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焦熱の日

Solar Navigation Calculations

Calculation of the Hour Angle and Declination of the Sun

Determine the Sun’s hour angle and declination
for January 1 at 01:20 UTC.

SUN_GHA.jpg
4.英語1-1_SUN.jpg

Step 1  
Identify the value of E◉ in the Nautical Almanac that immediately precedes the observation time.

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Step 2  
Since E◉ is tabulated at two-hour intervals, the value at the desired time can be obtained by interpolation.

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Step 3  
Add the observation time (UTC) to the value of E◉ obtained in Step 2 to determine the hour angle.

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Step 4  
Since the hour angle is expressed in time units, convert it to angular degrees by multiplying by 15.

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Step 5  
For declination, determine the value corresponding to the observation time.  
Apply the appropriate P.P. correction obtained from the right-hand column to derive the solar declination.

Calculation of the Meridian Passage Time of the Sun

Determine the meridian passage time on January 1 at longitude 140°E.

MP.jpg
4.英語1-1_SUN.jpg

Step 1  
At meridian passage, the Local Apparent Time (LAT) of the Sun is always 12h00m00s.

Step 2  
Longitude time is obtained by dividing the longitude by 15.  
Add the longitude time for east longitude, and subtract it for west longitude.

Step 3  
Using this longitude correction, obtain the Greenwich Apparent Time (GAT).  
From this time, determine the corresponding value of E◉ from the Nautical Almanac.

Step 4  
Since E◉ is tabulated at even-hour intervals, the value at the desired time can be obtained by interpolation.

Step 5  
The equation of time is obtained by subtracting 12h00m00s from E◉.

Step 6  
Greenwich Mean Time (GMT) is obtained by applying the equation of time to GAT.  
(Note: the sign of the equation of time is reversed.)

Step 7
Local Mean Time (LMT) is obtained by applying the longitude correction or standard time correction.
For this correction, subtract in the case of east longitude and add in the case of west longitude.

Step 8  
An approximate meridian passage time M.P.(LMT) can also be obtained from the value labeled M.P. in the Sun column of the Nautical Almanac.

Correction of the Observed Altitude of the Sun

SUN_CORR.jpg
気温ー気圧改正_ページ_1(英語).jpg
気温ー気圧改正_ページ_2(英語).jpg
太陽低高度改正.jpg
太陽高高度改正.jpg

Case 1  
For altitudes between 0° and 40°,  
both the first and second corrections shall be applied.


Case 2  
For altitudes above 40°,  
these corrections are not required.

Step 1  
Apply the index error (IE) of the sextant to the sextant altitude (As), and use the resulting value as the basis for subsequent corrections.

Step 2  
Using the Solar Altitude Correction Table, obtain the required correction values based on the altitude obtained in Step 1 and the observed height of eye.  
(Example: height of eye = 10 m, altitude = 55°)

Step 3  
Correction No. 4 accounts for the variation of the Sun’s horizontal parallax throughout the year.  
Apply the corresponding correction value from the table for each month.

Step 4  
Correction No. 5 accounts for the difference between air temperature and water temperature.  
Determine the temperature difference and apply the corresponding correction value from the table.

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