lecture15 - geowiki.ucsd.edu · 3) earth’s tilted axis orbits sun! sun in zenith at different...
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SIO15-19: Lecture15: The Atmosphere and Climate
SIO15-19: Lecture15: The Atmosphere and Climate
11/4/19
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SIO15-19: Lecture15: The Atmosphere and Climate
climate: average long-term condition; controlled by location regional to globalweather: short-term condition; controlled by atmospheric anomalies local to regional
climate: “I live in San Diego because it rains in Seattle”
weather: “San Diego got soaked last week”
SIO15-19: Lecture15: The Atmosphere and Climate
how much solar radiation is received in any area?
insolation per area:greater when Sun is overhead than near poles
Marshak: Earth, Portrait of a Planet
zenith
seasonswatchshortVideo15a
annually 2.4 times lowerat poles than at equator
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SIO15-19: Lecture15: The Atmosphere and Climate
how much solar radiation is retained in any area?
Albedo: fraction of insolation reflected back to space
- 80% fresh snow- 25% grass- 10% oceans
THE DUAL FUNCTION OF H2O
WATER VAPOR: most abundant greenhouse gas (warms)
CLOUDS: reflect sunlight back into space (cools)
Marshak: Earth, Portrait of a Planet
seasonswatchshortVideo15a
SIO15-19: Lecture15: The Atmosphere and Climate
- 30% reflected back to space- 51% absorbed at surface- 19% absorbed by atmosphere
Earth’s surface emits more heat (IR) than it receives
Ahrens: Meteorology Today
see Fig 11.4
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SIO15-19: Lecture15: The Atmosphere and Climate
+ 1% other stuff- 0.93% Ar- CO2 400ppm (0.04%)- Ne 18ppm- He 5ppm- CH4 2ppm- Kr 1ppm
mainly N2 and O2+ 0-4% water vapor (H2O) (variable)
Greenhouse Gases: H2O, CO2, CH4
watchshortVideo15b
SIO15-19: Lecture15: The Atmosphere and Climate
Which element is the main contributor to Earth’s atmosphere?
(0.33 pt)
Write your own pop quiz only. Have your student ID ready.Submitting a pop quiz for your friend is cheating!
We check handwriting.Suspected cheaters will lose ALL previous PQ credits!Students in class less than 20 min are NOT eligible to get PQ credit.
11/4/19
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SIO15-19: Lecture15: The Atmosphere and Climate
Earth’s atmosphere acts like a greenhouse
greenhouse gases: H2O, CO2, CH4- transparent to visible, UV light- absorb infrared- reflect IR back to Earth- > trap heat
Earth with greenhouse:16ºC/61ºFEarth without greenhouse: 34ºC/61ºF colder -> -18ºC/0ºF
Fig 11.8
H2O most abundant greenhouse gas
SIO15-19: Lecture15: The Atmosphere and Climate
What is Earth’s most abundant greenhouse gas?(0.34 pt)
Write your own pop quiz only. Have your student ID ready.Submitting a pop quiz for your friend is cheating!
We check handwriting.Suspected cheaters will lose ALL previous PQ credits!Students in class less than 20 min are NOT eligible to get PQ credit.
11/4/19
6
SIO15-19: Lecture15: The Atmosphere and Climate
3) Earth’s tilted axis orbits Sun! sun in zenith at different times (+/- 23.5º N/S)! local insolation changes throughout the year
Marshak: Earth, Portrait of a Planet
Fig 11.15
summer in San Diegobut winter in Santiago, Chile
seasonswatchshortVideo15a
SIO15-19: Lecture15: The Atmosphere and ClimateMarshak: Earth, Portrait of a Planet
oppositeseasonsbetweenNandShemispheres
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SIO15-19: Lecture15: The Atmosphere and Climate
Abbott: Natural Disasters
Marshak: Earth, Portrait of a Planet
SIO15-19: Lecture15: The Atmosphere and Climate
polar ice, subpolar Tundra, subtropical (temperate), dry land (desert), tropicalplus: highland, continental
Marshak: Earth, Portrait of a Planet
see Fig 11.7
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SIO15-19: Lecture15: The Atmosphere and Climate
Which season is it in Santiago, Chilewhen it is winter in San Diego? (0.33 pt)
Write your own pop quiz only. Have your student ID ready.Submitting a pop quiz for your friend is cheating!
We check handwriting.Suspected cheaters will lose ALL previous PQ credits!Students in class less than 20 min are NOT eligible to get PQ credit.
SIO15-19: Lecture15: The Atmosphere and Climate
• oceans store more heat than atmosphere • oceans are climate moderators (negative feedback) ! coastal areas have less extreme climate
Heat Capacity: ability to absorb heat without getting hot
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SIO15-19: Lecture15: The Atmosphere and Climate
- ocean processes longer-term than atmospheric processes- > ocean currents slower than atmospheric winds- currents blocked by continents- Driving Mechanism: cold and salty water sinks (thermohaline circulation)
source: Wikipedia
exact shape of heat conveyor not well known
SIO15-19: Lecture15: The Atmosphere and Climate
Ocean Surface Currents
Marshak: Earth, Portrait of a Planet
- warm western boundary currents (e.g. Gulf Stream)- cold eastern boundary currents (e.g. California Current) (think May Grey/June Gloom!)
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SIO15-19: Lecture15: The Atmosphere and Climate
! atmosphere has less CO2 than humans produced in last 150 yrs! oceans take up CO2! it’s not (only) the rain forest!! leads to ocean acidification
but what we do know!
SIO15-19: Lecture15: The Atmosphere and Climate
50% air below 5.6 km 90% air below 16 km 99.99997% below 100km
• air pressure: push due to weight of atmosphere above• greatest at sea level: 1 atmosphere, 14.7 PSI, 1035 mbar (g/cm2)• pressure and density decrease exponentially with altitude
simple
watchshortVideo15b
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SIO15-19: Lecture15: The Atmosphere and Climate
troposphere: lower 10km; weather layer, mixingstratosphere: next 35km; very dry, no vertical mixing, O3 layermesosphere: less O3; meteorites burn upthermosphere: < 1% air; (ISS at ~350 km)
Layers follow T-function
SIO15-19: Lecture15: The Atmosphere and Climate
it takes 600 cal to evaporate 1g waterevaporation: water vapor absorbs heat
condensation: water vapor releases heat
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SIO15-19: Lecture15: The Atmosphere and Climate
SIO15-19: Lecture15: The Atmosphere and Climateverysimilartopast2weeks
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SIO15-19: Lecture15: The Atmosphere and Climate
SIO15-19: Lecture15: The Atmosphere and Climate