Lecture 31 - Climate of the Earth

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ASTR 1210 (Exam 3)

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What Factors Can Cause Long-term Climate Change?

  • Energy in = energy out 

  • When those two things find equilibrium on a planet, that leads to getting the temp of a planet

  • Sun creates all the energy in the solar system = affects equilibrium temp 

  • Can take a planet and push it closer to the sun = equilibrium temp goes up because energy goes up and vice versa 

  • Can make my star hotter = increase energy even if planet is same distance

    • What is happening to the Sun 

  • Stars get hotter and hotter as years go on 

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Solar Brightening

  • Rate at which sun is fusing at = as it runs out of hydrogen, it has to fuse hydrogen faster

  • Sun very gradually grows brighter with time, increasing the amount of sunlight warming the planets

  • In Goldilocks Zone to allow liquid water exist on the Earth 

  • Mars will be pushed into the Goldilocks Zone

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Temperature vs Solar Activity

  • Sunlight is decreasing and relatively stable

  • Sun is getting colder, Earth is getting hotter

  • Has to do with the gases around the planet’s atmosphere

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Changes in Axis Tilt

  • Earth’s climate is affected by seasonal temperature changes

  • Has to do with the axial tilt of the Earth - tilt more extreme = seasons more extreme

  • Over many years, about 22 to 25 degrees - our tilt is stable because of the Moon

  • Moon acts as a gravitational sounding board that allows the tilt to stay the same

  • Mars has had more extreme tilts = more extreme climate change because it doesn’t have a big moon

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Changes in Reflectivity

  • If planet more reflective - energy in going down

  • Less reflective - energy in is gonna increase

  • Can change energy of the planet

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Changes in Greenhouse Gases

  • Cause the potential for significant temp change

  • Greenhouse gases are also vital for the Earth’s life to thrive

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Evolution of the Earth’s Atmosphere 

  • When Earth first formed, it was situated in gas and dust that was the solar nebula 

    • Hydrogen and helium made up Earth’s early atmosphere

  • Earth eventually lost the H and He over time - has to do with Earth’s gravity - can’t hold on to H and He

    • If planet was bigger, it could retain H and He - gas giants retained it

  • Ammonia and methane went away and atmosphere dominated by nitrogen, carbon dioxide, and water

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Sources of Gas

  1. Impacts — impacts vaporize rock 

  2. Outgassing — volcanos can significantly change the amount of gas in our atmosphere 

  3. Vaporization — ice or liquid vaporizes 

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Losses of Gas

  1. Reversible loss

    1. Condensation

    2. Chemical reactions with the surface

      1. Rust removes oxygen from the atmosphere

  2. Permanent loss — losing gas to space

    1. Thermal escape due to planet’s temperature

    2. Escape via the Solar World - particles from Sun smack into planet’s atmosphere and the energy can cause particles to escape the planet’s atmosphere

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Thermal Escape from an Atmosphere 

  • Average speed or thermal velocity of particles move at tells you the temperature 

  • Some of those particles travel faster/ some will travel slower

  • Some will be traveling GREATER than escape velocity - velocity of an object so that it escapes a planet 

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Thermal Velocity Equation

  • Particles that have less mass will be moving much faster than the other particle to reach escape velocity

<ul><li><p>Particles that have less mass will be moving much faster than the other particle to reach escape velocity</p></li></ul><p></p>
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Escape Velocity from Solar System Planets

  • Low-mass particles will move fastest at any given speed

  • Further from sun - colder you’re going to be 

  • Gravity affects escape velocity

<ul><li><p>Low-mass particles will move fastest at any given speed</p></li><li><p>Further from sun - colder you’re going to be&nbsp;</p></li><li><p>Gravity affects escape velocity </p></li></ul><p></p>
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Exospheres of the Moon and Mercury

  • Very, very thin atmosphere

  • Dominated by things smacking into these objects, vaporizing them…

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What is Mars like Today?

  • Thin atmosphere but it has some stuff

  • Impacts of weather on Mars - seasonally has dust storms

  • Dust in the Martian atmosphere that’s been blown around as a result of windstorms that has blurred features

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Seasonal Ice Caps of Mars

  • Polar ice cap biggest during winter, smallest during summer - made up of carbon dioxide (dry ice)

  • Going to increase/decrease CO2 seasonally on Mars

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How Has Mars’s Climate Differed in the Past? 

  • Likely had water on the surface 

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Changing Axis Tilt

  • layers of ice and rock that Mars goes through freezing and non-freezing periods - these layers were explained by axial tilt from Mars (0 to 60 degrees)

  • Could’ve cause Mars to lose atmosphere

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Why the Climate Change?

  • Loss of atmospheric gas

  • Loss of water

  • Size is a critical factor in the timescale for climate change on a planet

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Climate Change on Mars 

  • Magnetic field may have perserved early Martian atmosphere

  • Solar winds stripped atmosphere after field decreased because of interior cooling 

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What is Venus like today?