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Integrative Studies 410 Our Place in the Universe
Integrative Studies 410 Our Place in the Universe

... • All an illusion! There are no canals… ...
Projects in Atmospheric and Environmental Physics - Innsida
Projects in Atmospheric and Environmental Physics - Innsida

... sense the composition and temperature of the atmosphere where it is produced. Atmospheric waves passing through this shell modulate the temperature, and these changes may be used to quantify the wave energy in the middle atmosphere. Global small-scale wave variance. By using a global network of grou ...
Mercury Mercury is a dead planet and the
Mercury Mercury is a dead planet and the

... giant  is  larger  than  Earth.  Unlike  any  other  plant  in  our  solar  system,  Uranus  has  a  98-­‐ degree  tilt  to  its  axis.    Scientist  think  that  early  in  its  history  the  planet  was  hit  by   something  rea ...
13.14 The Eight Planets
13.14 The Eight Planets

... atmosphere on this planet is perfect for beings to have changed. Earth’s atmosphere is mainly made up of nitrogen, oxygen, and water vapour. There is a small amount of ozone in our atmosphere and this is what filters some of the damaging radiation from the Sun. **Find current info. on the state of t ...
1. Draw a pie chart to show the gases that make up our atmosphere
1. Draw a pie chart to show the gases that make up our atmosphere

... 8. What are the 2 main reasons for global winds? (Hint: Think about pressure and rotation of Earth) 1. differences in air pressure caused by difference in temperature. Warm air has low density and rises, creating regions of low pressure. Cold air has higher density and sinks, creating regions of hig ...
Solar System Fundamentals
Solar System Fundamentals

... • If the average velocity of a molecule is close to the escape velocity of the planet or satellite, then over time it will escape into space. • The effect of this is that hot, light planets or satellites will lose all lighter molecules that they might have had. – Mercury, Moon and all satellites ex ...
DTT Diagnosis test Edexcel Core Therapy Topic 3
DTT Diagnosis test Edexcel Core Therapy Topic 3

... Formation of rocks ...
Document
Document

... • A small solar system body that orbits the Sun. • Comets are made of ice, dust and small rocky particles. • When close enough to the Sun they display a visible coma (a fuzzy outline or atmosphere due to solar radiation) and sometimes a tail. ...
Planet Assignment
Planet Assignment

... You are going to be paired with 2 other students in the class to complete this assignment. One of the following will be assigned to you and your group: SUN EARTH URANUS PLUTO SATURN ...
3/3 What Are Planets?
3/3 What Are Planets?

... • Largest object in solar system (makes up 99.8% of mass of solar system!) • About 5 billion years old (half way there!) • Average surface temperature of 6,000°C • “Only” 93 million miles away! “Goldilocks Zone” • Can hold about a million Earth’s inside! • More than 400 Earth’s could fit across the ...
The Nine Planets
The Nine Planets

... Mercury is the closest planet to the Sun; therefore, it gets sunlight that is 10 times brighter than the Earth’s. Mercury does not have an atmosphere to help trap the heat it receives from the Sun, so it loses all of its heat at night dropping to -180 degrees Celsius (oC). Mercury’s daytime temperat ...
Air
Air

... heat energy is reflected back into space by the Earth’s surface, gases in the atmosphere, and clouds; some of it is absorbed and stored as heat. When the surface and atmosphere warm, they emit heat, or thermal energy, into space. The “radiation budget” is an accounting of these energy flows. If the ...
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File

... from Monday to demonstrate ability to interpret information from multiple sources. ...
weather and climate
weather and climate

... these areas more warmth. However, the polar regions are at such an angle to the Sun that they get little or no sunlight during the winter, causing colder temperatures. These differences in temperature create a restless movement of air and water in great swirling currents to distribute heat energy fr ...
Earth Systems and Atmosphere
Earth Systems and Atmosphere

... As carbon moves between the spheres, it affects or is affected by climate change. ...
The Atmosphere PowerPoint
The Atmosphere PowerPoint

... • The thin envelope of air that surrounds our planet is a mixture of gases, each with its own physical properties. The mixture is far from evenly divided. Two elements, nitrogen and oxygen, make up 99% of the volume of air. The other 1% is composed of "trace" gases, the most prevalent of which is th ...
Chapter 13 Section 3
Chapter 13 Section 3

... Rising CO2 Levels • After only a few years of measuring CO2 levels, it was obvious they were changing in other ways than just seasonal fluctuations • CO2 levels have increased by over 20% in less than 50 years • Due largely to CO2 released into air when fossil fuels burned ...
SNC2P (3.3) Natural Climate Change
SNC2P (3.3) Natural Climate Change

... • Mountain ranges that affect the path of moisture-carrying winds are created when continent-carrying crustal plates collide. This affects precipitation, which affects climate • Moving continents lead to increases or decreases in volcanic activity as crustal plates move together or apart. Volcanic a ...
Chapter 3: Introduction to the Atmosphere
Chapter 3: Introduction to the Atmosphere

... g. air temperature reaches minimum at top of the mesosphere; ~ 50 miles h. thermosphere: 1) air temperature increases with increasing altitude 2) heat source: splitting and heating of atoms and molecules that absorb ultraviolet radiation i. essentially all weather phenomena occur in the troposphere ...
Chapter 3: Introduction to the Atmosphere
Chapter 3: Introduction to the Atmosphere

... g. air temperature reaches minimum at top of the mesosphere; ~ 50 miles h. thermosphere: 1) air temperature increases with increasing altitude 2) heat source: splitting and heating of atoms and molecules that absorb ultraviolet radiation i. essentially all weather phenomena occur in the troposphere ...
Air pressure - SharpSchool
Air pressure - SharpSchool

... stratosphere. It is between 18km to 50km. • The layer above the stratosphere is the Mesosphere. It is between 50km to 80km. • The layer above the Mesosphere is the thermosphere. It is above 80 km high. ...
Earth`s Atmosphere and Temperature
Earth`s Atmosphere and Temperature

... contains broad, fast-flowing "rivers" of air circulating around the world. These are called jet streams. The jet streams can change weather patterns in the troposphere. Above the ozone layer of the stratosphere, temperature begins to drop once more. This is the beginning of the mesosphere. Temperatu ...
Our Solar System The Sun
Our Solar System The Sun

... • Made of elements [H] and [He] with a hot, solid core of [Fe] -almost a star! • “Red Spot” is a massive storm • 62 Moons: the four largest are named Io, Europa, Ganymede, Callisto, but there are more… ...
The Atmosphere Notes
The Atmosphere Notes

... together the amount that is backscattered to space, the amount reflected from clouds, and the amount reflected by the land-sea surface)  How much of the Sun’s energy is absorbed by Earth’s atmosphere and clouds?  How much of the Sun’s energy is absorbed by the land and sea?  Heating of the Atmosp ...
Inner and Outer Planets
Inner and Outer Planets

... meteors, interplanetary gas, dust, and all the “space” in between them. • The eight planets (and Pluto) of the Solar System are named for Greek and Roman Gods and Goddesses. ...
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Extraterrestrial atmosphere

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