The winter solstice occurs when the sun is
directly over the Tropic of Capricorn, which is located at
23.5° South of the equator
and runs through Australia, Chile, southern Brazil,
and northern South Africa. The winter solstice marks the shortest
day and longest night of the year in the Northern Hemisphere.
Additionally, the sun appears at its lowest elevation with
a noontime position that changes very little for several days
before and after the winter solstice. In fact, the word solstice
comes from Latin solstitium or sol (the sun)
+ -stit-, -stes (standing). This year, the Northern
Hemisphere solstice will
occur
at 11:08
pm MST on
December
21, 2007
(official time
is 0608 UTC on December 22). For a complete listing of the
dates of the winter and summer solstice's and spring and fall
equinox's
through 2020, check out this site from the U.S.
Naval Observatory.
The
Relationship between Length of Day and Temperature
Some of you may be wondering why the shortest day
of the year is not
normally the coldest day of the year. There is a lag
between the shortest day of the year and the coldest average temperatures
not only across New Mexico but for most of the mid and high
latitude locations. In the graph at the end of this section,
the length of daylight is plotted in red while the average daily
temperature
is
plotted
in blue, and the date of the solstice is depicted by yellow shading.
The sun angle is low before and after the winter solstice with a
minimum
number of daylight minutes
and
as
the
sun climbs
higher
in the
sky the length of daylight increases.
In Albuquerque, the minimum daily temperature occurs around 2 weeks
later in early January. This lag in temperature occurs because even
though
the minutes
of daylight are increasing, the earth's surface continues to lose
more energy that it receives from the sun. Average
temperatures continue to drop until the sun climbs higher in the
sky. While the effect is evident in the daily temperature plot, it
is more readily apparent by looking at changes in the monthly average
temperature (below and to the right). In Albuquerque, January averages
11.7F degrees less than December, with February also colder than
December by 6.0F, even though the days are longer.
Another interesting fact depicted in the graph below
is that while the solstice is the shortest day of the year, with 9
hours and 48 minutes of daylight in Albuquerque, it is just seconds
shorter than days on either side of the solstice. In fact, the U.S.
Observatory lists the length of daylight in Albuquerque (2007) as 9
hours and 48 minutes for December 16th through December 27th.
The Summer
Solstice, the Equinoxes and Season
We all know that the Earth makes a complete revolution
around the sun once every 365 days, following an orbit that is elliptical
in shape. This means that the distance between the Earth and sun,
which is 93 million miles on average, varies throughout the year.
During the first week in January, the Earth is about 1.6 million miles
closer to the sun. This is referred to as the perihelion. The
aphelion, or the point at which the Earth is about 1.6 million miles
farther away from the sun, occurs during the first week in July.
This fact may sound counter to what we know about seasons in the Northern
Hemisphere, but actually the difference is not significant in terms of
climate and is NOT the reason why we have seasons. Seasons are
caused by the fact that the Earth is tilted on its axis by 23.5°. This
can be seen graphically in the picture below.
The summer solstice occurs when the sun is directly
over the Tropic of Cancer, which is located at 23.5° North, and
runs through Mexico, the Bahamas, Egypt, Saudi Arabia, India, and southern
China. Because of the Earth's tilt, the sun was directly over
the Tropic of Cancer at 12:06 pm MDT on June 21, 2007. For every
place north of the Tropic of Cancer, the sun is at its highest point
in the sky and this is the longest day of the year. As stated above,
the winter solstice occurs when the sun is directly over the Tropic
of Capricorn, which is located at
23.5° South of the equator.
There are two times of the year when the Earth's axis
is tilted neither toward nor away from the sun resulting in an equal
amount of daylight and darkness at all latitudes. These events
are referred to as equinoxes and occur near March 21 (Vernal Equinox)
and near September 21 (Autumnal Equinox). At the equator, the sun
is directly overhead at noon on the two equinoxes. The Vernal Equinox
occurred at 6:07 pm MDT on March 20, 2007. The Autumnal Equinox
occurred at 3:51 am MDT on September 23, 2007.
National Weather Service
Albuquerque Weather Forecast Office
2341 Clark Carr LP SE
Albuquerque, NM 87106
Ph: 505.243.0702
Web Master's Email: ABQ Webmaster
Page Author: WFO Albuquerque, NM
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