The Planet Earth
The earth is in constant motion. Being a planet, it travels
around the sun in roughly 365 days, turning around itself once every 24 hours
during its solar orbit.
These two motions, the orbit of the earth around the sun within the period of
one year and its rotation around itself within 24 hours, constitute the basis
for the determination of time.
The Planet Earth Illuminated globe incorporates a number of
novel features permitting the two motions of the earth to be demonstrated and
distinguishing this globe from any other type of globe currently available.
The base of the globe is provided with a scale that adjusts to each day of the
year. The ring surrounding the equator and dividing the globe into the Northern
and Southern hemispheres is designed as a dial divided into the 24 hours of the
day and including quarter-hour intermediate divisions.
When the interior light of the globe is switched on, the globe appears divided
into two halves: one illuminated, the other not. The illuminated half represents
the day-side while the non-illuminated half is the night-side of the earth.
The annual scale
By turning the scale, the globe can be set to each day of
the year. The index mark on the non-revolving base shows the day set. When
slowly turning the annual scale with the light on, the globe shows the movement
of the line separating the day-side and the night-side. This constant movement
of the line of light, which does not repeat itself until after the passing of
one year, after one complete revolution of the earth about the sun, that is,
accounts for what occurs in nature. The globe shows the position of the earth in
space on its path around the sun. Day for day the earth changes its position
with respect to the sun until the cycle is repeated after 365 days.
The time of day
While one motion of the earth, its orbit around the sun, is
demonstrated by the annual scale of the globe, the second motion, the rotation
of the earth around its axis, is shown by the equator ring, with its effect upon
the time of day appearing directly on the globe.
Due to the close relationship existing between the rotation of the globe and the
time of day, there must be kept in mind that any rotary movement of the globe
signifies a change in time; a quarter turn equals 6 hours, a half-turn 12 hours,
and a complete turn 24 hours.
Since all areas of the earth situated on one meridian have the same time, this
also applies to the globe. The meridians are blue lines on the map and lead from
the North Pole to the South Pole; they are drawn at intervals of ten degrees and
numbered below the equator. Read the time of each meridian where the line of
that meridian cuts the equator.
Reading the time of day
First of all, it is advisable to keep in mind that on every
day of the year all times of the day are present both on the earth and also on
the globe at the same time: When it is midnight in Europe, the sun of
high noon is shining at the same time over the Pacific Ocean, the sin is
rising in some areas of Russia, and is at the same time setting in some
areas of the United States. Consequently, any moment of time applies to only a
limited area. To read the time of day applying to that limited area at ay
moment, all you have to do is read the time indicated on the dial of the equator
ring for each meridian.
Along the line dividing day and night, the globe--when
illuminated, shows the three bright rings illustrating the zones of dawn and
dusk, the twilight before sunrise and after sunset. In nature, the gradual
passage between day and night occurs without steps. However, to identify the
different degrees of illumination while the twilight persists, the three circles
outline the following stages:
1st stage: Civil Twilight is recognized as beginning
or ending when the sun is about 6
below the horizon, and is determined by the amount of light necessary to permit
2nd stage: Nautical Daylight begins or ends when
the sun is 12 below the horizon, the illumination being then so poor that the
horizon can no longer be seen.
3rd stage: Astronomical Twilight begins or ends
when the sun reaches 18 below the horizon, and when no reflections of the sun's
light illuminate the nightly sky.
For the daybreak, the values come in reverse order.
As already described in the paragraph
Reading the time of day, the Planet Earth globe permits demonstrating the
course of the 24 hours of the day. Each complete rotation of the globe ball
about its axis equals the passing of 24 hours.
A glance at the dial of the equator ring shows that every two hour-division on
the dial include 15 meridians, which are represented in the map as blue lines
spaced 10 degrees apart. The time difference for every ten degrees is 40
The time that can be read on the globe for every place on earth along a meridian
is called local time.
In order to be able to read other standard times, such as the Central
European Time (CET) on the globe, you need some additional explanations.
Central European Time
Since large, economically interrelated areas
require a uniform time for reasons of traffic and communication, such areas have
been combined in time zones. Central Europe is one of these time zones. The
official time commonly agreed upon for this area is the local time of the
15th degree of Eastern longitude, which cuts right through the middle of
Central Europe. Read the Central European Time (CET) on the dial of the equator
ring midway between the 10 and 20 meridians. In this context it must be pointed
out that all local times the globe indicates for the large area of
Central Europe remain additionally applicable. Occasionally, the times of
sunrise and sunset published in pocket almanacs are indicated in local time
because the time differences with respect to standard time tend to cause
substantial errors. After all, the difference in apparent or local time between
the western and eastern regions of Central Europe is almost two hours.
Division in time zones
The illustration above shows the pattern
permitting vast regions with different local times to be combined, in a simple
manner, in time zones having the same standard time. For this, the surface of
the earth has been divided into 24 zones extending along the meridians. Each
zone has a width of 15 degrees, so that the local time within one zone differs
by exactly one hour between the two extremes. The time generally applicable
within each zone is the local time of the meridian in the middle of each zone.
This system assures that the local times within each zone differ by not more
than a maximum of thirty minutes from the standard time. Moreover the change in
time when entering the neighboring time zone is exactly one hour.
However, a look at the CET area, which extends over two zones,
shows that such a system can hardly be reconciled with the practical
requirements of the land areas of the world.
Division of land areas in time zones
As mentioned before, reasons of traffic and communication
make it necessary to have a common time for economically and politically
interrelated areas. The map shows how the various areas, based on the
aforementioned schematic pattern, are divided into time zones.
The standard time system has been introduced by nearly all countries of the
world by appropriate legislation. A number of countries, especially for economic
reasons, have adopted a Summer Time (or Daylight Savings Time) for the summer
half-year, with the clocks being advanced by one hour.
The subsolar area I
With the globe illuminated, a bright dot of light will be
seen near the 12 o' clock mark of the dial on the equator ring. This light spot
marks the area in which the sun's rays cast no shadow in the surface of the
earth at 12:00 hours: It is the time when the sun is directly overhead and the
respective area is directly below the sun. This is why that area is
called subsolar area.
Turn the globe and you will note that ever new areas of the earth will reach the
dot of light and become subsolar areas for a short while.
Since the sun must be considered to be vertically above the dot of light on
the surface of the earth, the observer will (after a little practice) soon
be able to estimate the altitude or position of the sun in any region of the
earth and on any day of the year.
The subsolar area II
The Tropic of Cancer and The Tropic of Capricorn
are delineated on the globe with a dotted line, which runs parallel to the
equator. The Tropic of Cancer is
found north of the equator, and the Tropic of Capricorn
can be found to the south of the equator. The names have been adopted from olden
times; they refer to the perceived path of the sun and stand for the respective
Signs of the Zodiac. However, these zodiacal constellations are no longer
correct because the apparent path of the sun has changed.
The dot of light of the subsolar area reveals the significance of the tropics.
When the annual scale is turned, the light dot will travel between the tropics
and turn back after having reached the dotted lines. The annual scale
then indicates the time of the summer solstice on June 21, or of the
winter solstice on December 21.
The International Dateline
To understand the significance and function of the
dateline, find the dateline on the globe. It is a dotted line leading from the
North Pole to the South Pole opposite the zero-meridian. Whenever the dateline
is crossed, regardless of whether this be from the east to the west or tin the
opposite direction from the west to the east, the date must be changed. So, for
example, when it's Thursday, May 6th on one side of the dateline, it's
Wednesday, May 5th on the other side.
The simultaneous existence of two different dates is absolutely necessary to
permit a uniform date to be counted for the population of the world. For
an explanation of this seemingly paradoxical statement turn the globe ball to
have the dateline below the 0:00 mark of the world. In this position, the same
date is used throughout the world, say Wednesday, May 5. But to keep the date
applicable, all areas of the world crossing the 0:00 mark must use the new date
beginning on 0:01: Thursday, May 6th. As a consequence, the inhabitants of the
Hawaii Islands will witness the forthcoming sunrise on Wednesday, May 5, while
their neighbors on the Marshall Islands will date the same sunrise as Thursday,
May 6th. at 0:00 o' clock. But shortly thereafter the same process will be
repeated: On the Marshall Islands the new date, Friday, May 7th, will commence.
The existence of two different dates at the same time of significance only for
those who cross the border or dateline. It makes no difference on what day or at
what time of day the dateline is crossed.
Travel agencies offer an attractive air travel arrangement: Anyone wanting to
celebrated New Year's Eve on the Fiji Islands is offered a flight to the Hawaii
Islands on the course of January 1st. Upon arriving in Hawaii the date is still
December 31st, and one has another chance to celebrate the arrival of the new
For the occupants of a spaceship, the repeated crossing of the dateline within
24 hours is of no significance. What counts is only the date that has been
adopted at the place of the landing in the course of the flight.
Click here to return to the
Planet Earth Globe.