Earth Processes Part 4: Coriolis Effect, Tides, and Seasons.
Flows around high and low pressure zones (winds) Earth not spinning No Coriolis Effect Earth...
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Transcript of Flows around high and low pressure zones (winds) Earth not spinning No Coriolis Effect Earth...
Flows around high and low pressure zones (winds)
Earth not spinningNo Coriolis Effect
Earth spinningCoriolis Effect
Hi
Hi Lo
Clockwise Counter-clockwise
DownwellingSubsidence
UpwellingLifting
Northern HemisphereMotion
Vertical Motion
Convergence DivergenceHi Altitude Motion
Lo
Santa Ana WindsHi (Cold)
Low (Warm)
WHY ARE SANTA ANAS
HOT?
Adiabatic heatingas the air pressureincreases
Why are Highs and Lows associated with Good and Bad
Weather, Respectively?
LO
Divergence
Convergence
Upw
elling
HI
Convergence
Divergence
Dow
nwelling
AdiabaticheatingRH
Adiabaticcooling
RH Clear Skies Clouds andPrecipitation
WeatherWhere there’s weather, there’s
clouds (or not)
This is why we watchbarometers
This is whatmakes T-storms
This is whyE Hawaii is wet
This is whywe getsquall linesand cyclones
Rain-Shadow Deserts
Orographic precipitation
Cold Front
Figure 8.11
Warm Front
Figure 8.13
Midlatitude Cyclone
Figure 8.14
Earth’s Climate SystemIt’s all about energy
Figure 10.1
Albedo and the Greenhouse Effect
max=2898/T6000 K: 0.5 m283 K: 10 m
Earth’s Albedo: 30%Major Controls?
Greenhouse Gases:H2OCO2
N2OCH4
Others
Climate and the CryosphereAlbedo-Climate FeedbacksThe Snowball Earth? (600-700 Ma)How would Earth get out of a Snowball Scenario?
Climate and the Cryosphere
Figure 10.32
Climate and the Cryosphere
What is the impact of changes in insolation?
• How much of a difference does 30 W/m2 make?
• -18.99°C to -17.59°C
• A range of 1.4°C
CO2 and the Earth System
CO2 and the Earth System
What effect does the collision between India and Asia have on
atmospheric CO2?
The Ocean, Heat and CO2Mass of Atmosphere: 5.1 x 1018 kgMass of Ocean: 1.4 x 1021 kg
To raise entire atmosphere 1 °C:
~ 5 x 1021 J or 1.2 x 1021 cal
To raise entire ocean 1 °C:
~ 6 x 1024 J or 1.4 x 1024 cal
CO2(g)
CO2(aq) +H2O -> H+(aq)+ HCO3(aq)
Global Temperatures
Figure 10.28
The Keeling Curve
Variations in CO2
Causes of Climate Change
From: Mann, Michael E., Raymond S. Bradley, and Malcolm K. Hughes. 1998. Nature , 392, pp.779-
787
Climate Relationships
Figure 10.3
Generalized Climate Regions
Figure 10.4
Latitudinal Transect
MoscowSouthCarolina
Amazonia SubarcticRussia
Continentalvs.
Maritime
Mediterranean Climates
Figure 10.16