Henry C. Adams

Capitolo 11

29, p.m.......  2.32....... 2.30.....  2 first mins.


Even if the times of the tides so notably varied, them
heights were precisely as aforesaid in the tide-table.

The records during a storm October 29 th 1838, it gave a
completely different result, as the time was delayed only ten or
twelve minutes, but the height was increased by 8 fts On another
you cause the tide to Liverpool 7 fts you/he/she was increased by a strong wind.
The Bristol Channel holds the record for the greatest tide
experimented around the beaches of Great Britain that it happened
to Chepstow in 1883, and it had an increase of 48 fts 6 in The
configuration of the Channel of Bristol is, clearly, contributor
to the great tides, but abnormally tall tides don't generally do
happens more frequently on our beaches that perhaps once in ten
years, the last that happens in the first part of 1904,
even if there it is able hostile the a lot of extra one tall during this period
of ten strong wind years of on-beach. Where tides draw near to a place
from different directions you/he/she can be an interval among the
times of arrival that give place to there being two periods of
tall and low water, as to Southampton, where the approach of tides
from every side of the island of Wight.

The time to which tall water happens to some place on the coast
to the duration of new moon or flood it is known as the establishment
of that place, and when this, together with the height to that
the tide rises above of low water has verified from actual
observation, is possible with the help of the nautical one
almanack to make calculations that the time will guess and
height of the daily tides to that place for every future time. From
he/she wants to say of a car that tide-foretells, invented by God Kelvin,
the tides for one whole year can be calculated in from three to
four hours. This car is fully described of minutes of
Procedures, Inst.C.E., Vol. LXV. The age of the tide to some
place is the time period between new moon or flood and the
event of spring tides to that place. The series of a tide