Time  HourAngle Conversion Table
Longitude as part of our geographical coordinate system may be given both as
the intersecting angle between the Local Meridian and the Prime Meridian of Greenwich
expressed in Degrees (°) and MinutesofArc (')
or as a time difference between the Local Time and the Time at the Prime Meridian of Greenwich
expressed in Hours (h), Minutes (m) and Seconds (s).
Time is closely linked to the rotation of the Earth.
Over the time span of 24 hours, the Greenwich Hour Angle of the Sun increases by 360°.
This implies an increase of 15° per hour.
Since local time is basically based on mean solar time, locations having
15° of Longitude difference, will have exactly 1 hour of local time difference.
Purpose and Scope
The Time  HourAngle Conversion Table tabulates the relationship between
Time and HourAngle as used as part of the celestial coordinate system.
HA Time
15° ~ 1h
1° ~ 4m
15' ~ 1m
1' ~ 4s 

This relationship allows to translate local time differences into Longitude differences and vice versa.
It also shows that on the spring and autumn equinoxes, when the Geographical Position of the Sun is
located on the Equator, the Geographical Position is "moving" at a speed of 15 nautical miles / minute
or 1 nautical mile / 4 seconds. 
Table

The Time  HourAngle Conversion Table gives the relation between Time and HourAngle for integral values
of the HourAngle.
Time is given in 4minute intervals.
The information for the fractional values of the HourAngle can be obtained from the first pages
of the Interpolation Tables for Celestial Navigation
(Pages "0Min"  "3Min": the column "dHA" gives the increment of HourAngle for the mean 15°/h GHA
increment of the Sun corresponding to the Time entry).

The table for the Time  HourAngle Conversion is also available from the precompiled
Interpolation Tables for Celestial Navigation (page 35).
Application of the Time  HourAngle Conversion Table
The standard application of this Time  HourAngle conversion is the translation of the
observed local noon time into the corresponding Longitude.
However, the table can also be useful for the determination of
Rise Time and Set Time of celestial objects.
Example 1: finding Longitude from Culmination Time
On Aug 23. 2001 at a location with unknown Longitude, it is observed that
local noon occurs at 03h 08m UT.
At this moment the Sun attains the highest altitude above the horizon and thus the
Geographical Position of the Sun is located on the local Meridian.
From the Nautical Almanac it can be read that on Aug 23. 2001 the Greenwich Culmination Time is:
Tculmination = 12h 03m (UT).
At the unknown position the Culmination Time is about 9 hours earlier, so this location must
be East of Greenwich. The exact time difference is:
Tdlocal = ( 03h 08m )  ( 12h 03m ) =  ( 08h 55m ).
The Time  HourAngle Conversion Table
(take the nearest entry lower than 08h 55m : "08:52") gives the following equivalence:
08:52 ~ 133° 00.0'
The result for the remaining 03 minutes has to be looked up in the
Interpolation Tables for Celestial Navigation
(entry "03 Min / 00 Sec", data column "dHA" on page 11):
00:03 ~ 45.0'
Adding the results together yields:
08:55 ~ 133° 45.0'
So the Longitude corresponding to 03h 08m UT local Culmination Time on Aug 23. 2001 is:
133° 45.0'
Notices:
Since the time differences between local Culmination Time and Greenwich Culmination Time
cannot be simply determined more accurately than 1 minute of time, the longitude accuracy obtained
in this way is limited to 15' (corresponding to 15 nautical miles on the Equator or less on
higher Latitudes).
The above method of finding Longitude with the time of local culmination, can be performed
with other celestial objects (Moon or Planets) of which the Greenwich Culmination Time is known.
Example 2: finding local rise or set times
In the next example the (local) time of sunrise on Aug 23. 2001
at location S 24° 37.4' E 079° 41.8' will be elaborated.
The Greenwich Culmination Time on this date is found in the Nautical Almanac:
Tculmination = 12h 03m (UT).
Also the Declination of the Sun at noon time (12:00 UT) can be found here:
DecSun = N 11° 19'4
Next the Longitude 079° 41.8' is translated into a time difference against the
Greenwich local time.
The Time  HourAngle Conversion Table
gives the time equivalent of 079°:
079° ~ 05h 16m 00s.
The rest of the time, corresponding to the remaining 41.8' of longitude, can be found in the
Interpolation Tables for Celestial Navigation.
Look for the dHA entry nearest to 41.8' (in the "2Min" column at page 10):
41.8' ~ 00h 02m 47s.
So the Longitude of E 079° 41.8' corresponds to a time lead
(Eastern Longitude = negative "Tdlocal") of:
Tdlocal =  ( 05h 16m 00s + 00h 02m 47s ) =  ( 05h 18m 47s )
compared to Greenwich time.
So at the given location, local noon will occur a little bit more than 5¼ hours before
Greenwich noon.
In order to find the time of sunrise, half the "lengthoftheday" must be subtracted from this time.
This "halfthelengthoftheday" value is obtained from the Sight Reduction Tables.
Look in the "CONTRARY" pages at the entry for S 24° Latitude (given Latitude = S 24° 37.4')
and N 11° Declination (for DecSun = N 11° 19'4) and then search
for the line at which the Altitude is zero (H=0). The Local HourAngle (LHA) for this combination is:
LHAH=0 = 85°
According to the Time  HourAngle Conversion Table these 85° correspond to a time difference of:
Tdh = 05h 40m
Adding the appropriate values as in the following scheme, gives a first iteration value of the
(local) time of sunrise:
Trise = Tculmination  Tdh + Tdlocal
Trise = ( 11h 46m 00s )  ( 05h 40m 00s )  ( 05h 18m 47s )
Trise = ( 11h 46m 00s )  ( 10h 58m 47s )
Trise = ( 10h 105m 60s )  ( 10h 58m 47s )
Trise = ( 00h 47m 13s )
This is only a first approximation because the Declination value for 12:00 UT was used and this will
be slightly different from the value for 00:47 that should have been used. However these changes are
small and for normal use, this first approximation will be sufficiently accurate.
So sunrise on Aug 23. 2001 the given position (S 24° 37.4' E 079° 41.8') can be expected at:
00h 47m (UT).
As mentioned, this is only a first iteration because integer values for Declination and Latitude
were used in the Sight Reduction Tables. Also the Declination value for 12:00 UT was used
and this will be slightly different from the value for 00:47 that should have been used.
However these changes are small and for normal use, this first approximation will be sufficiently
accurate.
For a second iteration, the Declination value of the Sun at 00h 47m 12s must be interpolated from the
Nautical Almanac and used as entry in the Sight Reduction Tables for determining the
value of Tdh ("halfthelengthoftheday" period), which also requires some interpolation, since
the Sight Reduction Tables have only integer values for Declination and Latitude.
Similar to the time of sunrise, the time of sunset can be determined by:
Tset = Tculmination + Tdh + Tdlocal
