwar für die
beiden in Deutschland hauptsächlich vorkom-
menden Flughöhen, 2.500 m und 1.900 m, dass
wir für diese beiden Flughöhen pro Monat be-
reits zu 19 oder 15 Bildflugtagen kommen. Das
heisst, dass im Durchschnitt jeder zweite Tag
für den Bildflug geeignet ist. Das scheint ein
ganz bedeutender Fortschritt zu sein, den man
in der praktischen Luftbildaufnahme beachten
sollte. Danke.
Herr Dr Hànnv: Ich danke Herrn Prof
Schwidefsky für seine ausserordentlich interes-
santen Ausführungen, die für uns vom Stand-
punkt der praktischen photogrammetrischen
Produktion aus sehr ermutigend sind. Und ich
móchte gleich übergehen und Herrn Fagerholm
bitten, uns seine Ausführungen zu geben über
eine konkrete Durchführung einer Aufnahme
und Auswertung für Grossmasstab-Photogram-
metrie aber eben auf Grund von Luftbildauf-
nahmen, die bei extrem ungünstiger Beleuchtung
ausgeführt wurden
Dr P. O. FAGERHOLM: When Dr Hürry a
couple of days ago asked me to present a report
on this investigation I had a feeling that our little
investigation might be of too little value for
such an eminent group as this. However, espe-
cially since having heard what Professor
Schwidefsky said about these investigations in
aerial photography when the sky is cloudy, I
think it might be of interest to give some infor-
mation about the work.
First, I may say that this investigation was
started late last Fall, and it was only possible to
carry it through by the co-operation given to us
by various Swedish Governmental Agencies, We
made the investigation within the Swedish
Hydrographic Department, and the project
engineer was one of my assistants. He was Mr
Thunberg and I should like to pay tribute to him
for his good work.
The background for the investigation was
that we were interested in having a possibility
for getting photogrammetric surveys of rather
limited areas without waiting for aerial photog-
raphic weather to arrive in the country. Also,
the nice weather has to be used for the larger
photographic missions and cannot be used for
rather small jobs.
In the first place, Sweden is pretty far north.
The southern part is about 59° latitude, and
the northern part extends up past the Arctic
Circle. That means that the sun is very often
low; the elevation angle to the sun is small.
The aerial photography I startel with was
made on 16th September. It was heavily cloud-
ed, a very dark, grey day, where you certainly
get out of the mood and do not like to do any-
thing in the way of aerial photography. It was
raining, the cloud height was about 270 metres.
The Geographical Survey Office made their
aerial photography from 250 metres, that was
with an aeroplane flying at 230 kilometres an
hour. The film was a fast one, 400 ASA. It was
an Ilford film. The shutter speed was only 1/425
of a second.
Four flights were made over the little terri-
tory, and three of these models were well enough
positioned for our purpose and were used. In
the test area we had placed about 200 signals,
most of them cardboard pieces — white card-
board — 6 X 6 cms. Some signals were also
painted on rocks or pavements. I should add
perhaps that we were very well aware of the fact
that the flying height was much lower than
needed for accuracy purposes, but we thought
we would try under very unfavourable condi-
tions. In the test area we made a small geodetic
net of high precision, composed of 13 points.
The scale was determined with a geodimeter 4.
The 13 points after adjustment gave a standard
error of = 2.2 mm in x and + 1 mm in y.
After the flight we surveyed as accurately as
we could. It was frosty and partly snow, and so
there were very unfavourably conditions for
accurate geodetic surveys. We surveyed about
130 signals which could be regarded as remain-
ing in the position from air photography. After
some sorting out of a few which certainly had
been moved by dogs or children — it was just in
Stockholm, this area — we had about 100 left
with an error margin of 10 mm. The diapositives
were made without the use of logetronics. I