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Position of the Sun

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20: 2256:. As the graph shows, a sundial can be up to about 16 minutes fast or slow, compared with a clock. Since the Earth rotates at a mean speed of one degree every four minutes, relative to the Sun, this 16-minute displacement corresponds to a shift eastward or westward of about four degrees in the apparent position of the Sun, compared with its mean position. A westward shift causes the sundial to be ahead of the clock. 1364: 2230: 3097: 1793:) is also discouraged for having an error of up to 0.28°. An additional error of up to 0.5° can occur in all equations around the equinoxes if not using a decimal place when selecting N to adjust for the time after UT midnight for the beginning of that day. So the above equation can have up to 2.0° of error, about four times the Sun's angular width, depending on how it is used. 1498:, in early July. This makes processes like the variation of the solar declination happen faster in January than in July. On the graph, this makes the minima more acute than the maxima. Also, since perihelion and aphelion do not happen on the exact dates as the solstices, the maxima and minima are slightly asymmetrical. The rates of change before and after are not quite equal. 1789:−1). The number 10, in (N+10), is the approximate number of days after the December solstice to January 1. This equation overestimates the declination near the September equinox by up to +1.5°. The sine function approximation by itself leads to an error of up to 0.26° and has been discouraged for use in solar energy applications. The 1971 Spencer formula (based on a 3121: 3073: 3109: 3085: 2243:
In addition to the annual north–south oscillation of the Sun's apparent position, corresponding to the variation of its declination described above, there is also a smaller but more complex oscillation in the east–west direction. This is caused by the tilt of the Earth's axis, and also by changes in
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is small, its orbit can be approximated as a circle which causes up to 1° of error. The circle approximation means the EL would be 90° ahead of the solstices in Earth's orbit (at the equinoxes), so that sin(EL) can be written as sin(90+NDS)=cos(NDS) where NDS is the number of days after the December
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of light in the atmosphere, which causes the apparent angle of elevation of the Sun as seen by an observer to be higher than the actual angle of elevation, especially at low Sun elevations. For example, when the Sun is at an elevation of 10°, it appears to be at 10.1°. The Sun's declination can be
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More complicated algorithms correct for changes to the ecliptic longitude by using terms in addition to the 1st-order eccentricity correction above. They also correct the 23.44° obliquity which changes very slightly with time. Corrections may also include the effects of the moon in offsetting the
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by astronomers) is the angle between the Earth's axis and a line perpendicular to the Earth's orbit. The Earth's axial tilt changes slowly over thousands of years but its current value of about ε = 23°44' is nearly constant, so the change in solar declination during one year is nearly the same as
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If the 90° axial tilt is decreased, then the absolute maximum and minimum values of the declination would decrease, to equal the axial tilt. Also, the shapes of the maxima and minima on the graph would become less acute, being curved to resemble the maxima and minima of a sine wave. However, even
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Zhang, T., Stackhouse, P.W., Macpherson, B., and Mikovitz, J.C., 2021. A solar azimuth formula that renders circumstantial treatment unnecessary without compromising mathematical rigor: Mathematical setup, application and extension of a formula based on the subsolar point and atan2 function.
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of the Earth's orbit. The eccentricity varies very slowly over time, but for dates fairly close to the present, it can be considered to be constant. The largest errors in this equation are less than ± 0.2°, but are less than ± 0.03° for a given year if the number 10 is adjusted up or down in
2328:, plotted horizontally. Usually, the scales are chosen so that equal distances on the diagram represent equal angles in both directions on the celestial sphere. Thus 4 minutes (more precisely 3 minutes, 56 seconds), in the equation of time, are represented by the same distance as 1° in the 2184:
fractional days as determined by how far the previous year's December solstice occurred before or after noon on December 22. These accuracies are compared to NOAA's advanced calculations which are based on the 1999 Jean Meeus algorithm that is accurate to within 0.01°.
2263:, using the word "equation" in a somewhat archaic sense meaning "correction". The oscillation is measured in units of time, minutes and seconds, corresponding to the amount that a sundial would be ahead of a clock. The equation of time can be positive or negative. 2203:
is applied, which depends on the observer's distance away from the center of the Earth. This correction is less than 0.0025°. The error in calculating the position of the center of the Sun can be less than 0.00015°. For comparison, the Sun's width is about 0.5°.
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with time. Eventually, the Sun would be directly above the South Pole, with a declination of −90°; then it would start to move northward at a constant speed. Thus, the graph of solar declination, as seen from this highly tilted Earth, would resemble a
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the speed of its orbital motion around the Sun produced by the elliptical shape of the orbit. The principal effects of this east–west oscillation are variations in the timing of events such as sunrise and sunset, and in the reading of a
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Some analemmas are marked to show the position of the Sun on the graph on various dates, a few days apart, throughout the year. This enables the analemma to be used to make simple analog computations of quantities such as the times and
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The path of the Sun over the celestial sphere through the course of the day for an observer at 56°N latitude. The Sun's path changes with its declination during the year. The intersections of the curves with the horizontal axis show
1060: 601: 1776: 776: 1123: 941: 711: 423: 364: 2166: 2005: 1660: 1267: 1222: 301: 1177: 2175:−1) and can include decimals to adjust for local times later or earlier in the day. The number 2, in (N-2), is the approximate number of days after January 1 to the Earth's 879: 985: 803: 637: 961: 1501:
The graph of apparent solar declination is therefore different in several ways from a sine wave. Calculating it accurately involves some complexity, as shown below.
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Earth's position from the center of the pair's orbit around the Sun. After obtaining the declination relative to the center of the Earth, a further correction for
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The declination can be more accurately calculated by not making the two approximations, using the parameters of the Earth's orbit to more accurately estimate EL:
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The equation of time — above the axis a sundial will appear fast relative to a clock showing local mean time, and below the axis a sundial will appear slow.
997: 2792: 2893: 3146: 2618: 2313:, which resembles a figure-8. An analemma can be pictured by superimposing photographs taken at the same time of day, a few days apart for a 533: 165:, for the observer's local time and location. This is the coordinate system normally used to calculate the position of the Sun in terms of 2850: 2822: 1680: 2682: 2506: 732: 2309:
is also occasionally, but rarely, used in other contexts.) It can be considered as an image of the Sun's apparent motion during a
2221:, to calculate its azimuth and also its true elevation, which can then be corrected for refraction to give its apparent position. 1075: 893: 255:, the number of days (positive or negative, including fractional days) since Greenwich noon, Terrestrial Time, on 1 January 2000 ( 19: 2997: 1674:
solstice. By also using the approximation that arcsin is close to d·cos(NDS), the following frequently used formula is obtained:
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of the Sun (actually, of the Earth in its orbit around the Sun, but it is convenient to pretend the Sun orbits the Earth), is:
1533:, the angle between the rays of the Sun and the plane of the Earth's equator reaches its maximum value of 23°44'. Therefore, δ 2407: 2412: 657: 379: 320: 3063: 1479:
when the axial tilt equals that of the actual Earth, the maxima and minima remain more acute than those of a sine wave.
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To find the Sun's position for a given location at a given time, one may therefore proceed in three steps as follows:
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To get RA at the right quadrant on computer programs use double argument Arctan function such as ATAN2(y,x)
2641: 236:, to a precision of about 0°.01 (36″), for dates between 1950 and 2050. Similar equations are coded into a 2213: 469: 2738: 2422: 2892:
Blanco-Muriel, Manuel; Alarcón-Padilla, Diego C; López-Moratalla, Teodoro; Lara-Coira, Martín (2001).
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Sproul, Alistair B. (2007). "Derivation of the solar geometric relationships using vector analysis".
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of the Sun never exceeds 0.00033° (a little over 1″), and the distance of the Sun from the Earth, in
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of 23.44°, but one lobe of the wave is several days longer than the other, among other differences.
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We see light from the Sun about 20 angle seconds from where the Sun is when the light is seen. See
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N is the number of days since midnight UT as January 1 begins (i.e. the days part of the
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U.S. Naval Observatory; U.K. Hydrographic Office, H.M. Nautical Almanac Office (2008).
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An analemma is drawn as it would be seen in the sky by an observer looking upward. If
3135: 3056: 2573: 2565: 2310: 2187:(The above formula is related to a reasonably simple and accurate calculation of the 1468: 1435: 1397: 1385: 1316: 24: 2671:
U.S. Naval Observatory Nautical Almanac Office (1992). P. Kenneth Seidelmann (ed.).
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around the Sun, and if its axis were tilted 90°, so that the axis itself is on the
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website. Positions of Solar System objects based on the INPOP series ephemerides.
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Much the same set of equations, covering the years 1800 to 2200, can be found at
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between plus and minus 90°, with linear segments between the maxima and minima.
1404:, when its value is the negative of the axial tilt. This variation produces the 1389: 1363: 1066: 260: 198: 194: 129: 99: 2595: 2229: 2212:
The declination calculations described above do not include the effects of the
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is a diagram that shows the annual variation of the Sun's position on the
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Since the main effect of this oscillation concerns time, it is called the
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website. Very accurate positions of Solar System objects based on the
2368: 1472: 1443: 1439: 1405: 596:{\displaystyle \lambda =L+1.915^{\circ }\sin g+0.020^{\circ }\sin 2g} 3036: 3032: 2271: 1669:(essentially, the Earth's position in its orbit). Since the Earth's 3084: 16:
Calculating the Sun's location in the sky at a given time and place
2648:. Graphs of the error of these equations, compared to an accurate 2548: 2355:, on which the continents, etc., are shown with west to the left. 2352: 2340: 2270: 2249: 2228: 1362: 83: 18: 1462:
at a constant rate, so that the solar declination would decrease
1450:, so its declination would be +90°. For the next few months, the 3021: 2638: 2344: 2314: 1771:{\displaystyle \delta _{\odot }=-23.44^{\circ }\cdot \cos \left} 95: 75: 3014:. An interactive calculator showing the Sun's path in the sky. 2321: 1781:
where N is the day of the year beginning with N=0 at midnight
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at a mean speed of 1° every 4 minutes, relative to the Sun.
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The Sun's declination at any given moment is calculated by:
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The following phenomena would occur if Earth were a perfect
1118:{\displaystyle \delta =\arcsin(\sin \epsilon \sin \lambda )} 936:{\displaystyle \alpha =\arctan(\cos \epsilon \tan \lambda )} 2936:"Solar Position Algorithm for Solar Radiation Applications" 228:, can be used to calculate the apparent coordinates of the 2731:"Fourier series representation of the position of the sun" 2677:. University Science Books, Mill Valley, CA. p. 12. 1376:
The Sun appears to move northward during the northern
706:{\displaystyle R=1.00014-0.01671\cos g-0.00014\cos 2g} 418:{\displaystyle g=357.528^{\circ }+0.9856003^{\circ }n} 359:{\displaystyle L=280.460^{\circ }+0.9856474^{\circ }n} 120:, so that the Sun appears to move across the sky in a 3061: 2497:(1991). "Chapter 12: Transformation of Coordinates". 2320:
An analemma can also be considered as a graph of the
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which can be simplified by evaluating constants to:
1785:(UT) as January 1 begins (i.e. the days part of the 1548:, the center of the Sun appears to pass through the 3020:, at the NOAA Earth System Research Laboratories's 1415:of the Sun's declination during a year resembles a 1372:
in degrees from North where the Sun rises and sets.
726:is not obtained elsewhere, it can be approximated: 173:, and the two parameters can be used to depict the 2674:Explanatory Supplement to the Astronomical Almanac 2160: 1999: 1770: 1654: 1331: 1307: 1283: 1261: 1216: 1171: 1117: 1054: 979: 955: 935: 873: 837: 817: 797: 770: 705: 631: 595: 508: 488: 460: 440: 417: 358: 295: 1392:reaches a maximum equal to the angle of Earth's 468:in the range 0° to 360° by adding or subtracting 240:90 routine in Ref. and are used to calculate the 2179:. The number 0.0167 is the current value of the 2964:National Oceanic and Atmospheric Administration 2466:, the Earth's orbit would be stated as being a 2161:{\displaystyle \delta _{\odot }=-\arcsin \left} 1537:= +23°44' at the northern summer solstice and δ 1490:. Earth moves more rapidly around the Sun near 3047:General ephemerides of the solar system bodies 3028:NOAA's declination and sun position calculator 2000:{\displaystyle \delta _{\odot }=\arcsin \left} 1655:{\displaystyle \delta _{\odot }=\arcsin \left} 1262:{\displaystyle Z=R\sin \epsilon \sin \lambda } 1217:{\displaystyle Y=R\cos \epsilon \sin \lambda } 98:, the Sun appears to move with respect to the 2716:"Selected Astronomical Constants, 2015 (TXT)" 2699:"Selected Astronomical Constants, 2015 (PDF)" 1442:). At one date in the year, the Sun would be 8: 3000:, at National Renewable Energy Laboratory's 2718:. US Naval Observatory. 2014. p. K6–K7. 2704:. US Naval Observatory. 2014. p. K6–K7. 2596:https://doi.org/10.1016/j.renene.2021.03.047 2841: 2839: 2585: 2583: 1541:= −23°44' at the southern summer solstice. 248:as observed from the surface of the Earth. 2613:. U.S. Govt. Printing Office. p. C5. 2610:The Astronomical Almanac for the Year 2010 2324:, usually plotted vertically, against the 1359:Declination of the Sun as seen from Earth 124:that depends on the observer's geographic 2547: 2534:(2013). "The Sun's position in the sky". 2526: 2524: 2522: 2520: 2518: 2118: 2097: 2065: 2024: 2018: 1952: 1946: 1918: 1912: 1879: 1873: 1848: 1810: 1804: 1730: 1724: 1704: 1688: 1682: 1611: 1573: 1567: 1324: 1300: 1276: 1230: 1185: 1149: 1077: 999: 972: 948: 895: 866: 830: 810: 790: 759: 746: 734: 659: 618: 575: 553: 535: 501: 481: 453: 433: 406: 393: 381: 347: 334: 322: 296:{\displaystyle n=\mathrm {JD} -2451545.0} 279: 271: 3068: 2486: 2455: 2960:"Atmospheric Refraction Approximation" 2747: 2736: 1137:rectangular equatorial coordinates in 7: 2501:. Richmond, VA: Willmann Bell, Inc. 263:for the desired time is known, then 147:calculate the Sun's position in the 3057:Solar position in R. Insol package. 2934:Ibrahim Reda & Afshin Andreas. 106:, along a circular path called the 2851:Earth System Research Laboratories 2823:Earth System Research Laboratories 1130:Rectangular equatorial coordinates 283: 280: 62:a.m. local time on a March morning 14: 234:mean equinox and ecliptic of date 3119: 3107: 3095: 3083: 3071: 1458:at constant speed, crossing the 1291:axis is in the direction of the 1172:{\displaystyle X=R\cos \lambda } 845:form a complete position of the 853:. This can be converted to the 3002:Renewable Resource Data Center 2639:U.S. Naval Observatory website 2408:Effect of Sun angle on climate 1494:, in early January, than near 1112: 1091: 1049: 1016: 930: 909: 310:of the Sun, corrected for the 181:This calculation is useful in 1: 2921:10.1016/s0038-092x(00)00156-0 2635:Approximate Solar Coordinates 3147:Dynamics of the Solar System 2894:"Computing the Solar Vector" 2779:10.1016/j.renene.2006.05.001 1354:Horizontal coordinate system 855:equatorial coordinate system 516:are really to be evaluated ( 163:horizontal coordinate system 156:equatorial coordinate system 2847:"Solar Calculation Details" 2536:European Journal of Physics 2413:Newcomb's Tables of the Sun 3163: 3022:Global Monitoring Division 2566:10.1088/0143-0807/34/3/633 2343:is shown at the top, then 2290: 2236: 1396:(23.44° or 23°26') on the 1351: 851:ecliptic coordinate system 222:These equations, from the 149:ecliptic coordinate system 136:depends on the geographic 74:is a function of both the 2872:"Astronomical Algorithms" 1523:obliquity of the ecliptic 1471:rather than a sine wave, 874:{\displaystyle \epsilon } 859:obliquity of the ecliptic 724:obliquity of the ecliptic 718:Obliquity of the ecliptic 476:— which is to say, 2998:Solar Position Algorithm 980:{\displaystyle \lambda } 798:{\displaystyle \lambda } 632:{\displaystyle \beta =0} 128:. The time when the Sun 3008:Sun Position Calculator 2819:"NOAA Solar Calculator" 2594:, 172, 1333-1340. DOI: 2499:Astronomical Algorithms 2398:Solar annual aberration 2385:Solar annual aberration 1509:The declination of the 956:{\displaystyle \alpha } 2746:Cite journal requires 2729:J. W. Spencer (1971). 2288: 2234: 2208:Atmospheric refraction 2162: 2001: 1772: 1656: 1544:At the moment of each 1526:during the next year. 1454:would move toward the 1373: 1348:Horizontal coordinates 1333: 1309: 1285: 1263: 1218: 1173: 1119: 1056: 981: 957: 937: 875: 839: 819: 818:{\displaystyle \beta } 799: 782:Equatorial coordinates 772: 707: 633: 610:of the Sun is nearly: 597: 510: 490: 462: 442: 419: 360: 297: 116:about its axis causes 63: 3018:NOAA Solar Calculator 2652:, can also be viewed. 2423:Solar elevation angle 2274: 2232: 2217:used, along with its 2191:, which is described 2163: 2002: 1773: 1657: 1366: 1352:Further information: 1334: 1310: 1286: 1264: 1219: 1174: 1120: 1057: 982: 958: 938: 876: 840: 820: 800: 773: 708: 634: 598: 511: 491: 463: 443: 420: 361: 298: 251:Start by calculating 94:over the course of a 22: 2661:Meeus (1991), p. 152 2472:orbital eccentricity 2017: 1803: 1681: 1671:orbital eccentricity 1566: 1341:North celestial pole 1323: 1299: 1275: 1229: 1184: 1148: 1076: 998: 971: 947: 894: 865: 829: 809: 789: 733: 658: 617: 534: 500: 480: 452: 432: 380: 321: 270: 225:Astronomical Almanac 218:Ecliptic coordinates 213:Approximate position 2913:2001SoEn...70..431B 2558:2013EJPh...34..633J 2464:celestial mechanics 2418:Solar azimuth angle 1460:circles of latitude 881:, and continuing: 857:by calculating the 312:aberration of light 246:solar azimuth angle 171:solar azimuth angle 80:geographic location 68:position of the Sun 42: /  2984:Sundial#Noon marks 2644:2016-01-31 at the 2532:Jenkins, Alejandro 2379:Light-time effects 2289: 2287:to the same scale 2235: 2158: 1997: 1768: 1667:ecliptic longitude 1652: 1374: 1329: 1305: 1281: 1259: 1214: 1169: 1139:astronomical units 1115: 1052: 977: 953: 933: 871: 835: 815: 795: 768: 703: 649:astronomical units 629: 593: 525:ecliptic longitude 506: 486: 458: 438: 415: 356: 293: 242:solar zenith angle 167:solar zenith angle 82:of observation on 64: 2620:978-0-7077-4082-9 2322:Sun's declination 1961: 1927: 1888: 1739: 1550:celestial equator 1444:directly overhead 1402:December solstice 1382:celestial equator 1339:axis towards the 1332:{\displaystyle Z} 1308:{\displaystyle Y} 1284:{\displaystyle X} 838:{\displaystyle R} 645:ecliptic latitude 608:ecliptic latitude 509:{\displaystyle g} 489:{\displaystyle L} 472:of 360° as needed 461:{\displaystyle g} 441:{\displaystyle L} 3154: 3124: 3123: 3122: 3112: 3111: 3110: 3100: 3099: 3098: 3088: 3087: 3076: 3075: 3074: 3067: 2986: 2981: 2975: 2974: 2972: 2970: 2956: 2950: 2949: 2947: 2945: 2940: 2931: 2925: 2924: 2898: 2889: 2883: 2882: 2880: 2878: 2868: 2862: 2861: 2859: 2857: 2843: 2834: 2833: 2831: 2829: 2815: 2809: 2808: 2806: 2804: 2795:. Archived from 2789: 2783: 2782: 2773:(7): 1187–1205. 2767:Renewable Energy 2762: 2756: 2755: 2749: 2744: 2742: 2734: 2726: 2720: 2719: 2712: 2706: 2705: 2703: 2695: 2689: 2688: 2668: 2662: 2659: 2653: 2631: 2625: 2624: 2604: 2598: 2592:Renewable Energy 2587: 2578: 2577: 2551: 2528: 2513: 2512: 2491: 2475: 2460: 2443:Sunrise equation 2428:Solar irradiance 2326:equation of time 2303:celestial sphere 2285:equation of time 2261:equation of time 2248:compared with a 2239:Equation of time 2225:Equation of time 2189:Equation of Time 2167: 2165: 2164: 2159: 2157: 2153: 2152: 2148: 2147: 2143: 2142: 2138: 2123: 2122: 2102: 2101: 2089: 2085: 2070: 2069: 2029: 2028: 2006: 2004: 2003: 1998: 1996: 1992: 1991: 1987: 1986: 1982: 1981: 1977: 1962: 1957: 1956: 1947: 1928: 1923: 1922: 1913: 1908: 1904: 1889: 1884: 1883: 1874: 1858: 1854: 1853: 1852: 1815: 1814: 1777: 1775: 1774: 1769: 1767: 1763: 1762: 1758: 1740: 1735: 1734: 1725: 1709: 1708: 1693: 1692: 1665:where EL is the 1661: 1659: 1658: 1653: 1651: 1647: 1646: 1642: 1621: 1617: 1616: 1615: 1578: 1577: 1338: 1336: 1335: 1330: 1314: 1312: 1311: 1306: 1290: 1288: 1287: 1282: 1268: 1266: 1265: 1260: 1223: 1221: 1220: 1215: 1178: 1176: 1175: 1170: 1124: 1122: 1121: 1116: 1061: 1059: 1058: 1053: 986: 984: 983: 978: 962: 960: 959: 954: 942: 940: 939: 934: 880: 878: 877: 872: 844: 842: 841: 836: 824: 822: 821: 816: 804: 802: 801: 796: 777: 775: 774: 769: 764: 763: 751: 750: 712: 710: 709: 704: 638: 636: 635: 630: 602: 600: 599: 594: 580: 579: 558: 557: 515: 513: 512: 507: 495: 493: 492: 487: 475: 467: 465: 464: 459: 447: 445: 444: 439: 424: 422: 421: 416: 411: 410: 398: 397: 365: 363: 362: 357: 352: 351: 339: 338: 302: 300: 299: 294: 286: 114:Earth's rotation 104:celestial sphere 61: 57: 56: 54: 53: 52: 47: 46:8.283°N 98.600°E 43: 40: 39: 38: 35: 3162: 3161: 3157: 3156: 3155: 3153: 3152: 3151: 3132: 3131: 3130: 3120: 3118: 3108: 3106: 3096: 3094: 3082: 3072: 3070: 3062: 3033:HORIZONS System 3012:pveducation.org 2994: 2989: 2982: 2978: 2968: 2966: 2958: 2957: 2953: 2943: 2941: 2938: 2933: 2932: 2928: 2896: 2891: 2890: 2886: 2876: 2874: 2870: 2869: 2865: 2855: 2853: 2845: 2844: 2837: 2827: 2825: 2817: 2816: 2812: 2802: 2800: 2799:on 9 March 2012 2791: 2790: 2786: 2764: 2763: 2759: 2745: 2735: 2728: 2727: 2723: 2714: 2713: 2709: 2701: 2697: 2696: 2692: 2685: 2670: 2669: 2665: 2660: 2656: 2646:Wayback Machine 2632: 2628: 2621: 2606: 2605: 2601: 2588: 2581: 2530: 2529: 2516: 2509: 2493: 2492: 2488: 2484: 2479: 2478: 2474:of less than 1. 2461: 2457: 2452: 2447: 2393: 2381: 2295: 2269: 2254:local mean time 2241: 2227: 2219:right ascension 2210: 2128: 2124: 2114: 2113: 2109: 2093: 2075: 2071: 2061: 2060: 2056: 2046: 2042: 2020: 2015: 2014: 1967: 1963: 1948: 1945: 1941: 1914: 1894: 1890: 1875: 1872: 1868: 1844: 1840: 1836: 1829: 1825: 1806: 1801: 1800: 1748: 1744: 1726: 1723: 1719: 1700: 1684: 1679: 1678: 1635: 1631: 1607: 1603: 1599: 1592: 1588: 1569: 1564: 1563: 1555: 1540: 1536: 1516: 1507: 1380:, crossing the 1361: 1356: 1350: 1321: 1320: 1297: 1296: 1273: 1272: 1227: 1226: 1182: 1181: 1146: 1145: 1132: 1074: 1073: 996: 995: 969: 968: 963:is in the same 945: 944: 892: 891: 885:Right ascension 863: 862: 827: 826: 807: 806: 787: 786: 784: 755: 742: 731: 730: 720: 656: 655: 615: 614: 571: 549: 532: 531: 527:of the Sun is: 498: 497: 478: 477: 473: 450: 449: 430: 429: 402: 389: 378: 377: 343: 330: 319: 318: 268: 267: 220: 215: 161:convert to the 154:convert to the 132:the observer's 86:'s surface. As 59: 50: 48: 44: 41: 36: 33: 31: 29: 28: 17: 12: 11: 5: 3160: 3158: 3150: 3149: 3144: 3134: 3133: 3129: 3128: 3116: 3104: 3092: 3080: 3060: 3059: 3054: 3044: 3030: 3025: 3015: 3005: 2993: 2992:External links 2990: 2988: 2987: 2976: 2951: 2926: 2907:(5): 431–441. 2884: 2863: 2835: 2810: 2784: 2757: 2748:|journal= 2721: 2707: 2690: 2683: 2663: 2654: 2626: 2619: 2599: 2579: 2542:(3): 633–652. 2514: 2507: 2485: 2483: 2480: 2477: 2476: 2454: 2453: 2451: 2448: 2446: 2445: 2440: 2435: 2430: 2425: 2420: 2415: 2410: 2405: 2400: 2394: 2392: 2389: 2380: 2377: 2291:Main article: 2268: 2265: 2237:Main article: 2226: 2223: 2209: 2206: 2169: 2168: 2156: 2151: 2146: 2141: 2137: 2134: 2131: 2127: 2121: 2117: 2112: 2108: 2105: 2100: 2096: 2092: 2088: 2084: 2081: 2078: 2074: 2068: 2064: 2059: 2055: 2052: 2049: 2045: 2041: 2038: 2035: 2032: 2027: 2023: 2008: 2007: 1995: 1990: 1985: 1980: 1976: 1973: 1970: 1966: 1960: 1955: 1951: 1944: 1940: 1937: 1934: 1931: 1926: 1921: 1917: 1911: 1907: 1903: 1900: 1897: 1893: 1887: 1882: 1878: 1871: 1867: 1864: 1861: 1857: 1851: 1847: 1843: 1839: 1835: 1832: 1828: 1824: 1821: 1818: 1813: 1809: 1791:Fourier series 1783:Universal Time 1779: 1778: 1766: 1761: 1757: 1754: 1751: 1747: 1743: 1738: 1733: 1729: 1722: 1718: 1715: 1712: 1707: 1703: 1699: 1696: 1691: 1687: 1663: 1662: 1650: 1645: 1641: 1638: 1634: 1630: 1627: 1624: 1620: 1614: 1610: 1606: 1602: 1598: 1595: 1591: 1587: 1584: 1581: 1576: 1572: 1553: 1538: 1534: 1514: 1506: 1503: 1452:subsolar point 1432:circular orbit 1360: 1357: 1349: 1346: 1345: 1344: 1328: 1304: 1280: 1269: 1258: 1255: 1252: 1249: 1246: 1243: 1240: 1237: 1234: 1224: 1213: 1210: 1207: 1204: 1201: 1198: 1195: 1192: 1189: 1179: 1168: 1165: 1162: 1159: 1156: 1153: 1131: 1128: 1127: 1126: 1114: 1111: 1108: 1105: 1102: 1099: 1096: 1093: 1090: 1087: 1084: 1081: 1063: 1062: 1051: 1048: 1045: 1042: 1039: 1036: 1033: 1030: 1027: 1024: 1021: 1018: 1015: 1012: 1009: 1006: 1003: 989: 988: 976: 952: 932: 929: 926: 923: 920: 917: 914: 911: 908: 905: 902: 899: 870: 834: 814: 794: 783: 780: 779: 778: 767: 762: 758: 754: 749: 745: 741: 738: 719: 716: 715: 714: 702: 699: 696: 693: 690: 687: 684: 681: 678: 675: 672: 669: 666: 663: 641: 640: 628: 625: 622: 604: 603: 592: 589: 586: 583: 578: 574: 570: 567: 564: 561: 556: 552: 548: 545: 542: 539: 505: 485: 457: 437: 426: 425: 414: 409: 405: 401: 396: 392: 388: 385: 367: 366: 355: 350: 346: 342: 337: 333: 329: 326: 308:mean longitude 304: 303: 292: 289: 285: 282: 278: 275: 219: 216: 214: 211: 179: 178: 159: 152: 118:diurnal motion 15: 13: 10: 9: 6: 4: 3: 2: 3159: 3148: 3145: 3143: 3140: 3139: 3137: 3127: 3117: 3115: 3105: 3103: 3093: 3091: 3086: 3081: 3079: 3069: 3065: 3058: 3055: 3052: 3048: 3045: 3042: 3041:JPL DE series 3038: 3034: 3031: 3029: 3026: 3023: 3019: 3016: 3013: 3009: 3006: 3003: 2999: 2996: 2995: 2991: 2985: 2980: 2977: 2965: 2961: 2955: 2952: 2937: 2930: 2927: 2922: 2918: 2914: 2910: 2906: 2902: 2895: 2888: 2885: 2873: 2867: 2864: 2852: 2848: 2842: 2840: 2836: 2824: 2820: 2814: 2811: 2798: 2794: 2788: 2785: 2780: 2776: 2772: 2768: 2761: 2758: 2753: 2740: 2732: 2725: 2722: 2717: 2711: 2708: 2700: 2694: 2691: 2686: 2684:0-935702-68-7 2680: 2676: 2675: 2667: 2664: 2658: 2655: 2651: 2647: 2643: 2640: 2636: 2630: 2627: 2622: 2616: 2612: 2611: 2603: 2600: 2597: 2593: 2586: 2584: 2580: 2575: 2571: 2567: 2563: 2559: 2555: 2550: 2545: 2541: 2537: 2533: 2527: 2525: 2523: 2521: 2519: 2515: 2510: 2508:0-943396-35-2 2504: 2500: 2496: 2490: 2487: 2481: 2473: 2469: 2465: 2459: 2456: 2449: 2444: 2441: 2439: 2436: 2434: 2431: 2429: 2426: 2424: 2421: 2419: 2416: 2414: 2411: 2409: 2406: 2404: 2401: 2399: 2396: 2395: 2390: 2388: 2386: 2378: 2376: 2374: 2370: 2366: 2362: 2356: 2354: 2350: 2346: 2342: 2337: 2335: 2334:Earth rotates 2331: 2327: 2323: 2318: 2316: 2312: 2308: 2304: 2300: 2294: 2286: 2282: 2278: 2273: 2266: 2264: 2262: 2257: 2255: 2251: 2247: 2240: 2231: 2224: 2222: 2220: 2215: 2207: 2205: 2202: 2196: 2194: 2190: 2185: 2182: 2178: 2174: 2154: 2149: 2144: 2139: 2135: 2132: 2129: 2125: 2119: 2115: 2110: 2106: 2103: 2098: 2094: 2090: 2086: 2082: 2079: 2076: 2072: 2066: 2062: 2057: 2053: 2050: 2047: 2043: 2039: 2036: 2033: 2030: 2025: 2021: 2013: 2012: 2011: 1993: 1988: 1983: 1978: 1974: 1971: 1968: 1964: 1958: 1953: 1949: 1942: 1938: 1935: 1932: 1929: 1924: 1919: 1915: 1909: 1905: 1901: 1898: 1895: 1891: 1885: 1880: 1876: 1869: 1865: 1862: 1859: 1855: 1849: 1845: 1841: 1837: 1833: 1830: 1826: 1822: 1819: 1816: 1811: 1807: 1799: 1798: 1797: 1794: 1792: 1788: 1784: 1764: 1759: 1755: 1752: 1749: 1745: 1741: 1736: 1731: 1727: 1720: 1716: 1713: 1710: 1705: 1701: 1697: 1694: 1689: 1685: 1677: 1676: 1675: 1672: 1668: 1648: 1643: 1639: 1636: 1632: 1628: 1625: 1622: 1618: 1612: 1608: 1604: 1600: 1596: 1593: 1589: 1585: 1582: 1579: 1574: 1570: 1562: 1561: 1560: 1557: 1551: 1547: 1542: 1532: 1527: 1524: 1520: 1512: 1504: 1502: 1499: 1497: 1493: 1489: 1485: 1484:Earth's orbit 1480: 1476: 1474: 1470: 1469:triangle wave 1465: 1461: 1457: 1453: 1449: 1445: 1441: 1437: 1436:orbital plane 1433: 1429: 1424: 1422: 1418: 1414: 1409: 1407: 1403: 1399: 1398:June solstice 1395: 1391: 1387: 1386:March equinox 1383: 1379: 1371: 1365: 1358: 1355: 1347: 1342: 1326: 1318: 1317:June Solstice 1315:axis towards 1302: 1294: 1293:March equinox 1278: 1270: 1256: 1253: 1250: 1247: 1244: 1241: 1238: 1235: 1232: 1225: 1211: 1208: 1205: 1202: 1199: 1196: 1193: 1190: 1187: 1180: 1166: 1163: 1160: 1157: 1154: 1151: 1144: 1143: 1142: 1140: 1136: 1129: 1109: 1106: 1103: 1100: 1097: 1094: 1088: 1085: 1082: 1079: 1072: 1071: 1070: 1068: 1046: 1043: 1040: 1037: 1034: 1031: 1028: 1025: 1022: 1019: 1013: 1010: 1007: 1004: 1001: 994: 993: 992: 974: 966: 950: 927: 924: 921: 918: 915: 912: 906: 903: 900: 897: 890: 889: 888: 886: 882: 868: 860: 856: 852: 848: 832: 812: 792: 781: 765: 760: 756: 752: 747: 743: 739: 736: 729: 728: 727: 725: 717: 700: 697: 694: 691: 688: 685: 682: 679: 676: 673: 670: 667: 664: 661: 654: 653: 652: 650: 646: 626: 623: 620: 613: 612: 611: 609: 590: 587: 584: 581: 576: 572: 568: 565: 562: 559: 554: 550: 546: 543: 540: 537: 530: 529: 528: 526: 523:Finally, the 521: 519: 503: 483: 471: 455: 435: 412: 407: 403: 399: 394: 390: 386: 383: 376: 375: 374: 372: 353: 348: 344: 340: 335: 331: 327: 324: 317: 316: 315: 313: 309: 290: 287: 276: 273: 266: 265: 264: 262: 258: 254: 249: 247: 243: 239: 235: 231: 227: 226: 217: 212: 210: 208: 204: 200: 196: 192: 188: 184: 176: 172: 168: 164: 160: 157: 153: 150: 146: 145: 144: 141: 139: 135: 131: 127: 123: 119: 115: 111: 109: 105: 101: 97: 93: 89: 85: 81: 77: 73: 69: 55: 51:8.283; 98.600 27:in Thailand ( 26: 25:Phang Nga Bay 23:The Sun over 21: 3126:Solar System 3043:ephemerides. 2979: 2967:. Retrieved 2954: 2942:. Retrieved 2929: 2904: 2901:Solar Energy 2900: 2887: 2875:. Retrieved 2866: 2854:. Retrieved 2826:. Retrieved 2813: 2801:. Retrieved 2797:the original 2787: 2770: 2766: 2760: 2739:cite journal 2724: 2710: 2693: 2673: 2666: 2657: 2629: 2609: 2602: 2591: 2539: 2535: 2498: 2489: 2468:Kepler orbit 2458: 2382: 2357: 2348: 2338: 2319: 2306: 2296: 2260: 2258: 2242: 2211: 2197: 2186: 2181:eccentricity 2173:ordinal date 2170: 2009: 1795: 1787:ordinal date 1780: 1664: 1558: 1543: 1528: 1522: 1521:(called the 1508: 1505:Calculations 1500: 1482:In reality, 1481: 1477: 1463: 1438:(similar to 1425: 1410: 1375: 1135:Right-handed 1133: 1064: 990: 883: 785: 721: 642: 605: 522: 427: 371:mean anomaly 368: 305: 252: 250: 223: 221: 203:solar energy 180: 142: 112: 88:Earth orbits 67: 65: 3114:Outer space 3102:Spaceflight 2969:28 February 2944:28 February 2877:28 February 2856:28 February 2828:28 February 2803:28 February 2495:Meeus, Jean 2330:declination 2281:declination 2279:with solar 1390:declination 1067:declination 261:Julian date 199:climatology 195:meteorology 100:fixed stars 49: / 3136:Categories 2793:"SunAlign" 2482:References 2433:Solar time 2347:is to the 2214:refraction 2177:perihelion 1519:axial tilt 1492:perihelion 1488:elliptical 1473:zigzagging 1456:South Pole 1448:North Pole 1413:line graph 1394:axial tilt 1319:, and the 722:Where the 259:). If the 187:navigation 58:), at 7:00 3078:Astronomy 3049:, at the 3035:, at the 2650:ephemeris 2637:, at the 2574:119282288 2549:1208.1043 2133:− 2120:∘ 2107:⁡ 2099:∘ 2067:∘ 2054:⁡ 2040:⁡ 2034:− 2026:⊙ 2022:δ 1972:− 1954:∘ 1939:⁡ 1930:⋅ 1925:π 1920:∘ 1881:∘ 1866:⁡ 1860:⋅ 1850:∘ 1842:− 1834:⁡ 1823:⁡ 1812:⊙ 1808:δ 1742:⋅ 1732:∘ 1717:⁡ 1711:⋅ 1706:∘ 1698:− 1690:⊙ 1686:δ 1629:⁡ 1623:⋅ 1613:∘ 1605:− 1597:⁡ 1586:⁡ 1575:⊙ 1571:δ 1531:solstices 1421:amplitude 1417:sine wave 1257:λ 1254:⁡ 1248:ϵ 1245:⁡ 1212:λ 1209:⁡ 1203:ϵ 1200:⁡ 1167:λ 1164:⁡ 1110:λ 1107:⁡ 1101:ϵ 1098:⁡ 1089:⁡ 1080:δ 1047:λ 1044:⁡ 1035:λ 1032:⁡ 1026:ϵ 1023:⁡ 1011:⁡ 1002:α 975:λ 951:α 928:λ 925:⁡ 919:ϵ 916:⁡ 907:⁡ 898:α 869:ϵ 813:β 793:λ 761:∘ 757:0.0000004 753:− 748:∘ 737:ϵ 695:⁡ 686:− 680:⁡ 671:− 621:β 585:⁡ 577:∘ 563:⁡ 555:∘ 538:λ 470:multiples 408:∘ 404:0.9856003 395:∘ 349:∘ 345:0.9856474 336:∘ 291:2451545.0 288:− 191:surveying 183:astronomy 138:longitude 3024:website. 3004:website. 2642:Archived 2470:with an 2438:Sun path 2403:Ecliptic 2391:See also 2373:sundials 2361:azimuths 2332:, since 2307:analemma 2299:analemma 2293:Analemma 2277:analemma 2267:Analemma 2252:showing 2201:parallax 1496:aphelion 1464:linearly 1419:with an 1370:azimuths 965:quadrant 943:, where 209:design. 175:Sun path 134:meridian 130:transits 126:latitude 122:Sun path 108:ecliptic 78:and the 3064:Portals 2909:Bibcode 2554:Bibcode 2365:sunrise 2246:sundial 2116:0.98565 2063:0.98565 2048:0.39779 1556:is 0°. 1552:, and δ 1546:equinox 1529:At the 1446:at the 1430:, in a 1406:seasons 1384:on the 849:in the 689:0.00014 674:0.01671 668:1.00014 643:as the 474:‍ 391:357.528 332:280.460 257:J2000.0 238:Fortran 207:sundial 102:on the 70:in the 37:98°36′E 2681:  2617:  2572:  2505:  2369:sunset 2037:arcsin 1959:365.24 1933:0.0167 1886:365.24 1820:arcsin 1583:arcsin 1440:Uranus 1428:sphere 1388:. 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Index


Phang Nga Bay
8°17′N 98°36′E / 8.283°N 98.600°E / 8.283; 98.600
sky
time
geographic location
Earth
Earth orbits
Sun
year
fixed stars
celestial sphere
ecliptic
Earth's rotation
diurnal motion
Sun path
latitude
transits
meridian
longitude
ecliptic coordinate system
equatorial coordinate system
horizontal coordinate system
solar zenith angle
solar azimuth angle
Sun path
astronomy
navigation
surveying
meteorology

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