In maritime navigation the horizon is not a perfectly flat line; the curvature of the Earth causes the visible sea horizon to lie slightly below the true geometric horizon. The angular distance between the true horizon and the visible line is called the dip of horizon.
The dip must be added to the observed altitude of a celestial body before it can be reduced to a true altitude. Failure to apply the dip leads to systematic errors in position fixes, especially when the observerβs eye is high above the water.
For a seaβlevel observer the dip can be approximated by a simple squareβroot relationship. The classic formula is expressed in minutes of arc as
h = height of eye above sea level (metres)
What is the dip of horizon in maritime navigation?
Why is it important to consider the dip of horizon in navigation?
How do I use this calculator to find the dip of horizon?
What is the formula used to calculate the dip of horizon?
Can this calculator be used for land navigation as well?
How does the dip of horizon vary with latitude?
What is the maximum possible dip of horizon?
Results are for informational purposes only and do not constitute professional advice.
