, inventor of the pendulum clock. Drawing is from his treatise
Horologium Oscillatorium, published 1673, Paris, and it records improvements to the mechanism that Huygens had illustrated in the 1658 publication of his invention, titled
Horologium. It is a weight-driven clock (the weight chain is removed) with a verge escapement (
K,
L), with the one-second pendulum (
X) suspended on a cord (
V). The large metal plate (
T) in front of the pendulum cord is the first illustration of Huygens' 'cycloidal cheeks', an attempt to improve accuracy by forcing the pendulum to follow a
cycloidal path, making its swing isochronous. The introduction of the pendulum, the first
harmonic oscillator used in timekeeping, increased the accuracy of clocks enormously, from about 15 minutes per day to 15 seconds per day The anchor became the standard escapement used in pendulum clocks. In addition to increased accuracy, the anchor's narrow pendulum swing allowed the clock's case to accommodate longer, slower pendulums, which needed less power and caused less wear on the movement. The seconds pendulum (also called the Royal pendulum), 0.994 m (39.1 in) long, in which each swing takes one second, became widely used in quality clocks. The long narrow clocks built around these pendulums, first made by William Clement around 1680, became known as
grandfather clocks. The increased accuracy resulting from these developments caused the minute hand, previously rare, to be added to clock faces beginning around 1690. The 18th- and 19th-century wave of
horological innovation that followed the invention of the pendulum brought many improvements to pendulum clocks. The
deadbeat escapement invented in 1675 by
Richard Towneley and popularised by
George Graham around 1715 in his precision "regulator" clocks gradually replaced the anchor escapement
Solar time is a calculation of the passage of
time based on the
position of the Sun in the
sky. The fundamental unit of solar time is the
day. Two types of solar time are apparent solar time (
sundial time) and mean solar time (clock time). Mean solar time is the hour angle of the mean Sun plus 12 hours. This 12 hour offset comes from the decision to make each day start at midnight for civil purposes whereas the hour angle or the mean sun is measured from the zenith (noon). The duration of daylight varies during the year but the length of a mean solar day is nearly constant, unlike that of an apparent solar day. An apparent solar day can be 20 seconds shorter or 30 seconds longer than a mean solar day. Long or short days occur in succession, so the difference builds up until mean time is ahead of apparent time by about 14 minutes near February 6 and behind apparent time by about 16 minutes near November 3. The
equation of time is this difference, which is cyclical and does not accumulate from year to year. Mean time follows the mean sun.
Jean Meeus describes the mean sun as follows: "Consider a first fictitious Sun travelling along the
ecliptic with a constant speed and coinciding with the true sun at the perigee and apogee (when the Earth is in perihelion and aphelion, respectively). Then consider a second fictitious Sun travelling along the
celestial equator at a constant speed and coinciding with the first fictitious Sun at the equinoxes. This second fictitious sun is the
mean Sun..." In 1936 French and German astronomers found that Earth's rotation speed is irregular. Since 1967
atomic clocks define the second. == Usage in metrology ==