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For the date
and time selected by the menus the declination and the local hour angle
Sun (LAH) are computed by numerical astronomical algorithms and
transferred to the geometrical construction. The altitude and azimuth
angle are the results
of the graphical construction, drawing Thales' circle using the
diameter of the altitude circle (parallel to the horizon) and the
diameter of the declination
circle (parallel to the celestial equator).
Setting the Sun below the horizon the times of sunrise and sunset can be read. |
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Select
your
location from the menu list, or
|
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Press the "now"
button to get the current position of the Sun. |
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Select from the
Details menu to show or hide items. |
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Check the boxes
to see the construction
by Thales' circle
. |
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The azimuth angle is measured eastwards of North: 0°
=
N,
90°
=
E,
180°
=
S,
270°
=
W
|
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You
may
use
the keys "m", "d", "h", "n" to increase
the month, day, hour, or minute, |
The observer is located at the centre of his "celestial sphere" with zenith Z above his head and the horizon plane N-E-S-W. The Sun rises at (1), moves along the red arc, passing the meridian NZS at (2), and sets at (3). This path is called the diurnal arc of the sun. ![]() Projecting the diurnal arc (circle of declination) of the Sun and the horizontal plane into the NZS plane, they are seen as straight lines intersecting at (1)=(3). The diurnal arc (declination circle) of the sun varies with the seasons:
There are two reasons for
the difference between the standard time and the solar time. To convert
solar time to standard time:
- add 4 minutes per degree west of the time zone meridean, and subtract if east, and take into account daylight saving time. For Berlin - time zone meridian 15° E and longitude 13.41° E, add 1.59*4 min = 6.4 minutes. - subtract the equation of time, due to the elliptic orbit of the earth around the Sun and the obliquity of the ecliptic (23.44°).
![]() The moment of sunrise is usually defined by the instant
when
the center of the sun is -0.83° below horizon (taking into account
the refraction of light by the atmosphere of the earth and the apparent
diameter of the Sun). For a latitude
of 50° this equivalent to a time interval of 5 to 7 minutes. As shown below the construction is in agreement with
the equation known from spheric trigonometry: (1) sin h = sin φ sin δ + cos φ cos δ cos τ (2) cos Az = (sin δ - sin φ sin h)/(cos h cos φ)
φ
= Latitude, h = Altitude, δ = Declination, τ = Local Hour Angle LHA (1) We start
computing a, the difference between the vertical lines a =
R
sin
(90°-φ+δ) - R sin h
a = x sin
(90°-φ) = x cos φ sin h = sin φ sin δ + cos φ cos δ cos τ
φ
= Latitude, h = Altitude, δ = Declination, τ = Local Hour Angle LHA (2) We start computing b, the difference between the vertical lines b = R sin (90°-φ+δ) - R sin h = x tan (90°-φ) x = a - r cos
(180°-az) R sin (90°-φ+δ) - R sin h = [R sin (φ-δ) + R cos h cos az] tan (90°-φ) sin (90°-φ+δ) - sin h = (sin (φ-δ) + cos h cos az) tan (90°-φ)
sin (90°-φ+δ) - sin h = sin (φ-δ) + cos h cos az] cos φ/sin φ cos φ cos δ + sin φ sin δ - sin h = [sin φ cos δ - cos φ sin δ + cos h cos az] cos φ/sin
φ sin φ cos φ cos δ + sin2 φ sin δ - sin φ sin h = [sin φ cos δ - cos φ sin δ + cos h cos az] cos φ
sin φ cos φ cos δ + sin2
φ sin δ - sin φ sin h = cos φ sin φ cos δ - cos2 φ sin δ + cos φ cos h cos az sin2 φ sin δ - sin φ sin h = - cos2 φ sin δ + cos φ cos h cos az sin δ - sin φ sin h = cos φ cos h cos az sin δ - sin φ sin h = cos φ cos h cos az cos Az = (sin δ - sin φ sin h)/(cos h cos φ) Both equations (1 and 2) can also be
found within the construction of my applet Quadratum Horarium Generale
(Regiomontanus Dial). |
Books |
Kurt
Hoffmann: Sterne, Mond und Sonne: Astronomie ohne
Fernrohr; Eva Hoffmann Verlag, Stuttgart 1999, ISBN 3-932001-03-6. |
|
Table
of
Sunrise/Sunset, Moonrise/Moonset, or Twilight Times for an Entire
Year Astronomical
Almanac from 1998 to 2059 Daylight Applet: Table of sunrise, sunset and twilight times |
Please visit my GeoAstro Applet Collection
Last modified: 2010, Jul 01
© 2001-2009 Juergen Giesen