6.3.3.1 The skipper of a fishing vessel should
bear in mind that ice formation is a complicated process which depends
upon meteorological conditions, condition of loading and behaviour
of the vessel in stormy weather as well as on the size and location
of superstructures and rigging. The most common cause of ice formation
is the deposit of water droplets on the vessel's structure. These
droplets come from spray driven from wave crests and from ship-generated
spray.
6.3.3.2 Ice formation may also occur in conditions
of snowfall, sea fog (including arctic sea smoke), a drastic fall
in ambient temperature, as well as from the freezing of drops of rain
on impact with the vessel's structure.
6.3.3.3 Ice formation may sometimes be caused
or accentuated by water shipped on board and retained on deck.
6.3.3.4 Intensive ice formation generally occurs
on stem, bulwark and bulwark rail, front walls of superstructures
and deck-houses, hawse holes, anchors, deck gear, forecastle deck
and upper deck, freeing ports, aerials, stays, shrouds, masts and
spars.
6.3.3.5 It should be borne in mind that the most
dangerous areas as far as ice formation is concerned are the sub-Arctic
regions.
6.3.3.6 The most intensive ice formation takes
place when wind and sea come from ahead. In beam and quartering winds,
ice accumulates quicker on the windward side of the vessel, thus leading
to a constant list which is extremely dangerous.
6.3.3.7 Listed below are meteorological conditions
causing the most common type of ice formation due to spraying of a
vessel. Examples of the weight of ice formation on a typical fishing
vessel of displacement in the range 100 t to 500 t are also given.
For larger vessels the weight will be correspondingly greater.
6.3.3.8 Slow accumulations of ice take place:
-
.1 at ambient temperature from -1°C to -3°C
and any wind force;
-
.2 at ambient temperature -4°C and lower and
wind force from 0 m/s to 9 m/s; and
-
.3 under the conditions of precipitation, fog
or sea mist followed by a drastic fall of the ambient temperature.
Under all these conditions the intensity of ice accumulation
may not exceed 1.5 t/h.
6.3.3.9 At ambient temperature of -4°C to
-8°C and wind force 10 m/s to 15 m/s, rapid accumulation of ice
takes place. Under these conditions the intensity of ice accumulation
can lie within the range 1.5 t/h to 4 t/h.
6.3.3.10 Very fast accumulation of ice takes place:
Under these conditions the intensity of ice accumulation
can exceed 4 t/h.
6.3.3.11 The skipper should bear in mind that
ice formation adversely affects the seaworthiness of the vessel as
ice formation leads to:
-
.1 an increase in the weight of the vessel due
to accumulation of ice on the vessel's surfaces which causes the reduction
of freeboard and buoyancy;
-
.2 a rise of the vessel's centre of gravity due
to the high location of ice on the vessel's structures with corresponding
reduction in the level of stability;
-
.3 an increase of windage area due to ice formation
on the upper parts of the vessel and hence an increase in the heeling
moment due to the action of the wind;
-
.4 a change of trim due to uneven distribution
of ice along the vessel's length;
-
.5 the development of a constant list due to uneven
distribution of ice across the breadth of the vessel; and
-
.6 impairment of the manoeuvrability and reduction
of the speed of the vessel.
6.3.4 Operational procedures related to ensuring
a fishing vessel's endurance in conditions of ice formation are given
in annex 2 (Recommendations for skippers of fishing vessels on ensuring
a vessel's endurance in conditions of ice formation).