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Environmental Physics:Climate Dynamics aspects
Arnaud Czaja
Space & Atmospheric Physics
Overview (Lectures #7-14)
• Greenhouse effect (#7, i.e. today)• Water Vapour feedback (#8)• Cooling mechanisms for the planet (#9)• Climate models (#10) + MATLAB session• Climate timescales (#11)• Climate sensitivity (#12)• Modes of climate variability (#13)• Discussion of a hot Topic (#14)
Our own EP Climate Model!
Atmosphere
Tropics
ExtraTropicsOcean
OH 2AT
1ST 2ST
1OT 2OT
AH
OH
Our own EP Climate Model!
Atmosphere
Tropics
ExtraTropicsOcean
OH 2AT
1ST 2ST
1OT 2OT
AH
OH
(i) Use of model is not mandatory and thus themodel is not examinable
(ii) MATLAB session on Thursday Feb 7 (5-6pm)(come if you wish, this is not mandatory)
Lecture 7The Greenhouse effect
Lecture 7The Greenhouse effect
Student: Oh yeah! It’s the trapping of radiation by the
atmosphere
Lecture 7The Greenhouse effect
Lecturer: Let’s be a bit more precise!!
7.1 Motivation:Observations of Earth from
Space
Total radiation seen by a satellite
(GERB project in Space & Atmospheric Physics)
NB: Photon energy is the main form of energyexchangedbetween theearth and space
LW SW
Long wavelength photons (emitted
by the Earth)
Short wavelength photons (reflected
from the Sun)
+
Terrestrial radiation λ≈10-20μm
1 erg s-1 cm-2 = 10-3 W m-2
Sun radiation Solar radiation λ≈0.2-1μm
To zero order…
• Solar photons are absorbed by the atmosphere (clouds, water vapour, ozone)
• …but much less so than are the terrestrial photons.
• This is because of the atmospheric composition, with tri-atomic molecules efficient at interacting with λ≈10-20μm photons (“greenhouse absorbers”).
Atmospheric composition (fraction of total molecules)
Main Greenhouse gas (GHG) is Water vapour (variable ≈1%)
Man influenced GHG
Pre-industrial IPCC (2007)
CO2 280ppmv 380 ppmv
CH4 700ppbv 1800 ppbv
N2O 270ppbv 320 ppbv
NB: 1ppmv = 1 molecule out of a million 1ppbv = 1 molecule out of a billion
N2
O2
CO2
What is meant by variable H2O…
sate
eRH
Upper tropospheric RH on April 27, 1999Low level enthalpy
qLTCh vp
0 1002.5
3.5
7.3 Observations of the greenhouse effect (G)
I
Observed Greenhouse effect24
WminITG clears
Water vapour content2
2
kgminM OH
Sea surface temperature
KinSST
180
50
50
10
303
273
NB: All are annual mean data (from Held & Soden, 2000)
Imperial College London
28 May 200320
Solar spectr
um
Lean (1991)
[adapted by Lockwood]