Announcements No lab after lecture tonight because of the 1 st Quarter night last Tuesday Homework: Chapter 2 # 2, 3, 4, 5, 7 & 8 Binoculars are available.

Slides:



Advertisements
Similar presentations
Earth’s Motion Days and Years.
Advertisements

The Moon orbits the Earth and returns to the same right ascension every days. (It moves eastward against the background of stars.) This is the sidereal.
Coordinate System & Time/Calendar
PHYS216 Practical Astrophysics Lecture 3 – Coordinate Systems 2
Chapter S1 Celestial Timekeeping and Navigation
Chapter S1 Celestial Timekeeping and Navigation
Lecture 2 Astron 1 Instructor: Dr. Babar Ali Fall 2014Astron 1Dr. Ali.
A100 Oct. 13 Keeping Time READ Essay 2 – Keeping Time in the text, pp
More cycles in the sky Announcements (no, not that kind)
The Day. Shadow Clock When positioned correctly, the value on a sundial in DeKalb tells A. universal time. B. local sidereal time. C. local mean solar.
Prof. John Hearnshaw ASTR211: COORDINATES AND TIME Coordinates and time Sections 9 – 17.
UNITS OF TIME.
Seasons and Calendar Lecture 4.
Announcements Homework Set 1 is due today
Astronomy 100 Tuesday, Thursday 2:30 - 3:45 pm Tom Burbine
ASTR 2310 Chapter 1: Example Problems
CALENDARSCALENDARS Chapter 3 The YEAR 2000 WAS YearAccording to: 1997Christ’s actual birth circa 4 BC 2753Old Roman calendar 2749Ancient Babylonian calendar.
Time Michelle Houck April 28, 2008, 4:15pm EST. What is time? Standard by which we measure Standard by which we measure One of the fundamental units of.
The Whirligig of Time Astronomy 360. Essay 2 Keeping Time The length of the day is set by the earth’s rotation on its axis With some reservations! The.
January 17, 2006Astronomy Chapter 3 Earth, Moon, and Sky How do we locate objects in the sky? How are seasons and tides related to astronomy? What.
AST 208 Topics Time and celestial coordinates. Telescopes.
An Earth Day Sidereal Day: 23 hr 56 min 4 sec Motion relative to background stars Mean Solar Day: 24 hours The average time between meridian crossings.
When does a “day” start?   set Universal Time using the Greenwich Meridian (Britannia rules the waves...)       since "noon" drifts around the Earth,
LECTURE 2, AUGUST 26, 2010 ASTR 101, SECTION 3 INSTRUCTOR, JACK BRANDT 1ASTR 101-3, FALL 2010.
LONGITUDE (to measure East-West), is all a matter of time…
Modern Navigation Thomas Herring MW 11:00-12:30 Room
Social Studies 9 Chapter 2 Time Zones.  A time zone is a region of the Earth that has adopted the same standard time, usually referred to as the local.
The Celestial Sphere The 88 official constellations cover the celestial sphere. If you do not have a model of the celestial sphere to bring to class, you.
LESSON 18: Time Learning ObjectivesLearning Objectives –Comprehend the longitude/time relationship, time conversion, zone time determination, and motions.
James T. Shipman Jerry D. Wilson Charles A. Higgins, Jr. Place and Time Chapter 15.
Announcements Homework set 1 is due today
2. The Celestial Sphere Goals Goals: 1. Gain familiarity with the basic co- ordinate systems used in astronomy. 2. Tackle simple problems in practical.
The Sun-Earth-Moon System (Chapter 3). Student Learning Objectives Associate cycles in the sky with time Describe why Earth has seasons Determine the.
Time What Time Is It? Before 1884, almost every town in the world kept its own local time. There were no national or international conventions which set.
The Seasons There would be no seasons if the Earth were not tilted on it’s axis!  Nick Devereux 2006.
Units of Time Based on Astronomical Motions and Objects Day: New: Time required for the earth to complete one rotation. Week: Based on 7 celestial bodies.
Chapter 16 Earth in Space. The Shape of the Earth The Earth is not a perfectly round sphere as believed by the ancient Greeks. It is flattened at the.
Word of the Day Nautical Mile: One minute of arc length of latitude or longitude at the equator, or 1852m.
EIS 2.2 Scaling of the Sun, Earth, Moon System
Earth’s Orbit and the Seasons. Seasons on the Earth.
Time “Does anybody really know what time it is? Does anybody really care?” – Chicago.
Intro To Astronomy.
Celestial Timekeeping
The Mathematics of Time A/P Helmer Aslaksen Dept. of Mathematics National University of Singapore
Times and Calendars Dr. Matt Wiesner Based on slides by Dr. Wei Cui
Coordinate Transformations TM, A. Tamburro Based on Slalib docs/sun67.htx/sun67.html Tested against MACRO algorithms and.
Longitude and Time.
Announcements Homework Set 1 is due today Homework set 2: Chapter 2 # 46, 50, 52, 53 & 54 + Determine the number of kilometers in 1° of longitude at the.
1 Lecture 29 Measuring Time on Earth Ozgur Unal. 2  What time is it in your hometown at the moment?  What time is it in NYC?
Rotation = 1 day, 15° per hour West to East Everything appears to rise in East and set in West.
Topic 4. How do we determine a frame of reference for time? A)Day – based upon one rotation of the Earth on its axis B)Month – based upon the length of.
Time Zones & Ellipse Pathway Objective: To map out the Earth’s time zones and draw the ellipse orbit around the sun with equinoxes and solstices.
Chapter S1 Celestial Timekeeping and Navigation
Astronomical Time Periods
The Sun-Earth-Moon System
Celestial Coordinates
Astronomical time SSP 2017.
Time Zones.
you thought of going into teaching?”
Solar time and Sidereal (Star) Time
Sidereal vs. Synodic Motion
Coordinates and Time.
-Time is based on longitude lines.
Announcements Dark Sky night Saturday night is looking iffy. Check before heading out to see if it is cancelled. Homework: Chapter.
Chapter 14 Section 2 What are time zones?
Chapter 14 Section 2 What are time zones?
Calendar Presented By S.ITHAYA EZHIL MANNA Assistant Professor In Mathematics St.Joseph’s College,Trichy-2.
Calendar.
Presentation transcript:

Announcements No lab after lecture tonight because of the 1 st Quarter night last Tuesday Homework: Chapter 2 # 2, 3, 4, 5, 7 & 8 Binoculars are available for check-out. I have six on campus and another eight out at the Farm. Telescopes can also be checked out for a weekend. They must be returned Monday. Don’t forget the Lunar Observations lab

Time

Keeping time by the Sun isn’t very accurate

The Equation of Time

Since solar time varies by location, we use standard time Each zone is 15 ° wide with allowance for political boundaries

The Earth’s rotation rate isn’t constant Terrestrial Dynamical Time corrects for the changes in Earth’s rotation rate

Sidereal Time Sidereal time is the time with respect to the background stars. One sidereal day is the true rotational period of the Earth. Uncorrected, it is 23 hours 56 minutes seconds

Calculating Sidereal Time Step 1 First: convert standard time to universal time For Central Standard Time UT = CST + 6 hours For Central Daylight Time UT = CDT + 5 hours If result is greater than 24 hrs, subtract 24 and add 1 to the date.

Calculating Sidereal Time Step 2 Determine the “solar interval” and convert to sidereal interval. The solar interval is simply the time since 0 hrs UT Solar to sidereal interval conversion: multiply by

Calculating Sidereal Time Step 3 Calculate the Greenwich Sidereal Time (GST) Look up the sidereal time at 0 hrs Greenwich for the date and add the sidereal interval to it. If you don’t own a current Astronomical Almanac, use the following formula to find GST GST = G N UT where G = GST at 0 hrs on “zeroth day” of that year (see Appendix 3 of textbook) N = number of days since the beginning of the year

Calculating Sidereal Time Step 4 Correct for local longitude Divide local longitude by 15 ° and add (if east of Greenwich) or subtract (if west of Greenwich) to GST to get Local Sidereal Time (LST) LST = GST ± (Longitude/15 °)

Julian Date Useful for calculating time interval between two dates. Julian dates start at noon UT The Julian Date (JD) is the number of days since January 1, 4713 BCE JD = 2,451, x (Year – 2000) + N + L Where N is the day number and L is the number of leap years since 2000

The Julian Calendar Instituted around 46 B.C. 1 year = days Years evenly divisible by 4 have 366 days. All other years have 365 The Tropical Year, sidereal year plus the effects of the Precession of the Equinox, is days so the Julian calendar “drifts”

The Gregorian Calendar First instituted in year = days Years evenly divisible by 4 have 366 days except century years. Only century years evenly divisible by 400 have 366 days. All other years (including century years not evenly divisible by 400) have 365 days Modified Gregorian Calendar (Never officially adopted) 1 year = Years evenly divisible by 4000 are not leap years. Otherwise the same as the Gregorian Calendar