Here is a comparison of the
relative day lengths (number of hours of daylight) in different cities (of varying
latitudes) on three dates in 1998.
City/Latitude |
|
March
21 |
June
21 |
December
21 |
|
Honolulu,
HI
21� N |
sunrise sunset
day length |
6:34 am
6:43 pm
12 hrs 9 min |
5:50 am
7:16 pm
13 hrs. 26 min |
7:04 am
5:55 pm
10 hrs. 51 min |
|
Raleigh,
NC
35� N |
sunrise sunset
day length |
6:17 am
6:27 pm
12 hrs. 10 min |
4:59 am
7:34 pm
14 hrs. 35 min |
7:21 am
5:05 pm
9 hrs. 44 min |
|
Burlington,
VT
44� N |
sunrise sunset
day length |
5:55 am
6:06 pm
12 hrs. 11 min |
4:08 am
7:41 pm
15 hrs. 33 min |
7:26 am
4:16 pm
8 hrs. 50 min |
|
Barrow,
AK
71� N |
sunrise sunset
day length |
7:20 am
7:51 pm
12 hrs. 31 min |
Sun never goes below horizon
24 hrs |
Sun never gets above horizon
0 hrs |
You can see that on March 21, the spring
equinox, all the cities listed have approximately 12 hours of sunlight. On June 21, the
summer solstice and longest day of the year for the northern hemisphere, the day length
ranges from about 13 � hours in Hawaii to 24 hours in northern Alaska. On December 21,
the shortest day of the year, the day length ranges from almost 11 hours in Hawaii to 0
hours in Northern Alaska.
This diagram shows the earths position relative to
the sun on the summer solstice in the northern hemisphere. The summer
solstice is the longest day of the year (that is, the day with the most hours of
daylight). When it is the summer solstice in the northern hemisphere, it is the winter
solstice in the southern hemispherethe shortest day of the year.
Remember that for the earth:
- one day equals one complete revolution on its axis.
- one year equals one complete orbit around the sun.
On the diagram youll see that the earths axis
of rotation isnt perpendicular to the sun. Rather, the earths axis is tipped
at a 23.5 degree angle. This angle remains constant as the earth orbits the sun. When the
northern hemisphere is tipped toward the sun, it is summer there. Six months later, when
the earths orbit reaches the other side of the sun, the northern hemisphere will be
tipped away from the sun, and it will be winter.
Find the equator on the diagram. Moving north, weve
labeled the latitudes of Honolulu, Hawaii, Burlington, Vermont, and Barrow, Alaska. South
of the equator, in the southern hemisphere, youll find Hamilton, Australia.
Following are these cities latitudes, from northermost to southermost:
- Barrow, Alaska: 71 degrees North
- Burlington, Vermont: 44 degrees North
- Honolulu, Hawaii: 21 degrees North
- Equator: 0 degrees
- Hamilton, Australia: 38 degrees South
Note the shading on the "dark side of the
earth"the half of the planet that is not receiving sunlight.
Now lets put all these factors together to show the
difference in relative day lengths of each of these cities. The dark lines indicate the
portion of the day that is in daylight. The dotted/dashed line indicates the portion that
is in darkness.
Lets start with Alaska. You can see from the diagram
that at no time of the earths revolution is Alaska out of the daylight. On this day,
the sun never setsthe "day length" is 24 hours!
Moving south, you can see that most of Vermonts day
is lit by sunlight; only a small percentage of the day, maybe one third, is in darkness.
On the summer solstice, Vermonts daylength is 15.5 hours.
In Hawaii, slightly more than half the revolution is in
daylight, or 13.5 hours.
In Australia, less than half the revolution receives
daylight, only 9 hours.
The purpose of all this is to show that day
length, or number of hours of daylight, varies dramatically with latitude at certain times
of the year. The further you get from the equator, the more dramatic the difference in the
number of hours of daylight during the longest and shortest days of the year.
Now lets look at another factor besides
day length that influences the onset of flowering.
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Note: See the
last page for a link to a web site with a chart showing the time of sunrise and sunset for
cities across the U.S. for any year. |
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