Astronomy L0l Lecture 券l

Total Page:16

File Type:pdf, Size:1020Kb

Astronomy L0l Lecture 券l Astronomy 101 Lecture #2 Today: Time in Astronomy Charts and Catalogs Reading: Ch. 2, 3 Tomorrow, and tomorrow, and tomorrow, Creeps in this petty pace from day to day. ± William Shakespeare What then is time? If no one asks me, I know what it is. If I wish to explain it to him who asks, I do not know. ± Saint Augustine Astronomy 101 Lecture #2 I. The Length of Day Sidereal Time = RA of stars crossing the meridian or HA of Vernal Equinox. For any star: ST = RA+HA Sidereal Day = time between two successive meridian crossings of VE . Astronomy 101 Lecture #2 Solar Time = HA of the Sun +/- 12h Solar Day = time between two successive meridian crossings of the Sun. Difference between solar and sidereal days. Astronomy 101 Lecture #2 Solar Time is non-uniform due to: 1) ellipticity of the Earth©s orbit 2) tilt of the Earth©s polar axis with respect to the ecliptic. Mean Solar Time (MST) = HA of hypothetical mean Sun +/- 12h. Mean Solar Day = time between two successive meridian crossings of the hypothetical mean Sun. 1 solar day = 86,400 solar seconds. Astronomy 101 Lecture #2 Universal Time (UT) = MST at Greenwich observatory in England. Also known as Greenwich Mean Time (GMT). Difference between PST and UT is 8 hours in winter and 7 hours in summer (because of daylight savings time change). Astronomy 101 Lecture #2 How long a minute is, depends II. Precise Timekeeping on which side of the bathroom door you're on. -Zall's Second Law Before 1958: 1 s = 1/86400 solar day t / t≃2×10−10 1958 ± 1867: 1 s = 1 ephemeris second = = 1/31556925.9747 tropical year After 1967:Sun 1 s = 1 atomic (SI) second = 133 = 9192631770 cycles of Cs hyperfine transition. t / t≃10−14 Astronomy 101 Lecture #2 Atomic Time (TAI, Temps Atomique International) = based on SI second. TAI clock agreed with UT clock in 1958. 1 SI second = 1 solar second in 1820! Now the offset between UT and TAI clocks is About 1.2 s per year. Universal Coordinated Time (UTC) = based on SI second, but is adjusted on June 20 and/or Dec 31 by a adding a leap second to match UT to within 0.9 s. Astronomers typically time-stamp their data using UTC! Astronomy 101 Lecture #2 Effects of General Relativity 1. Moving clocks run slower relative to a clock at rest. 2. Clocks in a gravitational potential well run slowly relative to a clock in away from sources of gravity. Barycentric Dynamical Time (TDB) = time kept by a clock on a surface of a hypothetical Earth in a circular orbit around the Sun with the same period as the real Earth. Eliminated annual fluctuations with amplitude of about 1.7ms relative to TDT. Barycentric Coordinate Time (TCB) = time kept by a clock infinitely far from the Solar System barycenter and at rest relative to it. Runs faster than TDB by 49s per 100 years. Astronomy 101 Lecture #2 Heliocentric Time = time recorded by an observer on a hypothetical Earth located at the Solar System barycenter. Runs at the same rate as BDT, but eliminates time of travel variations caused by the varying distance between the Earth and the target due to Earth©s motion around the Sun. Earth Sun Star Earth Astronomy 101 Lecture #2 II. Calendar Julian Date (JD) = number of days since 12h noon on Jan 1, 4713 BC. At 0h UT on any day after Jan 1, 2000: JD = 2,451,544.5 + 365 (Y ± 2000) + N + L Y = year of interest N = day number L = number of leap days between Jan 1, 2001 and the day of interest. Epoch = J2000 was set at 12h Jan 1, 2000 (TDB). JD(TDB) = 2,451,545.0(TDB) +(365[E±2000]). Astronomy 101 Lecture #2 II. Calendar Sidereal Year = time it takes the Earth to orbit the Sun relative to distant stars. Sidereal year = 365.256363 days Tropical Year = time between two successive vernal equinox crossings of the Sun. Tropical year = 365.242190 days .
Recommended publications
  • Ast 443 / Phy 517
    AST 443 / PHY 517 Astronomical Observing Techniques Prof. F.M. Walter I. The Basics The 3 basic measurements: • WHERE something is • WHEN something happened • HOW BRIGHT something is Since this is science, let’s be quantitative! Where • Positions: – 2-dimensional projections on celestial sphere (q,f) • q,f are angular measures: radians, or degrees, minutes, arcsec – 3-dimensional position in space (x,y,z) or (q, f, r). • (x,y,z) are linear positions within a right-handed rectilinear coordinate system. • R is a distance (spherical coordinates) • Galactic positions are sometimes presented in cylindrical coordinates, of galactocentric radius, height above the galactic plane, and azimuth. Angles There are • 360 degrees (o) in a circle • 60 minutes of arc (‘) in a degree (arcmin) • 60 seconds of arc (“) in an arcmin There are • 24 hours (h) along the equator • 60 minutes of time (m) per hour • 60 seconds of time (s) per minute • 1 second of time = 15”/cos(latitude) Coordinate Systems "What good are Mercator's North Poles and Equators Tropics, Zones, and Meridian Lines?" So the Bellman would cry, and the crew would reply "They are merely conventional signs" L. Carroll -- The Hunting of the Snark • Equatorial (celestial): based on terrestrial longitude & latitude • Ecliptic: based on the Earth’s orbit • Altitude-Azimuth (alt-az): local • Galactic: based on MilKy Way • Supergalactic: based on supergalactic plane Reference points Celestial coordinates (Right Ascension α, Declination δ) • δ = 0: projection oF terrestrial equator • (α, δ) = (0,0):
    [Show full text]
  • Geological Timeline
    Geological Timeline In this pack you will find information and activities to help your class grasp the concept of geological time, just how old our planet is, and just how young we, as a species, are. Planet Earth is 4,600 million years old. We all know this is very old indeed, but big numbers like this are always difficult to get your head around. The activities in this pack will help your class to make visual representations of the age of the Earth to help them get to grips with the timescales involved. Important EvEnts In thE Earth’s hIstory 4600 mya (million years ago) – Planet Earth formed. Dust left over from the birth of the sun clumped together to form planet Earth. The other planets in our solar system were also formed in this way at about the same time. 4500 mya – Earth’s core and crust formed. Dense metals sank to the centre of the Earth and formed the core, while the outside layer cooled and solidified to form the Earth’s crust. 4400 mya – The Earth’s first oceans formed. Water vapour was released into the Earth’s atmosphere by volcanism. It then cooled, fell back down as rain, and formed the Earth’s first oceans. Some water may also have been brought to Earth by comets and asteroids. 3850 mya – The first life appeared on Earth. It was very simple single-celled organisms. Exactly how life first arose is a mystery. 1500 mya – Oxygen began to accumulate in the Earth’s atmosphere. Oxygen is made by cyanobacteria (blue-green algae) as a product of photosynthesis.
    [Show full text]
  • 2020-2021 Districtwide School Year Calendar
    FINAL 2020 – 2021 Districtwide School Year Calendar AUGUST FEBRUARY 2020-21 Calendar M T W T F M T W T F 3 4 5 6 7 1 2 3 4 5 Aug 17 Professional Meeting Day. No Students 8 Aug 18 -21 Staff Professional Development Day. 10 11 12 13 14 9 10 11 12 M No Students. Aug 24 Schools Open. Students Report. 17 18 19 20 21 15 16 17 18 19 Sept 7 Labor Day. Holiday. Schools Closed Sep 14 Midterm Week 24 25 26 27 28 22 23 24 25 26 Sep 21 –Oct 9 Fall Gifted Screening 31 Sep 28- Oct 9 INVIEW / Terra Nova (Elementary) Oct 14 PSAT (High Schools) Oct 16 End of First Quarter. Students Report. SEPTEMBER MARCH (39 Instructional Days, 44 Staff Days). M T W T F M T W T F Oct 21 – 27 3rd Grade Fall ELA. 1 2 3 4 1 2 3 4 5 Nov 2 Conference Comp Day –School Closed Nov 3 Election Day – Conference Day. 7 8 9 10 11 8 9 10 11 12 Q No Students. 14 M 15 16 17 18 15 16 17 18 19 Nov 9 Midterm Week 21 22 23 24 25 22 23 24 25 26 Nov 11 Veterans’ Day. Holiday Observance. Schools Closed. 28 29 30 29 30 31 Nov 25 Conference Day. No Students. Nov 26 Thanksgiving. Holiday Observance. OCTOBER APRIL Nov 27 Schools Closed. Dec 1 – 11 Fall HS End of Course M T W T F M T W T F Dec 14 -18 Semester 1 Exams (High Schools) 1 2 1 2 Dec 18 End of Second Quarter.
    [Show full text]
  • The Mathematics of the Chinese, Indian, Islamic and Gregorian Calendars
    Heavenly Mathematics: The Mathematics of the Chinese, Indian, Islamic and Gregorian Calendars Helmer Aslaksen Department of Mathematics National University of Singapore [email protected] www.math.nus.edu.sg/aslaksen/ www.chinesecalendar.net 1 Public Holidays There are 11 public holidays in Singapore. Three of them are secular. 1. New Year’s Day 2. Labour Day 3. National Day The remaining eight cultural, racial or reli- gious holidays consist of two Chinese, two Muslim, two Indian and two Christian. 2 Cultural, Racial or Religious Holidays 1. Chinese New Year and day after 2. Good Friday 3. Vesak Day 4. Deepavali 5. Christmas Day 6. Hari Raya Puasa 7. Hari Raya Haji Listed in order, except for the Muslim hol- idays, which can occur anytime during the year. Christmas Day falls on a fixed date, but all the others move. 3 A Quick Course in Astronomy The Earth revolves counterclockwise around the Sun in an elliptical orbit. The Earth ro- tates counterclockwise around an axis that is tilted 23.5 degrees. March equinox June December solstice solstice September equinox E E N S N S W W June equi Dec June equi Dec sol sol sol sol Beijing Singapore In the northern hemisphere, the day will be longest at the June solstice and shortest at the December solstice. At the two equinoxes day and night will be equally long. The equi- noxes and solstices are called the seasonal markers. 4 The Year The tropical year (or solar year) is the time from one March equinox to the next. The mean value is 365.2422 days.
    [Show full text]
  • Capricious Suntime
    [Physics in daily life] I L.J.F. (Jo) Hermans - Leiden University, e Netherlands - [email protected] - DOI: 10.1051/epn/2011202 Capricious suntime t what time of the day does the sun reach its is that the solar time will gradually deviate from the time highest point, or culmination point, when on our watch. We expect this‘eccentricity effect’ to show a its position is exactly in the South? e ans - sine-like behaviour with a period of a year. A wer to this question is not so trivial. For ere is a second, even more important complication. It is one thing, it depends on our location within our time due to the fact that the rotational axis of the earth is not zone. For Berlin, which is near the Eastern end of the perpendicular to the ecliptic, but is tilted by about 23.5 Central European time zone, it may happen around degrees. is is, aer all, the cause of our seasons. To noon, whereas in Paris it may be close to 1 p.m. (we understand this ‘tilt effect’ we must realise that what mat - ignore the daylight saving ters for the deviation in time time which adds an extra is the variation of the sun’s hour in the summer). horizontal motion against But even for a fixed loca - the stellar background tion, the time at which the during the year. In mid- sun reaches its culmination summer and mid-winter, point varies throughout the when the sun reaches its year in a surprising way.
    [Show full text]
  • Day-Ahead Market Enhancements Phase 1: 15-Minute Scheduling
    Day-Ahead Market Enhancements Phase 1: 15-minute scheduling Phase 2: flexible ramping product Stakeholder Meeting March 7, 2019 Agenda Time Topic Presenter 10:00 – 10:10 Welcome and Introductions Kristina Osborne 10:10 – 12:00 Phase 1: 15-Minute Granularity Megan Poage 12:00 – 1:00 Lunch 1:00 – 3:20 Phase 2: Flexible Ramping Product Elliott Nethercutt & and Market Formulation George Angelidis 3:20 – 3:30 Next Steps Kristina Osborne Page 2 DAME initiative has been split into in two phases for policy development and implementation • Phase 1: 15-Minute Granularity – 15-minute scheduling – 15-minute bidding • Phase 2: Day-Ahead Flexible Ramping Product (FRP) – Day-ahead market formulation – Introduction of day-ahead flexible ramping product – Improve deliverability of FRP and ancillary services (AS) – Re-optimization of AS in real-time 15-minute market Page 3 ISO Policy Initiative Stakeholder Process for DAME Phase 1 POLICY AND PLAN DEVELOPMENT Issue Straw Draft Final June 2018 July 2018 Paper Proposal Proposal EIM GB ISO Board Implementation Fall 2020 Stakeholder Input We are here Page 4 DAME Phase 1 schedule • Third Revised Straw Proposal – March 2019 • Draft Final Proposal – April 2019 • EIM Governing Body – June 2019 • ISO Board of Governors – July 2019 • Implementation – Fall 2020 Page 5 ISO Policy Initiative Stakeholder Process for DAME Phase 2 POLICY AND PLAN DEVELOPMENT Issue Straw Draft Final Q4 2019 Q4 2019 Paper Proposal Proposal EIM GB ISO Board Implementation Fall 2021 Stakeholder Input We are here Page 6 DAME Phase 2 schedule • Issue Paper/Straw Proposal – March 2019 • Revised Straw Proposal – Summer 2019 • Draft Final Proposal – Fall 2019 • EIM GB and BOG decision – Q4 2019 • Implementation – Fall 2021 Page 7 Day-Ahead Market Enhancements Third Revised Straw Proposal 15-MINUTE GRANULARITY Megan Poage Sr.
    [Show full text]
  • Solar Engineering Basics
    Solar Energy Fundamentals Course No: M04-018 Credit: 4 PDH Harlan H. Bengtson, PhD, P.E. Continuing Education and Development, Inc. 22 Stonewall Court Woodcliff Lake, NJ 07677 P: (877) 322-5800 [email protected] Solar Energy Fundamentals Harlan H. Bengtson, PhD, P.E. COURSE CONTENT 1. Introduction Solar energy travels from the sun to the earth in the form of electromagnetic radiation. In this course properties of electromagnetic radiation will be discussed and basic calculations for electromagnetic radiation will be described. Several solar position parameters will be discussed along with means of calculating values for them. The major methods by which solar radiation is converted into other useable forms of energy will be discussed briefly. Extraterrestrial solar radiation (that striking the earth’s outer atmosphere) will be discussed and means of estimating its value at a given location and time will be presented. Finally there will be a presentation of how to obtain values for the average monthly rate of solar radiation striking the surface of a typical solar collector, at a specified location in the United States for a given month. Numerous examples are included to illustrate the calculations and data retrieval methods presented. Image Credit: NOAA, Earth System Research Laboratory 1 • Be able to calculate wavelength if given frequency for specified electromagnetic radiation. • Be able to calculate frequency if given wavelength for specified electromagnetic radiation. • Know the meaning of absorbance, reflectance and transmittance as applied to a surface receiving electromagnetic radiation and be able to make calculations with those parameters. • Be able to obtain or calculate values for solar declination, solar hour angle, solar altitude angle, sunrise angle, and sunset angle.
    [Show full text]
  • Prime Meridian ×
    This website would like to remind you: Your browser (Apple Safari 4) is out of date. Update your browser for more × security, comfort and the best experience on this site. Encyclopedic Entry prime meridian For the complete encyclopedic entry with media resources, visit: http://education.nationalgeographic.com/encyclopedia/prime-meridian/ The prime meridian is the line of 0 longitude, the starting point for measuring distance both east and west around the Earth. The prime meridian is arbitrary, meaning it could be chosen to be anywhere. Any line of longitude (a meridian) can serve as the 0 longitude line. However, there is an international agreement that the meridian that runs through Greenwich, England, is considered the official prime meridian. Governments did not always agree that the Greenwich meridian was the prime meridian, making navigation over long distances very difficult. Different countries published maps and charts with longitude based on the meridian passing through their capital city. France would publish maps with 0 longitude running through Paris. Cartographers in China would publish maps with 0 longitude running through Beijing. Even different parts of the same country published materials based on local meridians. Finally, at an international convention called by U.S. President Chester Arthur in 1884, representatives from 25 countries agreed to pick a single, standard meridian. They chose the meridian passing through the Royal Observatory in Greenwich, England. The Greenwich Meridian became the international standard for the prime meridian. UTC The prime meridian also sets Coordinated Universal Time (UTC). UTC never changes for daylight savings or anything else. Just as the prime meridian is the standard for longitude, UTC is the standard for time.
    [Show full text]
  • How Long Is a Year.Pdf
    How Long Is A Year? Dr. Bryan Mendez Space Sciences Laboratory UC Berkeley Keeping Time The basic unit of time is a Day. Different starting points: • Sunrise, • Noon, • Sunset, • Midnight tied to the Sun’s motion. Universal Time uses midnight as the starting point of a day. Length: sunrise to sunrise, sunset to sunset? Day Noon to noon – The seasonal motion of the Sun changes its rise and set times, so sunrise to sunrise would be a variable measure. Noon to noon is far more constant. Noon: time of the Sun’s transit of the meridian Stellarium View and measure a day Day Aday is caused by Earth’s motion: spinning on an axis and orbiting around the Sun. Earth’s spin is very regular (daily variations on the order of a few milliseconds, due to internal rearrangement of Earth’s mass and external gravitational forces primarily from the Moon and Sun). Synodic Day Noon to noon = synodic or solar day (point 1 to 3). This is not the time for one complete spin of Earth (1 to 2). Because Earth also orbits at the same time as it is spinning, it takes a little extra time for the Sun to come back to noon after one complete spin. Because the orbit is elliptical, when Earth is closest to the Sun it is moving faster, and it takes longer to bring the Sun back around to noon. When Earth is farther it moves slower and it takes less time to rotate the Sun back to noon. Mean Solar Day is an average of the amount time it takes to go from noon to noon throughout an orbit = 24 Hours Real solar day varies by up to 30 seconds depending on the time of year.
    [Show full text]
  • The Determination of Longitude in Landsurveying.” by ROBERTHENRY BURNSIDE DOWSES, Assoc
    316 DOWNES ON LONGITUDE IN LAXD SUIWETISG. [Selected (Paper No. 3027.) The Determination of Longitude in LandSurveying.” By ROBERTHENRY BURNSIDE DOWSES, Assoc. M. Inst. C.E. THISPaper is presented as a sequel tothe Author’s former communication on “Practical Astronomy as applied inLand Surveying.”’ It is not generally possible for a surveyor in the field to obtain accurate determinationsof longitude unless furnished with more powerful instruments than is usually the case, except in geodetic camps; still, by the methods here given, he may with care obtain results near the truth, the error being only instrumental. There are threesuch methods for obtaining longitudes. Method 1. By Telrgrcrph or by Chronometer.-In either case it is necessary to obtain the truemean time of the place with accuracy, by means of an observation of the sun or z star; then, if fitted with a field telegraph connected with some knownlongitude, the true mean time of that place is obtained by telegraph and carefully compared withthe observed true mean time atthe observer’s place, andthe difference between thesetimes is the difference of longitude required. With a reliable chronometer set totrue Greenwich mean time, or that of anyother known observatory, the difference between the times of the place and the time of the chronometer must be noted, when the difference of longitude is directly deduced. Thisis the simplest method where a camp is furnisl~ed with eitherof these appliances, which is comparatively rarely the case. Method 2. By Lunar Distances.-This observation is one requiring great care, accurately adjusted instruments, and some littleskill to obtain good results;and the calculations are somewhat laborious.
    [Show full text]
  • The Geology of Cuba: a Brief Cuba: a of the Geology It’S Time—Renew Your GSA Membership and Save 15% and Save Membership GSA Time—Renew Your It’S
    It’s Time—Renew Your GSA Membership and Save 15% OCTOBER | VOL. 26, 2016 10 NO. A PUBLICATION OF THE GEOLOGICAL SOCIETY OF AMERICA® The geology of Cuba: A brief overview and synthesis OCTOBER 2016 | VOLUME 26, NUMBER 10 Featured Article GSA TODAY (ISSN 1052-5173 USPS 0456-530) prints news and information for more than 26,000 GSA member readers and subscribing libraries, with 11 monthly issues (March/ April is a combined issue). GSA TODAY is published by The SCIENCE Geological Society of America® Inc. (GSA) with offices at 3300 Penrose Place, Boulder, Colorado, USA, and a mail- 4 The geology of Cuba: A brief overview ing address of P.O. Box 9140, Boulder, CO 80301-9140, USA. and synthesis GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, M.A. Iturralde-Vinent, A. García-Casco, regardless of race, citizenship, gender, sexual orientation, Y. Rojas-Agramonte, J.A. Proenza, J.B. Murphy, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. and R.J. Stern © 2016 The Geological Society of America Inc. All rights Cover: Valle de Viñales, Pinar del Río Province, western reserved. Copyright not claimed on content prepared Cuba. Karstic relief on passive margin Upper Jurassic and wholly by U.S. government employees within the scope of Cretaceous limestones. The world-famous Cuban tobacco is their employment. Individual scientists are hereby granted permission, without fees or request to GSA, to use a single grown in this valley. Photo by Antonio García Casco, 31 July figure, table, and/or brief paragraph of text in subsequent 2014.
    [Show full text]
  • Sidereal Time Distribution in Large-Scale of Orbits by Usingastronomical Algorithm Method
    International Journal of Science and Research (IJSR) ISSN (Online): 2319-7064 Index Copernicus Value (2013): 6.14 | Impact Factor (2013): 4.438 Sidereal Time Distribution in Large-Scale of Orbits by usingAstronomical Algorithm Method Kutaiba Sabah Nimma 1UniversitiTenagaNasional,Electrical Engineering Department, Selangor, Malaysia Abstract: Sidereal Time literally means star time. The time we are used to using in our everyday lives is Solar Time.Astronomy, time based upon the rotation of the earth with respect to the distant stars, the sidereal day being the unit of measurement.Traditionally, the sidereal day is described as the time it takes for the Earth to complete one rotation relative to the stars, and help astronomers to keep them telescops directions on a given star in a night sky. In other words, earth’s rate of rotation determine according to fixed stars which is controlling the time scale of sidereal time. Many reserachers are concerned about how long the earth takes to spin based on fixed stars since the earth does not actually spin around 360 degrees in one solar day.Furthermore, the computations of the sidereal time needs to take a long time to calculate the number of the Julian centuries. This paper shows a new method of calculating the Sidereal Time, which is very important to determine the stars location at any given time. In addition, this method provdes high accuracy results with short time of calculation. Keywords: Sidereal time; Orbit allocation;Geostationary Orbit;SolarDays;Sidereal Day 1. Introduction (the upper meridian) in the sky[6]. Solar time is what the time we all use where a day is defined as 24 hours, which is The word "sidereal" comes from the Latin word sider, the average time that it takes for the sun to return to its meaning star.
    [Show full text]