Sidereal Time Calculator

Calculate local and Greenwich sidereal time for astronomical observations.

Current Time

Local: 9/29/2025, 2:54:47 AM

Select date and time for calculation

Select hemisphere for longitude

Enter longitude in degrees, minutes, and seconds (e.g., 100° 3' 30") for local sidereal time calculation

Methodology

This calculator uses standard astronomical algorithms based on the J2000.0 epoch. GMST is calculated using the IAU polynomial formula, and GAST includes nutation corrections via the equation of equinoxes. Local sidereal times are computed by adding the longitude correction in hours.

About This Calculator

1. What is the difference between mean and apparent sidereal time?

Mean sidereal time assumes uniform Earth rotation, while apparent sidereal time includes corrections for nutation (small wobbles in Earth's axis caused by gravitational effects of the Sun and Moon). The difference is typically less than 1 second.

2. Why is sidereal time important for astronomy?

Sidereal time directly relates to the position of stars in the sky. Combined with a celestial object's right ascension, it determines the object's hour angle, which tells astronomers when and where to find objects in the sky.

3. How accurate are these calculations?

The calculations use standard astronomical algorithms with accuracy suitable for most amateur astronomy applications. For professional precision, more complex nutation models and atmospheric corrections would be needed.

4. What is the equation of equinoxes?

The equation of equinoxes is a correction that accounts for nutation effects on the position of the vernal equinox. It's the difference between apparent and mean sidereal time, typically ranging from -1.2 to +1.2 seconds.