Class VIII Geography Guide by INFANT JESUS HIGH SCHOOLTITLE Understanding Earth's Atmosphere and Climate Patterns TITLE Earth as a Rotating Sphere Lecture by Prof. MyneniTITLE Comparing Earth and Moon Shapes and MotionsTITLE Key Facts About Earth's Unique EnvironmentTITLE Explaining Life's Origins on Earth and Early FormsTITLE Proving Earth is Spherical Through ObservationTITLE First Moon Landing by Neil Armstrong in 1969TITLE Quiz on Basic Facts About Earth
The document discusses the phases of the moon. It explains that the moon does not produce its own light, but rather reflects light from the sun. As the moon orbits Earth, different portions are illuminated by the sun, appearing to change shape from our perspective on Earth. This cycle, where the illuminated portion appears to grow and then shrink over the course of around 29.5 days, is what causes the phases of the moon. The document then defines and provides images for each of the 8 main phases: new moon, waxing crescent, first quarter, waxing gibbous, full moon, waning gibbous, last quarter, and waning crescent.
Similaire à Class VIII Geography Guide by INFANT JESUS HIGH SCHOOLTITLE Understanding Earth's Atmosphere and Climate Patterns TITLE Earth as a Rotating Sphere Lecture by Prof. MyneniTITLE Comparing Earth and Moon Shapes and MotionsTITLE Key Facts About Earth's Unique EnvironmentTITLE Explaining Life's Origins on Earth and Early FormsTITLE Proving Earth is Spherical Through ObservationTITLE First Moon Landing by Neil Armstrong in 1969TITLE Quiz on Basic Facts About Earth
Similaire à Class VIII Geography Guide by INFANT JESUS HIGH SCHOOLTITLE Understanding Earth's Atmosphere and Climate Patterns TITLE Earth as a Rotating Sphere Lecture by Prof. MyneniTITLE Comparing Earth and Moon Shapes and MotionsTITLE Key Facts About Earth's Unique EnvironmentTITLE Explaining Life's Origins on Earth and Early FormsTITLE Proving Earth is Spherical Through ObservationTITLE First Moon Landing by Neil Armstrong in 1969TITLE Quiz on Basic Facts About Earth (20)
Class VIII Geography Guide by INFANT JESUS HIGH SCHOOLTITLE Understanding Earth's Atmosphere and Climate Patterns TITLE Earth as a Rotating Sphere Lecture by Prof. MyneniTITLE Comparing Earth and Moon Shapes and MotionsTITLE Key Facts About Earth's Unique EnvironmentTITLE Explaining Life's Origins on Earth and Early FormsTITLE Proving Earth is Spherical Through ObservationTITLE First Moon Landing by Neil Armstrong in 1969TITLE Quiz on Basic Facts About Earth
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3. Earth and Moon Presented by Br. Hector Pinto INFANT JESUS SCHOOL, CHALLAKERE
52. The phases of the moon are caused by the relative positions of the earth, sun, and moon. The moon goes around the earth, on average, in 27 days 7 hours 43 minutes.
132. "Here lie the bodies of Ho and Hi, Whose fate, though sad, is risible; Being slain because they could not spy Th' eclipse which was invisible." Author unknown: Said to refer to the Chinese eclipse of 2136 BC or 2159 BC. "On the day of the new moon, in the month of Hiyar, the Sun was put to shame, and went down in the daytime, with Mars in attendance." One of the earliest written records of an eclipse of the Sun, on 3 May 1375 BC, found in the city of Ugarit in Mesopotamia.(Reprinted, from Chasing the Shadow , copyright 1994 by Joel K Harris and Richard L Talcott , by permission of Kalmbach Publishing Co. "If the Sun at its rising is like a crescent and wears a crown like the Moon: the king wll capture his enemy's land; evil will leave the land, and (the land) will experience good . . . " Refers to a solar eclipse of 27 May 669 BC. Rasil the older, Babylonian scribe to the king. Quoted in Historical Eclipses and Earth's Rotation , by F Richard Stephenson, Cambridge University Press, 1997, page 125. "Nothing can be surprising any more or impossible or miraculous, now that Zeus, father of the Olympians has made night out of noonday, hiding the bright sunlight, and . . . fear has come upon mankind. After this, men can believe anything, expect anything. Don't any of you be surprised in future if land beasts change places with dolphins and go to live in their salty pastures, and get to like the sounding waves of the sea more than the land, while the dolphins prefer the mountains." May refer to a total solar eclipse of 6 April 648 BC. Archilochus, Greek poet (c680-640 BC) Quoted in Historical Eclipses and Earth's Rotation , by F Richard Stephenson, Cambridge University Press, 1997, page 338. Partly quoted in Encyclopaedia Britannica CD 98 . ECLIPSE QUOTES
136. When the moon is new or full, the gravitational forces of the sun and moon are pulling at the same side of the earth. (See the diagram below.) This occurrence creates the extra large "spring" tides. When the moon is at first and third quarter, the gravitational forces of the sun and moon are pulling at 90 degrees from each other. (see the diagram below.) This occurrence yeilds little net tides called neap tides.
137. More Fun Tidal Tales…. Every few years people that measure such things (chronologists?) need to add a leap second to the year. The Earth's rotation is decelerating at a rate of about 0.002 seconds per day per century. The Earth will eventually stop slowing down – when it’s rotation is equal to the moon’s orbital period !!! The Proxigean Tide occurs when the Moon is at its closest point in its orbit to the Earth and in its New or Full Moon phase. At this time, its tidal effect on the Earth is maximum. The times when this will happen often coincide with major coastal flooding events. Between 1997 and 2020 there will be 102 times when this will happen. The moon shows the same face to the Earth because it was deformed by Earth’s gravity when it was still molten. Earth uses this “memory” to grab the moon and slow its spin rate down. WHY ?
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141. Answer: H The sun is the largest! Our sun is the only star in our solar system. The sun is also the largest heavenly body in our solar system.
145. • Rotation:- earth rotates on its own axis from west to east. This movement is known as ROTATION • The earth takes 23 hours & 56 minutes & 4.09 seconds to complete one rotation. The average time required for the earth’s rotation from one sunrise to another sunrise is 24 hours. This period is known as a solar day.
146. Each team will need a scorekeeper ---> Effects of Rotation Life on earth is affected in many was as the earth spins on its own axis. Day & night are the result of the earth’s rotation. As the earth rotates on it’s axis only one half of the earth faces to sun at a given time. It is a day on the side of the earth which is turned towards the sun and receives light, & night for the other half of the earth which is away from the sun and is covered in darkness.
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148. Midnight Noon Sunrise Sunset The Earth rotates towards the east (CCW) The Earth’s Rotation: Daily Motion
151. The reasons for seasons – the Earth travels around the sun, and its axis of rotation is tilted by 23.5 degrees to the plane of the orbit. In July, the northern hemisphere is getting more sunlight than in January. The heliocentric model
159. It takes 8 minutes for light to reach us from the Sun! Light travels 300 000 kilometres through space every second!
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162. We can make shadows ! - by blocking out the light. Changing positions varies the size of the shadow. If you are close to the lamp, the shadow is large. If you are close to the screen, the shadow is smaller.
175. Northern Hemisphere Summer More daylight hours, more direct sunlight INFANT JESUS HIGH SCHOOL, CHALLAKERE
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177. Height of Sun Winter: The Sun rises in the southeast, stays low in the sky, and sets in the southwest. Spring: The Sun rises due east, moves higher in the sky than in winter, and sets due west. Summer: The Sun rises in the northeast, travels high (near zenith), and sets in the northwest. Fall: The Sun rises due east, travels to a medium-height in the sky, and sets due west.
199. Let's play . . . Rotation OR Revolution JEOPARDY ! Rules --->
200. Each team will need a scorekeeper ---> RULES 1. Each team will get a turn. 2-3 teams . 2. Each question is worth 3 points . 3. If a team misses a question, they forfeit 1 point . 4. The QUESTION to each ANSWER is either rotation or revolution . 5. Each answer must be in the form of a QUESTION. 6. Applause = Correct Explosion = Incorrect
201. Round One 1. The Earth spinning on its axis. Rotation Revolution 2. Going around a larger body. Rotation Revolution Revolution 4. Causes the Earth’s seasons. Revolution Rotation 5. Creates a year. 3. 24 hours. Rotation Revolution Revolution Rotation 6. The moon going around Earth. Revolution Rotation Go on to Round Two --->
202. Round Two Identify the motion being shown in each of these pictures. Each team must write their answers for each figure in the form of a question. Earth Figure #1 Rotation Revolution Figure #2 Rotation Revolution Final Round ---> Planet
203. Each team must confer and write the amount of points they would like to risk on the Final Round - The topic is Seasons .
204. X CLICK HERE FOR A FINAL MESSAGE Which team had most points? You’re all WINNERS!!! SUN The Final Round Identify the Season being shown in this picture.---> Winter Fall Summer Spring Choose the correct tree-->
244. Positioning on the Earth’s Surface Latitude and Longitude together enable the fixing of position on the Earth’s surface. Equator Latitude 0 o Latitude: ( 90 o N to 90 o S) Latitude 23½ o North Tropic of Cancer Latitude 23½ o South Tropic of Capricorn Longitude 30 o East Longitude 60 o East Longitude 30 o West Longitude 60 o West East is the direction of rotation of the Earth North Pole South Pole 23½ o 23½ o 66½ o 90 o 90 0 21 st June 22 nd December 22 nd Sept 20 th March 30 o E 60 o E 90 o E 90 o W 30 o W 60 o W Longitude 90 o East Longitude 90 o West Prime Meridian 0 o Longitude Longitude: (180 o E to 180 o W)
Part 2 -- Copernicus (15 minutes) The Copernican model was based on the hypothesis that the Earth moves, in two ways. {READ}
The Scientific Revolution (1543 – 1687) was driven by astronomy. The famous names are Copernicus… Galileo… Kepler… Newton… After their advances in science, the human view of the universe had changed dramatically! A question: At which position in our orbit around the sun are we today? A, B, C, or D? Now… this picture was the beginning of a kind of conflict between science and religion. Galileo was tried for heresy in 1633, in the midst of the scientific revolution (next slide!) His crime was to argue in favor of the Copernican model.
People used to think that the earth was flat. If they sailed too far in one direction, they thought they would fall off the edge!
Talk about the order of the phases here.
The moon appears to change shape over the course of a lunar month (one rotation around the Earth) because, from Earth, we see different parts of the moon illuminated by the sun. Since the moon gives off no light of its own, we rely on reflected sunlight to show us its surface.
The moon orbits the Earth in an ellipse. When the moon is closest to us (Perigee), it appears larger. At Apogee (furthest from Earth), it appears smaller. At Apogee, it is too small to cover the entire sun during a solar eclipse so we see only an annular eclipse.
It is waxing! The moon would be seen to be approximately in first quarter phase.
During a solar eclipse, the moon passes directly between the Earth and the sun, blocking out the sun as seen from Earth. A path of totality is formed where the moon blocks out the entire sun and observers can see a total eclipse. Outside the path of totality, only a partial eclipse can be viewed.
This graphic illustrates how the shadow of the moon falls on the Earth during a total solar eclipse. Notice how small and narrow the path of totality is.
Shadow of the moon on the Earth as observed from the MIR space station.
Total Solar Eclipse showing the corona and a few prominences off the limb (in red). When the moon blocks the light from the bright solar photosphere, we can see the much dimmer, more subtle evidence of the corona.
In a lunar eclipse, the Earth moves between the sun and the moon and casts a shadow on the moon. Lunar eclipses can come in a variety of colors from deep black to rich shades of red. The red coloring comes from light from the sun that is filtered as it passes through the Earth’s atmosphere and is bent toward the moon. That light reflects off the surface of the moon and into our eyes on Earth. Lunar eclipses are only evident when the moon is passing through the Earth’s umbral shadow.
Lunar eclipse.
Many solar system bodies partake in eclipses, transits, and occultations. Here, Jupiter’s moon, Io, casts a shadow on Jovian cloud tops.
Saturn slowly disappears behind the limb of the moon in this video sequence.
In 1973, Fred Espenak photographed this transit of the planet Mercury across the face of the sun. There are about 13 transits of Mercury each century. The next one will occur on November 8 th, 2006 and will be visible from the United States.
The 1882 transit of the planet Venus across the sun was viewed by millions of professional and amateur astronomers. This image was taken at the US Naval Observatory.
Transits of planets around distant stars are one way astronomers can detect these extra solar planets. As the planet moves in front of the star, a small percentage of the light from that the star is blocked and the light curve (shown at right) dips. When the planet moves off the limb of the star, the light curve recovers. This method is only effective when the plane of the orbit of the planet is in our line of sight. This viewgraph depicts real data of a planetary transit around the star HD209458 in the constellation of Pegasus.
Part 2 -- Copernicus (15 minutes) The Copernican model was based on the hypothesis that the Earth moves, in two ways. {READ}
Copernicus believed that the Earth rotates once per day, and revolves around the Sun once per year, as shown in the figure. Do you think these motions of the Earth affect you? Well, they produce day and night; and they produce the seasons . {READ reasons for seasons } The axis of rotation of the Earth is constant (points always in the same direction) and is at an angle to the plane of the orbit. Therefore the solar illumination in the northern or southern hemisphere varies throughout the year as the Earth goes around the sun. Solar illumination is greatest during the summer and least during the winter. A common misconception is that the Earth is closer to the sun during the summer (so that the summer is hotter). That’s false! The distance to the sun has nothing to do with the seasons. Perihelion occurs in December. In any case, summer in the northern hemisphere is winter in the southern hemisphere; and vice versa. If the distance to the sun were relevant, then the two hemispheres would have the same seasons. But, on the contrary, their seasons are out of phase by 6 months. Right now – today -- it is winter in Australia and South America. The figure shows the solstices and equinoxes (A, B, C, D). At winter solstice (for the N hemisphere) the axis of rotation points away from the sun, so that the N hemisphere gets the least solar radiation. At summer solstice (for the N hemisphere) the axis points toward the sun, so that the N hemisphere gets the most solar radiation.
We begin our workshop with a discussion of some of the misconceptions about seasons. Squirrel image taken at Kennedy Space Center http://nix.ksc.nasa.gov/info;jsessionid=as5nrgqin0a7k?id=KSC-99PC-0137&orgid=5 Blue Heron also taken at Kennedy Space Center http://mediaarchive.ksc.nasa.gov/detail.cfm?mediaid=27144
An understanding of seasons can begin with observations. What is it like here in December? In June? What is it like in other cities? In other countries? Teachers can use satellite photos like these, or look at newspapers with temperatures for various cities around the world throughout the year. Photos from http://www.nasa.gov/vision/earth/features/blue_marble.html Using data from the Moderate Resolution Imaging Spectroradiometer (MODIS) aboard NASA’s Terra satellite, scientists and data visualizers stitched together a full year’s worth of monthly observations of the land surface, coastal oceans, sea ice, and clouds into a seamless, photo-like mosaic of every square kilometer (.386 square mile) of our planet. Changes in ice are most obvious for the northern hemisphere; changes in vegetation can be seen in Africa and South America. A separate animation can be downloaded and played here: http://library01.gsfc.nasa.gov/svs/html/SVS000435.html
More information is at http://www.lpi.usra.edu/education/skytellers/seasons/about.shtml This image shows the reason Earth experiences seasons. Points we discuss using this image are: 1) Earth’s orbit around the Sun is only slightly elliptical 2) Earth’s path around the Sun brings us closer to the Sun in January. Many students think we have seasons because Earth is sometimes closer and sometimes farther from the Sun. This is correct, however, we actually are closer to the Sun in January in the Northern Hemisphere! 3) Earth’s seasons are caused by Earth’s tilt on its axis (~23 degrees). Earth’s axis essentially is fixed - it always points to the same place in the sky (on the celestial sphere) – towards Polaris. As we orbit the Sun each year, first one polar region is tilted toward the Sun, and then the other is tilted toward the Sun. When the north polar region is tilted toward the Sun (summer) the south polar region is tilted away (winter). Notes: Earth’s tilt does change over very long time periods, but for the most part, it moves between 22 and 23 degrees. Earth’s axis also wobble a bit, but over time periods of thousands of years, pointing toward different stars.
At this point, we have participants use styrofoam balls with sticks and a bright lamp to model the seasons on the Earth, with the axis of the “Earth” tilted toward a “North Star” that has been placed high in the corner of the room. For part of our orbit the northern half of Earth is tilted toward the Sun. This is summer in the northern hemisphere; there are longer periods of daylight, the Sun is higher in the sky, and the Sun's rays strike the surface more directly, giving us warmer temperatures. The north pole is in constant daylight! When the northern half of Earth is tilted toward the Sun, the southern hemisphere is tilted away. People in the southern hemisphere experience the shorter day lengths and colder temperatures of winter. During winter in the northern hemisphere, our northern axis continues to point to the North Star, but, because we have moved in our orbit around the Sun, our northern hemisphere now points away from our Sun. The north pole is completely dark and other places in the northern hemisphere experience the shorter day lengths and colder temperatures of winter as the Sun traces a lower arc across the southern sky and the Sun's rays strike the surface at a lower angle. When it is winter in the northern half of Earth, the southern hemisphere, tilted toward our Sun, has summer. During fall and spring, some locations on Earth experience similar, milder, conditions. Earth has moved to a position in its orbit where its axis is more or less perpendicular to the incoming rays of the Sun. The durations of daylight and darkness are more equally distributed across all latitudes of the globe. Solstices occur when Earth's axis is pointed directly toward our Sun. This happens twice a year during Earth's orbit. Near June 21 the north pole is tilted 23.5 degrees toward our Sun and the northern hemisphere experiences summer solstice, the longest day of the northern hemisphere year. On that same day, the southern hemisphere is tilted 23.5 degrees away from our Sun and the southern regions of Earth experience the shortest day of the year — the winter solstice. The second solstice occurs on December 21 or 22 when the north pole is tilting 23.5 degrees away from our Sun and the south pole is inclined toward it. This is the shortest day of the year in the northern hemisphere — the northern hemisphere winter solstice. Twice each year, during the equinoxes (“equal nights”), Earth's axis is not pointed toward our Sun, but is perpendicular to the incoming rays. During the equinoxes every location on our Earth (except the extreme poles) experiences 12 hours of daylight and 12 hours of darkness. The vernal or spring equinox occurs in the northern hemisphere on March 21 or 22 (the fall equinox of the southern hemisphere). September 22 or 23 marks the northern hemisphere autumnal or fall equinox. As Earth orbits our Sun, the position of its axis relative to the Sun changes. This results in a change in the observed height of our Sun above the horizon. For any given location on Earth, our Sun is observed to trace a higher path above the horizon in the summer, and a lower path in the winter. During spring and fall, it traces an intermediate path. This means that our Sun takes a greater amount of time tocross the sky in the summer and a shorter amount of time in the winter. This effect is greater as you move toward the poles; people living near the equator experience only small changes in daylight during the year. The change is more extreme toward the poles. From the National Maritime Museum During the northern hemisphere summer solstice, Earth is tilted such that the Sun's rays strike perpendicular to the surface at the Tropic of Cancer (23.5 degrees north latitude, corresponding to the tilt of Earth's axis). At (solar) noon, our Sun is directly overhead in this location (and at a decreasing height above the horizon north and south of the Tropic of Cancer). At locations north, our Sun will be at its highest position above the horizon and will take the greatest amount of time to cross the sky. All northern locations have more than 12 hours of daylight. All locations south experience less than 12 hours of daylight. Locations above the Arctic Circle (north of 66.5 degrees latitude; 90 degrees minus the tilt of Earth's axis) receive 24 hours of sunlight. Locations below the Antarctic Circle (66.5 degrees south latitude) experience 24 hours of darkness. During the northern hemisphere winter solstice, the Sun's incoming rays are perpendicular to the Tropic of Capricorn at 23.5 degrees south latitude. The Sun's path is the lowest above the horizon in locations north of the equator, and these regions experience the shortest day of the year. Between the winter and summer solstices, daylight increases as Earth continues its orbit around our Sun. During the equinoxes, sunlight strikes perpendicular to the surface at Earth's equator. All locations on Earth, regardless of latitude, experience 12 hours of daylight and 12 hours of darkness. The spring equinox marks the change from 24 hours of darkness to 24 hours of daylight at Earth's poles . In these extreme locations, our Sun moves above the horizon at the spring equinox and does not go below the horizon until the fall equinox.
More information at http://www.physicalgeography.net/fundamentals/6h.html
During this section, we demonstrate physically, using a planetarium or the horizon or the walls of the classroom, the location of the Sun’s path across the sky for each of the seasons, and ask the participants to predict how high the Sun rises in the sky and where it will set.
The reasons for seasons. This slide illustrates summer in the northern hemisphere. Note that (1) the period of daytime (dawn to dusk) is more than 12 hours in the northern hemisphere, because more than half the northern hemisphere is in sunlight at any give time; however, the period from dawn to dusk is less than 12 hours in the southern hemisphere. Also, (2) the solar radiation is more direct, concentrated, intense in the northern hemisphere. And, (3) the sun is higher in the sky. DEMO [1/3] Flashlight at an angle and the intensity or concentration of light