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Time Converter

Convert between various time units from microseconds to centuries. Includes common time formats, decimal time, and scientific notation for precise measurements.

About Time Converter

The History of Time Measurement

Time measurement has been fundamental to human civilization since its earliest days. Ancient civilizations tracked time using natural phenomena like the Sun's position and seasonal changes. The Egyptians divided day and night into 12 parts each, giving us the 24-hour day. The Babylonians' sexagesimal (base-60) system gave us minutes and seconds. From sundials to atomic clocks, our methods of measuring time have evolved dramatically, reflecting humanity's quest for ever-greater precision.

Common Time Units

UnitEqual ToCommon Uses
SecondSI base unitScientific measurement
Minute60 secondsDaily scheduling
Hour3600 secondsWork/activity planning
Day86400 secondsCalendar events

The Second: Our Base Unit

Modern Definition

The second is defined as the duration of 9,192,631,770 periods of the radiation corresponding to the transition between two hyperfine levels of the ground state of the cesium-133 atom at absolute zero temperature.

Historical Definitions

  • Ancient: 1/86400 of a mean solar day
  • 1956: 1/31,556,925.9747 of the tropical year
  • 1967: Current atomic definition adopted
  • 1997: Definition refined for cesium at absolute zero

Specialized Time Units

Scientific

  • Nanoseconds: Computer processing
  • Milliseconds: Network latency
  • Microseconds: High-speed photography
  • Planck time: Theoretical physics

Calendar

  • Fortnight: Two weeks
  • Quarter: Three months
  • Decade: Ten years
  • Century: Hundred years

Modern Time Measurement

Modern time measurement spans from the infinitesimal to the cosmic. Atomic clocks measure time with incredible precision, losing less than a second over millions of years. GPS satellites carry atomic clocks and must account for relativistic time dilation. In particle physics, events are measured in nanoseconds or shorter. Geologists and astronomers deal with billions of years when studying Earth's history and the universe's evolution. Each scale requires different measurement techniques and considerations.