The Julian date (JD) is the interval of time in days and fractions of a day, since 4713 B.C. January 1, Greenwich noon, Julian proleptic calendar. In precise work, the timescale, e.g., Terrestrial Time (TT) or Universal Time (UT), should be specified.
The Julian day number (JDN) is the integral part of the Julian date (JD). Negative values can also be used, although those predate all recorded history. Now, at the Julian day number is .
A Julian date of 2454115.05486 means that the date and Universal Time is Sunday January 14, 2007 at 13:18:59.9.
The decimal parts of a Julian date:
0.1 = 2.4 hours or 144 minutes or 8640 seconds
0.01 = 0.24 hours or 14.4 minutes or 864 seconds
0.001 = 0.024 hours or 1.44 minutes or 86.4 seconds
0.0001 = 0.0024 hours or 0.144 minutes or 8.64 seconds
0.00001 = 0.00024 hours or 0.0144 minutes or 0.864 seconds.
Almost 2.5 million Julian days have elapsed since the initial epoch. JDN 2,400,000 was November 16, 1858. JD 2,500,000.0 will occur on August 31, 2132 at noon UT.
If the Julian date of noon is applied to the entire midnight-to-midnight civil day centered on that noon, rounding Julian dates (fractional days) for the twelve hours before noon up while rounding those after noon down, then the remainder upon division by 7 represents the day of the week, with 0 representing Monday, 1 representing Tuesday, and so forth. Now at the nearest noon JDN is yielding a remainder of .
The Julian day number can be considered a very simple calendar, where its calendar date is just an integer. This is useful for reference, computations, and conversions. It allows the time between any two dates in history to be computed by simple subtraction.
The Julian day system was introduced by astronomers to provide a single system of dates that could be used when working with different calendars and to unify different historical chronologies. Apart from the choice of the zero point and name, this Julian day and Julian date are not directly related to the Julian calendar, although it is possible to convert any date from one calendar to the other.
Historical Julian dates were recorded relative to GMT or Ephemeris Time, but the International Astronomical Union now recommends that Julian Dates be specified in Terrestrial Time, and that when necessary to specify Julian Dates using a different time scale, that the time scale used be indicated when required, such as JD(UT1). The fraction of the day is found by converting the number of hours, minutes, and seconds after noon into the equivalent decimal fraction.
The term Julian date is also used to refer to:
The use of Julian date to refer to the day-of-year (ordinal date) is usually considered to be incorrect, however it is widely used that way in the earth sciences and computer programming.
Because the starting point is so long ago, numbers in the Julian day can be quite large and cumbersome. A more recent starting point is sometimes used, for instance by dropping the leading digits, in order to fit into limited computer memory with an adequate amount of precision.
|Name||Current Epoch||Calculation||Current Value||Notes|
|Julian Date (JD)||BC 4713-01-01 12:00, Monday|
|Julian Day Number (JDN)||BC 4713-01-01 12:00, Monday||JDN = floor (JD)||Changes at noon UT or TT|
|Chronological Julian Day (CJD)||BC 4713-01-01 00:00, Monday||JDN = floor (JD + 0.5)||(UT)||Specific to time zone; UT CJD given|
|Reduced Julian Day (RJD)||1858-11-16 12:00, Tuesday||RJD = JD − 2400000||Used by astronomers|
|Modified Julian Day (MJD)||1858-11-17 00:00, Wednesday||MJD = JD − 2,400,000.5||Introduced by SAO in 1957|
|Truncated Julian Day (TJD)|| 1968-05-24 00:00, Friday|
1995-10-10 00:00, Tuesday
| TJD = JD − 2440000.5|
TJD = (JD − 0.5) mod 10000
| || - Definition as introduced by NASA |
- NIST definition
|Dublin Julian Day (DJD)||1899-12-31 12:00, Sunday||DJD = JD − 2415020||Introduced by the IAU in 1955|
|Lilian Day Number||1582-10-15, Friday (as Day 1)||floor (JD - 2299160.5)||The count of days of the Gregorian calendar for Lilian date reckoned in Universal time.|
|ANSI Date||1601-01-01, Monday (as Day 1)||floor (JD - 2305812.5)||The origin of COBOL integer dates|
|Rata Die||0001-01-01, Monday (as Day 1)||floor (JD - 1721425.5)||The count of days of the Common Era (Gregorian)|
|Unix Time||1970-01-01, Thursday||(JD – 2440587.5) × 86400||Counts by the second, not the day|
The Heliocentric Julian Day (HJD) is the same as the Julian day, but adjusted to the frame of reference of the Sun, and thus can differ from the Julian day by as much as 8.3 minutes, that being the time it takes the Sun's light to reach Earth. The Julian day is sometimes referred to as the Geocentric Julian Day (GJD) in order to distinguish it from HJD.
The Julian day number is based on the Julian Period proposed by Joseph Scaliger in 1583, at the time of the Gregorian calendar reform, but it is the multiple of three calendar cycles used with the Julian calendar:
Its epoch falls at the last time when all three cycles were in their first year together — Scaliger chose this because it pre-dated all historical dates.
Note: although many references say that the Julian in "Julian day" refers to Scaliger's father, Julius Scaliger, in the introduction to Book V of his Opus de Emendatione Temporum ("Work on the Emendation of Time") he states, "Iulianum vocavimus: quia ad annum Iulianum dumtaxat accomodata est", which translates more or less as "We have called it Julian merely because it is accommodated to the Julian year." This Julian refers to Julius Caesar, who introduced the Julian calendar in 46 BC.
In his book Outlines of Astronomy, first published in 1849, the astronomer John Herschel wrote:
The first year of the current Julian period, or that of which the number in each of the three subordinate cycles is 1, was the year 4713 B.C., and the noon of the 1st of January of that year, for the meridian of Alexandria, is the chronological epoch, to which all historical eras are most readily and intelligibly referred, by computing the number of integer days intervening between that epoch and the noon (for Alexandria) of the day, which is reckoned to be the first of the particular era in question. The meridian of Alexandria is chosen as that to which Ptolemy refers the commencement of the era of Nabonassar, the basis of all his calculations.
Astronomers adopted Herschel's Julian Days in the late nineteenth century, but used the meridian of Greenwich instead of Alexandria, after the former was adopted as the Prime Meridian after the International Meridian Conference in Washington in 1884. This has now become the standard system of Julian days. Julian days are typically used by astronomers to date astronomical observations, thus eliminating the complications resulting from using standard calendar periods like eras, years, or months. They were first introduced into variable star work by Edward Charles Pickering, of the Harvard College Observatory, in 1890.
Julian days begin at noon because when Herschel recommended them, the astronomical day began at noon (it did so until 1925). The astronomical day had begun at noon ever since Ptolemy chose to begin the days in his astronomical periods at noon. He chose noon because the transit of the Sun across the observer's meridian occurs at the same apparent time every day of the year, unlike sunrise or sunset, which vary by several hours. Midnight was not even considered because it could not be accurately determined using water clocks. Nevertheless, he double-dated most nighttime observations with both Egyptian days beginning at sunrise and Babylonian days beginning at sunset. This would seem to imply that his choice of noon was not, as is sometimes stated, made in order to allow all observations from a given night to be recorded with the same date.
The Julian day number can be calculated using the following formulas:
The months January to December are 1 to 12. Astronomical year numbering is used, thus 1 BC is 0, 2 BC is −1, and 4713 BC is −4712. In all divisions (except for JD) the floor function is applied to the quotient (for dates since 1 March −4800 all quotients are non-negative, so we can also apply truncation).
For a date in the Gregorian calendar (at noon):
For a date in the Julian calendar (at noon):
The constants used at the end of the Gregorian and Julian formulas are required to return the same JDN for the same date in both calendars between March 1, 200 and February 28, 300. The constants are the JDNs of February 29, −4800 in each calendar. In the proleptic Gregorian calendar the Julian day zero is November 24, 4714 BC which is 32045 days apart from the start of the Gregorian quadricentennial cycle (i.e. 400-year cycle starting and ending in a year divisible by 400) containing the Julian day zero, which begins on March 1, 4801 BC in the proleptic Gregorian calendar.
For the full Julian date, not counting leap seconds (divisions are real numbers):
So, for example, January 1, 2000 at midday corresponds to JD = 2451545.0
|JDN mod 7||0||1||2||3||4||5||6|
|Day of the week||Mon||Tue||Wed||Thu||Fri||Sat||Sun|
We can then develop these formulas into a single inlined formula per component, computed as above. All this computing requires only integers and so is not sensitive to rounding errors caused by floating point approximations (most decimal fractions have an inexact representation within the binary format used by floating point arithmetic used by most computer software, so using them would produce false results on some dates because of roundoff errors).
The formulae below (which use Euclidian division — integer division (div) and modulo (mod) — without any negative numbers) are valid for the whole range of dates since −4800. For dates before 1582, the resulting date components are valid only in the Gregorian proleptic calendar. This is based on the Gregorian calendar but extended to cover dates before its introduction, including the pre-Christian era. For dates in that era (before year 1 CE), astronomical year numbering is used. This includes a year zero, which immediately precedes 1 CE. Astronomical year zero is 1 BCE in the proleptic Gregorian calendar and, in general, year n BCE = astronomical year 1 − n, and for astronomical year A (A < 1), the BCE year is 1 + abs(A).
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