az-amp.doc

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AMPLITUDES

Glasgow College of Nautical Studies                                           Faculty of Maritime Studies

 

AMPLITUDES

 

Amplitude refers to the bearing of a celestial body when it is rising or setting above the Rational Horizon, i.e. True Altitude = 00° 00.0'.                                                                         

NOTE An Amplitude of the sun is taken when the lower limb of the body is 1 semi-diameter above the visible horizon, allowing for the corrections this is when the sun has a True Alt 0°

An amplitude is the angle measured from the East / West line, to the body.

The Amplitude is named E or W depending on whether the body is rising or setting.

The Amplitude is named N or S depending on the Declination of the body.

              Sine Amplitude  =  Sine Declination

                                         Cosine Latitude

 

AZIMUTHS

The Azimuth is calculated using A, B, C Tables or by calculator it is a function of:

·         Latitude,

·                     Declination,

·                     LHA.

A =  Tan Lat                            Named opposite to Lat except when Hour Angle between 90° and 270°

       Tan LHA

 

B = Tan Dec                            Always named same as Declination.

       Sin LHA

 

C = A ± B                            + if A and B are the same names.

                                          -  if A and B are different names.

                                          C is named the same as the greater component.

 

Tan Azimuth =           1             

                                C x Cos Lat

 

Azimuth is named by C and LHA                 LHA 0° to 180° Body is to the West of the observer

                                                                         LHA 180° to 360° Body is to the East of the observer

 

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