Henry C. Adams
Capitolo 9
where the tides are produced, when it is his/her Southerner
declination and furthest street when in the north but the sun
it is indeed more next to the earth December 31 (the perihelion)
and furthest by July me (the aphelion), the difference among
the maximum one and to be of distance of minimum one-thirtieth of the
whole.
The moon travels in a diagonal and similar direction around the
earth, varying above between 18-1/2 degrees and 28-1/2 degreeds
and under the equator. The south change north
declination takes place every fourteen days but these changes
doesn't necessarily happen to the change in the phases of
the moon. When the moon is southern of the equator, she is more neighbor
to the Southern ocean, where the tides are produced. The new one
moon is more neighbor to the sun and crosses the midday meridian,
while the full moon crosses it to midnight.
The height of the tide in the afternoon varies from that of the
tide in the morning; sometimes one is the tallest and sometimes the
other, according to the declination of the sun and moon. This
you/he/she has called her/it "diurnal inequality." The middle difference
between the night and tides in the morning they are approximately 5 in on the east
coast and approximately 8in on the coast of the west. When there is a
the considerable difference in the height of tall water of two
consecutive tides, the decline that follows the tallest tide is
you lower that that following the tall and lower water, and as a
it regulates general the tallest the tide rises lowers him it will fall.
The various height of spring tides in the whole year, while being to
a maximum when the sun is on the equator to the equinoxes and
to a minimum in June to the solstice in summer when the sun is
furthest street from the equator. In the tall Southern ocean
water of spring tides happens to mean-day on the meridian of
Greenwich and to midnight on the 180 meridian, and it is later
the coasts of other seas in proportion to the time taken for
the derivative waves to contact them the tide that is approximately three,-