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Marine Observers Handbook
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Although the use of such terms as fog, mist and haze is suitable for a general indication of the
state of visibility in the WW code or in the text of a ship's logbook, a more precise method is
needed in weather messages to indicate to the meteorologist the degree of obscurity of the
atmosphere, irrespective of the reason that causes it. On land, observations are made of a
number of selected objects at fixed distances, the distances increasing roughly in such a way
that each distance is nearly double the next smaller distance. The determination of the most
distant object of the series which is visible on any given occasion constitutes the observation
of visibility. At sea such a detailed determination of visibility is not usually possible, but in
making estimates of visibility a coarser scale is used, as shown below.
VISIBILITY SCALE FOR USE AT SEA
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Code
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Code
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figure
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figure
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90
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Less than 50m
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95
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1.1 n.mile or 2km
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91
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5 0m
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96
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2.2n.mile or 4km
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92
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0.1 1 n.mile or 200m
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97
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5.4n.mile or 10km
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93
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0.27 n. mile or 500 m
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98
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10.8 n. mile or20 km
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94
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0.54 n. mile or 1km
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99
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27.0 n. mile or 50km
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Note 1: If the distance of visibility is between two of the distances given in the table, the code figure for the shorter
distance is reported. Note 2: The prefix '9' before each of the scale numbers appears here because this table is part
of a code for reporting visibility in two figures by radio (see Met.O.509, Ship’s Code and Decode Book, or Admiralty
List of Radio Signals, Volume 3).
In a long vessel the determination of the lowest numbers offers no difficulty as objects at
known distances may be used. Visibility numbers in the middle range indicate conditions of
obscurity such that the visibility is greater than the length of the ship but is not sufficient to
allow full speed to be maintained. The only means of obtaining observations for the higher
numbers of the scale are as follows. When coasting and when fixes can be obtained, the
distance of points when first sighted, or last seen may be measured, from the chart. In the
open sea, when other ships are sighted, visibility may be estimated by noting the radar range
when the vessel is first sighted visually and again when it disappears from view. It is
customary to use the horizon to estimate visibility numbers in the higher range although this
cannot be relied upon. There are cases of abnormal refraction when the visible horizon may
be very misleading as a means of judging distances, particularly when the height of the eye is
great, as in the case of an observer on the bridge of a large vessel.
The estimation of visibility at night is very difficult. What the meteorologist is interested in
knowing is the degree of transparency of the atmosphere. But the distance seen at night
depends on the amount of illumination; and the distance at which a light is seen depends on
its intensity or candle-power. If there is no obvious change in meteorological conditions, the
visibility just after dark will be the same as that recorded just before dark irrespective of the
fact that one may not be able to see as far. A deterioration in visibility can sometimes be
detected afterwards and the visibility figure adjusted accordingly. In doing this, care must be
taken not to confuse the effect of a decrease in illumination, as for example when the moon
sets, with a genuine decrease in visibility. The presence of a 'loom' around the vessel's
navigation lights is frequently a guide to deteriorating visibility.