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mean solar day sentence in Hindi

"mean solar day" meaning in Hindimean solar day in a sentence
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  • Thus the rete rotated once in 365 / 366 of a mean solar day, which equated 366 successive meridian transits of the vernal equinox with 365 similar transits of the sun.
  • All of these factors cause the mean solar day, on the average, to be slightly longer than the nominal 86, 400 SI seconds, the traditional number of seconds per day.
  • However, for the past several centuries, the length of the mean solar day has been increasing by about 1.4 1.7 ms per century, depending on the averaging time.
  • If instead of mean solar day we use the sidereal year as our time unit, the value of is very close to 2 [ [ pi | ] ] ( = } } ).
  • A mean solar day ( what we normally measure as a " day " ) is the average time between local solar noons ( " average " since this varies slightly over the year ).
  • The Analemma was devised as a means of calculating deviations in the actual day from the mean solar day .-- 32 " "'14 : 58, 25 November 2010 ( UTC)
  • However, the duration of one mean solar day is now slightly longer ( by roughly 0.001 seconds ) than 24 hours ( 86400 SI seconds ) because the rotation of the Earth has slowed down.
  • Near the end of the 20th century, the length of the mean solar day ( also known simply as " length of day " or " LOD " ) was approximately 86, 400.0013 s.
  • Its average duration is mean solar days ( 365 d 6 h 9 min 9.76 s ) ( at the epoch J2000.0 = January 1, 2000, 12 : 00 : 00 TT ).
  • A key development in understanding the tropical year over long periods of time is the discovery that the rate of rotation of the earth, or equivalently, the length of the mean solar day, is not constant.
  • If the law was written to say the second is " 1 / 86 400 of the mean solar day " or whatever, then yes this would need to be changed or updated or it would still apply.
  • The length of the SI second was calibrated on the basis of the second of ephemeris time and can now be seen to have a relationship with the mean solar day observed between 1750 and 1892, analysed by Simon Newcomb.
  • Therefore, time standards that change the date after precisely 86, 400 SI seconds, such as the International Atomic Time ( TAI ), will get increasingly ahead of time standards tied to the mean solar day, such as Greenwich Mean Time ( GMT ).
  • Originally the second was defined as 1 / 86, 400 of the mean solar day, which is the year-average of the solar day, being the time interval between two successive noons, i . e ., the time interval between two successive passages of the sun across the meridian.
  • Recently ( 1999 2010 ) the average annual length of the mean solar day in excess of 86, 400 SI seconds has varied between and, which must be added to both the stellar and sidereal days given in mean solar time above to obtain their lengths in SI seconds ( see Fluctuations in the length of day ).
  • In the introduction to Newcomb's Tables of the Sun ( 1895 ) the basis of the tables ( p . 9 ) includes a formula for the Sun's mean longitude, at a time indicated by interval T ( in Julian centuries of 36525 mean solar days ) reckoned from Greenwich Mean Noon on 0 January 1900:
  • The tiny increase of the mean solar day due to the slowing down of the Earth's rotation, by about 2 ms per day per century, which currently accumulates up to about 1 second every year, is not taken into account in traditional definitions of the equation of time, as it is imperceptible at the accuracy level of sundials.
  • The fact that these planes don't match has to be taken into account when calculating the difference between the " mean solar day " ( i . e . an exact 24 hour period measured on the clock ) and the " apparent solar day ", which is the time between the reappearance of the sun in the same position on successive turns of the earth around its axis.
  • Just as adding a leap day every four years does not mean the year is getting longer by one day every four years, the insertion of a leap second every 800 days does not indicate that the mean solar day is getting longer by a second every 800 days . It will take about 50, 000 years for a mean solar day to lengthen by one second ( at a rate of 2 ms / cy, where cy means century ).
  • Just as adding a leap day every four years does not mean the year is getting longer by one day every four years, the insertion of a leap second every 800 days does not indicate that the mean solar day is getting longer by a second every 800 days . It will take about 50, 000 years for a mean solar day to lengthen by one second ( at a rate of 2 ms / cy, where cy means century ).
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