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Faint Young Sun Paradox Part I
Faint Young Sun Paradox Part I

...  Methane and ammonia are even better GHG than carbon ...
Document
Document

...  Methane and ammonia are even better GHG than carbon ...
Unit 3: The Solar System Historical Models of the Solar System
Unit 3: The Solar System Historical Models of the Solar System

... Ptolemy (100-170 CE) - His geocentric model was used for 1400 years. - All orbits of all bodies in space traveled in a perfect circle at a constant speed - “Wheels on wheels” model – planets move in small circles that moved in larger circles ...
Lunar Data Comparison 3 – Sidereal vs
Lunar Data Comparison 3 – Sidereal vs

... Interestingly, by just including sidereal data one can come up with a 360-degree motion of the Earth around the Sun (the point of delta 1.00000) in a sidereal year but this orbit of the Earth around the Sun is longer, in time and distance (about 22,000 miles), than the 360 degree tropical model of t ...
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... • Many, many moons ...
3rd Grade Science Curriculum Map Standards – Quarter 1
3rd Grade Science Curriculum Map Standards – Quarter 1

... a cooler one by contact or at a distance and the cooler object gets warmer. 3.P.3.1 Students know that rubbing objects together results in friction which releases heat energy. 3.P.3.2 Students know that objects can transfer energy by touching or by giving off or receiving energy waves. Heat can move ...
Early Astronomy
Early Astronomy

... points of light on the sky, like the stars, but unlike the Sun and Moon. These objects received special attention because they:  moved against the background of stars,  are always located within several degrees of the ecliptic,  periodically undergo retrograde motion with respect to the backgroun ...
Study Guide for Astronomy
Study Guide for Astronomy

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Chapter 10
Chapter 10

... of Ptolemy, they were used to help locate and predict the positions of the Sun, Moon and stars  Using a compass and an astrolabe, they were able to describe the position of any celestial body in relation to the direction North as well as in relation to the horizon. ...
Conditions for Life
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... Part III The temperature on Earth does not go from one extreme to the other. There are areas of extreme cold and heat, but overall, the Earth’s climate is stable. This is due to Earth’s distance from the Sun as it orbits around it and its axial tilt during rotation. Look at a globe of Earth. Notice ...
Science The Earth Powerpoint_GB
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...  The light from the Sun can only shine on the whole surface for one night in each cycle: a full moon.  On one night, no light from the Sun can reach the moon at all: a new moon. ...
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PHYS 390 Lecture 9 - Planetary atmospheres 9
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... Jupiter, Saturn, Uranus, and Neptune are called Jovian planets since the outer planets have characteristics similar to those of Jupiter. Pluto is an exception since it does not resemble either the Earth or Jupiter. If the solar system is viewed from a position far above the Earth's North Pole, the ...
Satellite Communication - univ
Satellite Communication - univ

... slot only. • More than one time slot can be assigned to stations with more bandwidth requirements. • Requires time synchronization between the Earth Stations. ...
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PS 224: Astronomy Fall 2014 Midterm (October 16, 2014)
PS 224: Astronomy Fall 2014 Midterm (October 16, 2014)

... False. Energy can neither be created nor destroyed but only converted from one form or another. h. Images taken in X-ray are always displayed in false color. True. We cannot see X-ray photons with our eye. They have to be rendered in one of the visible colors for us to be able to see them. i. The mo ...
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Minor Members of the Solar System

... 23.4 Minor Members of the Solar System Asteroids: Microplanets  An asteroid is a small, rocky body whose diameter can range from a few hundred kilometers to less than a kilometer.  Most asteroids lie between the orbits of Mars and Jupiter. They have orbital periods of three to six years. ...
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... c. Do you think it would still be possible to have life on Earth? No, at least not life as we know it. With rare exceptions, life on Earth is not capable of surviving at extreme climates, and a sun with double the temperature and 16 times the power would certainly produce extreme climates. At those ...
DOCX
DOCX

... and the ice wall. There is no south pole. The sun and moon are the same size, each about 32 miles in diameter, and less than 3,000 miles above the earth. The sun is not a star and the 'planets' are not physical (rocky or gaseous) bodies but wandering stars. We have night and day because sunlight is ...
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... diameter shield volcano that was formed billions of years ago. Scientists have found a lot of recent evidence of volcanic lava which suggests Olympus Mons may still be active. It is the second highest mountain in the entire solar system, topped only by the Rheasilvia central peak on the asteroid Ves ...
Henry6SCI (H6SCIASTRO)
Henry6SCI (H6SCIASTRO)

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94263_Solar_Sys_Halfs
94263_Solar_Sys_Halfs

... 1. Examine the data above, your measures (in cm), the Actual distances in AU to the planets, and Bode’s Law predictions. How close are Bode’s Law predictions and your measurements to the ACTUAL AU distance? 2. Pluto is not a planet, but Bode’s Law predicted the farthest planet to be at 78 AU (Pluto’ ...
Exam Name___________________________________
Exam Name___________________________________

... from space, why then are there so few equivalent craters from such impacts on the Earth? A) Because geological processes and erosion by water and wind have destroyed most of the craters that have formed on Earth. B) Because the gravitational field of the Moon attracted incoming objects and this shie ...
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Comparative planetary science

Comparative planetary science or comparative planetology is a branch of space science and planetary science in which different natural processes and systems are studied by their effects and phenomena on and between multiple bodies. The planetary processes in question include geology, hydrology, atmospheric physics, and interactions such as impact cratering, space weathering, and magnetospheric physics in the solar wind, and possibly biology, via astrobiology.Comparison of multiple bodies assists the researcher, if for no other reason than the Earth is far more accessible than any other body. Those distant bodies may then be evaluated in the context of processes already characterized on Earth. Conversely, other bodies (including extrasolar ones) may provide additional examples, edge cases, and counterexamples to earthbound processes; without a greater context, studying these phenomena in relation to Earth alone may result in low sample sizes and observational biases.
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