1126_worldclimatechange
-
Upload
dipanjan-das -
Category
Documents
-
view
215 -
download
0
Transcript of 1126_worldclimatechange
-
7/27/2019 1126_worldclimatechange
1/18
Media Myths about ClimateBe skeptical be very skeptical !
Concern about global warming is based on recenttemperature trends
9 of the 10 hottest years on record
If somebody could find some other cause for recentwarming, we could quit worrying
Global warming is a theory based on complicatedcomputer models
CO2is air pollution cutting emissions will leadto falling CO2 and therefore cooling
If we stop burning coal, well freeze in the dark!
-
7/27/2019 1126_worldclimatechange
2/18
Global Warming isBased on Common Sense
not computer models not recent temperatures
not complicated!
-
7/27/2019 1126_worldclimatechange
3/18
Planetary Energy Balance
Energy In = Energy Out
2 2 4(1 ) 4S R R T
o18 CT
But the observed Ts is about 15 C
-
7/27/2019 1126_worldclimatechange
4/18
Dancing Molecules and Heat Rays!
Nearly all of the air is
made of oxygen (O2)and nitrogen (N2) inwhich two atoms ofthe same elementshare electrons
Infrared (heat)
energy radiated upfrom the surface canbe absorbed by thesemolecules, but not
very well
N N
O O
Diatomic molecules can
vibrate back and forthl ike balls on a spring, but
the ends are identical
-
7/27/2019 1126_worldclimatechange
5/18
Dancing Molecules and Heat Rays!
Carbon dioxide (CO2)
and water vapor (H2O)are different!
They have many moreways to vibrate androtate, so they arevery good at absorbingand emitting infrared(heat) radiation
Molecules that have manyways to wiggle are called
Greenhouse molecules
O OC
H H
O
Absorption spectrum of CO2 was measured by John Tyndall in 1863
-
7/27/2019 1126_worldclimatechange
6/18
Common Sense
Doubling CO2 wouldadd 4 watts toevery square meterof the surface of
the Earth, 24/7 Doing that would
make the surfacewarmer
This was knownbefore light bulbswere invented!
4 Watts
John Tyndall , January 1863
-
7/27/2019 1126_worldclimatechange
7/18
Common Misconception #1Expectations of future warming are based on
extrapolation of recent warming trends
WRONG! They are based on the idea that whenwe add energy to the surface, it will warm up
-
7/27/2019 1126_worldclimatechange
8/18
19th Century Climate Physics(Svante Arrhenius, 1897)
S0(1 )r2
TS4 (4r2 )
S0(1 ) 4TS4
0 4TS
4 4(4TS
4 )
Differentiate, apply chain rule
TS
TS
4
Ar rhenius worked out a simple formula
for the change in sur face temperature
given a change in effective
atmospher ic emissivity due to CO2
Earth
Ts
aS0
esTs4
S0
-
7/27/2019 1126_worldclimatechange
9/18
19th Century ClimatePhysics(contd)
Plug in measured values
TS TS
4
TS
4 240 W m-2
(from satellite data)
()(
TS
4
) 4 W m-2
(for 2 x CO2
from radiative transfer)
4
240
Ts = 288 K
TS
288K
4
4
240
1.2K
For CO2 alone (no feedback), expect about 2F warming for 2 x CO2
-
7/27/2019 1126_worldclimatechange
10/18
Climate Feedback Processes
Positive Feedbacks(amplify changes) Water vapor
Ice-albedo
High clouds
De DTS Dvapor
D albedo
DLW
D hi cloud
D lo cloud
Negative feedbacks
(damp changes) Longwave cooling Low clouds
-
7/27/2019 1126_worldclimatechange
11/18
Tiny Bubbles Priceless
ice age ice age ice ageice age
-
7/27/2019 1126_worldclimatechange
12/18
Estimating Total Climate Sensitivity
At the Last Glacial Maximum
(~ 18k years ago) surface temp ~ 6C colder CO2 was ~ 180 ppm
(weaker greenhouse, 4.1 W m-2 more LW)
Brighter surface due to snow and ice, estimate3.4 W m-2 more reflected solar
Or, for doubling of CO2: expect 4 x 0.8 = 3.2C of
T
S
FTS(now)T
S(then)
F(now
) F
(then
)
6K
(4.1 3.4)Wm2 0.8
K
Wm2
-
7/27/2019 1126_worldclimatechange
13/18
Review: 19th Century Physics(updated using paleo-data)
Forcing: changes in properties ofatmosphere as measured by spectroscopy(4 W m-2 per doubling of CO2)
Feedback: both positive and negative, totalresponse to forcing estimated from Ice Ageclimate data (about 0.8C per W m-2)
Response: about 3.2 C warming for 2 xCO2No climate models required just based on observations
(modern calculations agree coincidence?)
-
7/27/2019 1126_worldclimatechange
14/18
CO2 and the Modern Age
370 ppm in 2000
Vostok (400k yr) Ice Core data (Petit et al, 1999)
180
230
280
330
380
-400000 -300000 -200000 -100000 0
year
Over the past 420,000
years atmospheric CO2has varied between 180and 280 parts permillion, beating in timewith the last four glacialcycles
Since the IndustrialRevolution, CO2 has risen
very rapidly ice iceiceice
CO2
388 ppm in 2009
f rom measurements
-
7/27/2019 1126_worldclimatechange
15/18
CO2 and the Future
Vostok (400k yr) Ice Core data (Petit et al, 1999)
0
200
400
600
800
1000
-400000 -300000 -200000 -100000 0
year
Over the past 420,000
years atmospheric CO2has varied between 180and 280 parts permillion, beating in timewith the last four glacial
cycles
Since the IndustrialRevolution, CO2 has risenvery rapidly
If China & India developusing 19th Centurytechnology, CO2 willreach 900 ppm in this
century
ice iceiceice
CO2
900 ppm in 2100
388 ppm in 2009
You aint seen nothing yet!
-
7/27/2019 1126_worldclimatechange
16/18
Climate vs. Weather
Weather tells you what to wear today climate tells you what clothes to buy!
Climate is an envelope of possibilitieswithin which the weather bounces around
Weather depends very sensitively on theevolution of the system from one momentto the next (initial conditions)
Climate is determined by the properties ofthe Earth system itself(the boundary conditions)
-
7/27/2019 1126_worldclimatechange
17/18
Climate Predictability
Predicting the response of the climate to achange in the radiative forcing is notanalogousto weather prediction
If the change in forcing is large and predictable,
the response can also be predictable I cant predict the weather in Fort Collins on
December 18, 2009 (nobody can!)
I can predict with 100% confidence that theaverage temperature in Fort Collins forDecember, 2009 will be warmer than the averagefor July!
-
7/27/2019 1126_worldclimatechange
18/18
Climate Forcing
Changes in climate often reflect changes in forcing, asamplified or damped by climate feedbacks Diurnal cycle
Seasonal cycle
Ice ages
Response to volcanic aerosol
Solar variability
Greenhouse forcing
If forcing is sufficiently strong, and the forcing itself is
predictable, then the response of the climate can bepredictable too!