Celestial Clock - the Sun, the Moon, and the Stars
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What Causes the Seasons? – How Does the Orientation of Earth's Axis Change with Time?
2.2 The Reason for Seasons • Our goals for learning: – What causes the seasons? – How does the orientation of Earth's axis change with time? © 2014 Pearson Education, Inc. Thought Question TRUE OR FALSE? Earth is closer to the Sun in summer and farther from the Sun in winter. © 2014 Pearson Education, Inc. Thought Question TRUE OR FALSE? Earth is closer to the Sun in summer and farther from the Sun in winter. Hint: When it is summer in America, it is winter in Australia. © 2014 Pearson Education, Inc. Thought Question TRUE OR FALSE! Earth is closer to the Sun in summer and farther from the Sun in winter. • Seasons are opposite in the N and S hemispheres, so distance cannot be the reason. • The real reason for seasons involves Earth's axis tilt. © 2014 Pearson Education, Inc. What causes the seasons? © 2014 Pearson Education, Inc. Axis tilt changes directness of sunlight during the year. © 2014 Pearson Education, Inc. Sun's altitude also changes with seasons Sun’s position at noon in summer: Higher altitude means more direct sunlight. Sun’s position at noon in winter: Lower altitude means less direct sunlight. Summary: The Real Reason for Seasons • Earth's axis points in the same direction (to Polaris) all year round, so its orientation relative to the Sun changes as Earth orbits the Sun. • Summer occurs in your hemisphere when sunlight hits it more directly; winter occurs when the sunlight is less direct. • AXIS TILT is the key to the seasons; without it, we would not have seasons on Earth. -
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. -
The Basques of Lapurdi, Zuberoa, and Lower Navarre Their History and Their Traditions
Center for Basque Studies Basque Classics Series, No. 6 The Basques of Lapurdi, Zuberoa, and Lower Navarre Their History and Their Traditions by Philippe Veyrin Translated by Andrew Brown Center for Basque Studies University of Nevada, Reno Reno, Nevada This book was published with generous financial support obtained by the Association of Friends of the Center for Basque Studies from the Provincial Government of Bizkaia. Basque Classics Series, No. 6 Series Editors: William A. Douglass, Gregorio Monreal, and Pello Salaburu Center for Basque Studies University of Nevada, Reno Reno, Nevada 89557 http://basque.unr.edu Copyright © 2011 by the Center for Basque Studies All rights reserved. Printed in the United States of America Cover and series design © 2011 by Jose Luis Agote Cover illustration: Xiberoko maskaradak (Maskaradak of Zuberoa), drawing by Paul-Adolph Kaufman, 1906 Library of Congress Cataloging-in-Publication Data Veyrin, Philippe, 1900-1962. [Basques de Labourd, de Soule et de Basse Navarre. English] The Basques of Lapurdi, Zuberoa, and Lower Navarre : their history and their traditions / by Philippe Veyrin ; with an introduction by Sandra Ott ; translated by Andrew Brown. p. cm. Translation of: Les Basques, de Labourd, de Soule et de Basse Navarre Includes bibliographical references and index. Summary: “Classic book on the Basques of Iparralde (French Basque Country) originally published in 1942, treating Basque history and culture in the region”--Provided by publisher. ISBN 978-1-877802-99-7 (hardcover) 1. Pays Basque (France)--Description and travel. 2. Pays Basque (France)-- History. I. Title. DC611.B313V513 2011 944’.716--dc22 2011001810 Contents List of Illustrations..................................................... vii Note on Basque Orthography......................................... -
Autumnal Equinox in Northern Hemisphere
Autumnal Equinox in Northern Hemisphere drishtiias.com/printpdf/autumnal-equinox-in-northern-hemisphere Why in News On 22nd September 2020, the day and night was almost equal in most locations marking the start of autumn in the Northern Hemisphere which lasts until the winter solstice (December 21 or 22). Similarly, the Vernal equinox falls around March 21, marking the start of spring in the Northern Hemisphere. In the Southern Hemisphere the seasons are reversed (Christmas is celebrated in Australia and New Zealand in the summer season). Key Points 1/3 About: The word equinox is derived from two Latin words - aequus (equal) and nox (night). There are only two times of the year when the Earth's axis is tilted neither toward nor away from the sun, resulting in a nearly equal amount of daylight and darkness at all latitudes. These events are referred to as Equinoxes. The equinoxes happen in March (about March 21) and September (about September 23). These are the days when the Sun is exactly above the Equator, which makes day and night of equal length. It can be noted that the most places on Earth receive more than 12 hours of daylight on equinoxes. This is because of the atmospheric refraction of sunlight and how the length of the day is defined. The equinoxes are prime time for Northern Lights – geomagnetic activities are twice more likely to take place in the spring and fall time, than in the summer or winter. Varying Dates: While the September equinox usually occurs on September 22 or 23, it can very rarely fall on September 21 or September 24. -
PRIME MERIDIAN a Place Is
Lines of Latitude and Longitude help us to answer a key geographical question: “Where am I?” What are Lines of Latitude and Longitude? Lines of Latitude and Longitude refer to the grid system of imaginary lines you will find on a map or globe. PARALLELS of Latitude and MERIDIANS of Longitude form an invisible grid over the earth’s surface and assist in pinpointing any location on Earth with great accuracy; everywhere has its own unique grid location, and this is expressed in terms of LATITUDE and LONGITUDE COORDINATES. Lines of LATITUDE are the ‘horizontal’ lines. They tell us whether a place is located in the NORTHERN or the SOUTHERN HEMISPHERE as well as how far North or South from the EQUATOR it is. Lines of LONGITUDE are the ‘vertical’ lines. They indicate how far East or West of the PRIME MERIDIAN a place is. • The EQUATOR is the 0° LATITUDE LINE. o North of the EQUATOR is the NORTHERN HEMISPHERE. o South of the EQUATOR is the SOUTHERN HEMISPHERE. • Lines of Latitude cross the PRIME MERIDIAN (longitude line) at right angles (90°). • Lines of Latitude circle the globe/world in an east- west direction. • Lines of Latitude are also known as PARALLELS. o As they are parallel to the Equator and apart always at the same distance. • Lines of Latitude measure distance north or south from the equator i.e. how far north or south a point lies from the Equator. • The distance between degree lines is about 69 miles (or about 110km). o A DEGREE (°) equals 60 minutes - 60’. -
307 Lesson 21: Eratosthenes' Measurement of the Earth the Most
307 Lesson 21: Eratosthenes’ Measurement of the Earth The most important parallel of latitude is the equator; it is the only parallel of latitude that is a great circle. However, in the previous lesson we learned about four other parallels of latitude which are of great importance because of the relative geometry of the Earth and the Sun. These are the Tropics of Cancer and Capricorn and the Arctic and Antarctic Circles. We briefly review the basic facts about these four parallels. At each moment on the day of the summer solstice, there is a single point on the surface of the Earth that is closet to the Sun. As the Earth rotates through the day of the summer solstice, this closest point to the Sun moves around the surface of the Earth and traces a parallel of latitude called the Tropic of Cancer. Another description of the Tropic of Cancer is that it is the set of all points on the Earth’s surface where the Sun is directly overhead at solar noon on the day of the summer solstice. The latitude coordinate of the Tropic of Cancer equals the measure of the angle that the Earth’s axis makes with the perpendicular to the ecliptic plane: approximately 23.5º N. On the day of the summer solstice, as the Earth rotates about its axis, the terminator (the division between daytime and nighttime) moves, and its northernmost point traces out a parallel of latitude called the Arctic Circle. Similarly, as the Earth rotates, the southernmost point of the terminator traces out a parallel of latitude called the Antarctic Circle. -
The Sun-Earth-Moon System 9
CHAPTER 20 LESSON 1 The Sun-Earth-Moon System Earth’s Motion Key Concepts • How does Earth move? What do you think? Read the two statements below and decide • Why is Earth warmer at the whether you agree or disagree with them. Place an A in the Before column equator and colder at the if you agree with the statement or a D if you disagree. After you’ve read poles? this lesson, reread the statements to see if you have changed your mind. • Why do the seasons change Before Statement After as Earth moves around 1. Earth’s movement around the Sun causes the Sun? sunrises and sunsets. 2. Earth has seasons because its distance from the Sun changes throughout the year. Earth and the Sun Identify Main Ideas Highlight each head in one If you look around you, it does not seem as if Earth color. Use another color to is moving. The ground, trees, and buildings do not seem to highlight key words in the be moving. But Earth is always in motion. It spins and paragraphs under the head moves around the Sun. Earth’s motion causes changes on that explain or support the Earth. As Earth spins, day changes to night and back to day head. Use your highlighting again. The seasons change as Earth moves around the Sun. to review the lesson. Summer turns to winter because Earth’s motion changes how energy from the Sun spreads out over Earth’s surface. The Sun The nearest star to Earth is the Sun. The Sun is about 150 million km from Earth. -
North Pole • South Pole
Divisions of the Earth The Earth can be divided in many ways. Today, we will learn about the seven most important divisions on the planet: • equator • northern hemisphere • southern hemisphere • tropic of Capricorn • tropic of Cancer • North Pole • South Pole Let’s find out more! Equator • The equator is an imaginary line that divides the Earth in half. • The equator is an equal distance between the North and South Poles. • The weather on the equator is hot all year round. • At the equator, day and night are both 12 hours long. Did You Know? Although the weather is generally hot, there is a mountain on the equator where you can ski! Challenge Question Why do you think places at the equator are hot? Northern Hemisphere • The part of the Earth north of the equator is called the northern hemisphere. • 80% of the world’s population lives in the northern hemisphere. • 90% of land is in the northern hemisphere. • The northern hemisphere includes all of north America, Europe and most of Asia and Africa. Southern Hemisphere • The part of the Earth south of the equator is called the southern hemisphere. • Only 20% of the world’s population lives in the southern hemisphere. • 90% of the planet’s water is in the southern hemisphere. • The southern hemisphere includes all of Australia, Antarctica and most of South America. Did You Know? When it is winter in the southern hemisphere, it is summer in the northern hemisphere! Tropic of Cancer • The tropic of Cancer is an imaginary line in the northern hemisphere. • It is also called the northern tropic. -
Equinox - Wikipedia, the Free Encyclopedia
Equinox - Wikipedia, the free encyclopedia Your continued donations keep Wikipedia running! Equinox From Wikipedia, the free encyclopedia Jump to: navigation, search For other uses, see Equinox (disambiguation). UTC Date and Time of Solstice and Equinox Equinox Solstice Equinox Solstice year Mar June Sept Dec day time day time day time day time 2002 20 19:16 21 13:24 23 04:55 22 01:14 2003 21 01:00 21 19:10 23 10:47 22 07:04 2004 20 06:49 21 00:57 22 16:30 21 12:42 2005 20 12:33 21 06:46 22 22:23 21 18:35 2006 20 18:26 21 12:26 23 04:03 22 00:22 2007 21 00:07 21 18:06 23 09:51 22 06:08 Illumination of the Earth by the Sun on 2008 20 05:48 20 23:59 22 15:44 21 12:04 the day of equinox, (ignoring twilight). 2009 20 11:44 21 05:45 22 21:18 21 17:47 2010 20 17:32 21 11:28 23 03:09 21 23:38 2011 20 23:21 21 17:16 23 09:04 22 05:30 2012 20 05:14 20 23:09 22 14:49 21 11:11 2013 20 11:02 21 05:04 22 20:44 21 17:11 2014 20 16:57 21 10:51 23 02:29 21 23:03 The Earth in its orbit around the Sun causes the Sun to appear on the celestial sphere moving over the ecliptic (red), which is tilted on the equator (blue). -
Principal Weather Systems in Subtropical and Tropical Zones - I
ENVIRONMENTAL STRUCTURE AND FUNCTION: CLIMATE SYSTEM – Vol. I - Principal Weather Systems in Subtropical and Tropical Zones - I. G. Sitnikov PRINCIPAL WEATHER SYSTEMS IN SUBTROPICAL AND TROPICAL ZONES I. G. Sitnikov The Hydrometeorological Research Center of Russia, Moscow, Russia Keywords: Cloud cluster, depression, easterly, general circulation, hurricane, interaction with extratropics, intertropical convergence zone, mesoconvective system, monsoon, numerical modeling, quasi-biennial oscillation, squall line, subtropical highs, tornado, trade winds, monsoons, tropical cyclone, tropical disturbances, typhoon, waves Contents 1. Introduction 2. The general circulation: tropics and subtropics 2.1. Main Elements 2.2. Trade Winds 2.3. The Intertropical Convergence Zone 2.4. Monsoons 3. Main perturbation systems in tropical and subtropical zones 3.1. Tropical Cyclones 3.2. Waves in the Tropical Atmosphere 3.2.1. Easterly Waves 3.2.2. Other Waves in the Tropical and Equatorial Zone 3.3. Monsoon Depressions and Monsoon Lows 3.4. Madden-Julian Oscillation (MJO) 3.5. Quasi-biennial Oscillation (QBO) 3.6. Mesoscale Rain and Convective Systems 3.7. Cloud Clusters and Squall Lines 3.8. Tornadoes 4. Conclusion Glossary Bibliography Biographical Sketch SummaryUNESCO – EOLSS The principal weatherSAMPLE systems in the subtropi calCHAPTERS and tropical zones may be divided into two classes: 1) those comprising immutable links of the general atmospheric circulation (subtropical Highs as centers of action of the atmosphere, trade winds, the Intertropical convergence zone, monsoons) and 2) main perturbation systems in the tropics and subtropics (tropical cyclones, easterly and some other waves, monsoon depressions and Lows, the quasi-biennial oscillation and Madden-Julian oscillation, mesoscale rain and convective systems, cloud clusters and squall lines, small-scale vortices like tornadoes etc.). -
NOWRUZ FESTIVAL Common Cultural Heritage of the ECO Region
THE QUARTERLY CULTURAL MAGAZINE OF ECO CULTURAL INSTITUTE (ECI) ECO HERITAGE ISSUE 28, VOLUME 9, NOWRUZ SPECIAL ISSUE ISSN 2008-546X NOWRUZ FESTIVAL Common Cultural Heritage of the ECO Region ISSN 2008-546X 9 772008 546002 Called whether Tartars, Turks or Afghans, we ف نی ن ت ی هن ا غا م و ی رتک و تار م ,Belong to one great garden, one great tree چم ی خ ی ن زاد م و از یک شا سار م .Born of a springtide that was glorious تمی ب س ز رنگ و و رب ما رحام ا ت .Distinction of colour is a sin for us ٔ هک ما رپورده یک نو بهاریم A Persian Poem by Sir Muhammad Iqbal( ), عﻻهم محمداقبال the most prominent poet of Pakistan from his book " "PAYAM-I-MASHRIQ" (Message from the East), English translation: M. HADI HUSSAIN Publisher ECO Cultural Institute (ECI) Supervision Sarvar Bakhti, President, THE QUARTERLY CULTURAL MAGAZINE OF ECO CULTURAL INSTITUTE (ECI) ECO Cultural Institute (ECI) ECO HERITAGE ISSUE 28, VOLUME 9, NOWRUZ SPECIAL ISSUE ISSN 2008-546X Director-in-Charge Mehdi Omraninejad Chief Editor Said Reza Huseini Senior Copy Editor Nastaran Nosratzadegan NOWRUZ FESTIVAL Common Cultural Heritage of the ECO Region Editorial Board Nazif Mohib Shahrani (Afghanistan) Mohammad Sakhi Rezaie (Afghanistan) Jahangir Selimkhanov (Rep. Azerbaijan) Mandana Tishehyar (Iran) ISSN 2008-546X 9 772008 546002 Elaheh Koulaee (Iran) Dosbol Baikonakov (Kazakhstan) Aizhan Bekkulova (Kazakhstan) Cover photo by: Afshin Shahroudi Inam ul-Haq Javeed (Pakistan) (The photo was higly commended in the Photo section of the Shaheena Ayub Bhatti (Pakistan) ECO International Visual Arts Festival 2012) Asliddin Nizami (Tajikistan) Dilshod Rahimi (Tajikistan) Hicabi Kırlangı (Turkey) Advisory Board Prof. -
Equinoxes Day and Night Are Not Exactly of Equal Length at the Time Of
Equinoxes Day and night are not exactly of equal length at the time of the March and September equinoxes. The dates on which day and night are each 12 hours occur a few days before and after the equinoxes. The specific dates of this occurrence are different for different latitudes. On the day of an equinox, the geometric center of the Sun's disk crosses the equator, and this point is above the horizon for 12 hours everywhere on the Earth. However, the Sun is not simply a geometric point. Sunrise is defined as the instant when the leading edge of the Sun's disk becomes visible on the horizon, whereas sunset is the instant when the trailing edge of the disk disappears below the horizon. These are the moments of first and last direct sunlight. At these times the center of the disk is below the horizon. Furthermore, atmospheric refraction causes the Sun's disk to appear higher in the sky than it would if the Earth had no atmosphere. Thus, in the morning the upper edge of the disk is visible for several minutes before the geometric edge of the disk reaches the horizon. Similarly, in the evening the upper edge of the disk disappears several minutes after the geometric disk has passed below the horizon. The times of sunrise and sunset in almanacs are calculated for the normal atmospheric refraction of 34 minutes of arc and a semidiameter of 16 minutes of arc for the disk. Therefore, at the tabulated time the geometric center of the Sun is actually 50 minutes of arc below a regular and unobstructed horizon for an observer on the surface of the Earth in a level region.