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This Week: Future Climate
Future CO2 Forcing
Climate Sensitivity – Feedbacks
Natural Short and Long-term Forcings
Global Warming Impacts
Announcements
• See handout and website for details regarding paper and poster content
• Poster Sessions: March 12 and 13 in Mary Gates Commons 10:30 – 11:20
• Monday March 17 8:30 AM, Final Exam, JHN 075 (here)
• Papers and descriptions of 3 other posters due Wednesday March 19
Kaya Identity Model
kaya identity model
Future Atmospheric CO2
One emission scenario
Range of predictions suggest double pre-industrial by mid-century
Figure 10.20
Stabilization Scenarios
2000 23002100 2200
What our emissions can be for different constant CO2 levels.
What do these tell us about future biosphere and ocean sinks?
Committed to Warming: Time Response
Figure 10.4
A Long View of Fossil Fuel Perturbation
Figure 7.12
Climate Sensitivity-All about Feedbacks
T = F
is climate sensitivity parameter
units: K “per” W/m2
determined by feedbacks!
Estimates of Climate Sensitivity
Box 10.2, Figure 1
T change for a 4 W/m2 forcing (i.e. “double CO2”)
Most probable ~ 0.75 K/(W/m2)
Announcements
• Get a handout on paper/poster guidelines
• Brian’s office hours today canceled, moved to Thursday 5-6pm
• My office hours are today, 3:30 – 4:30pm in 506 ATG
Feedbacks
Initial ForcingState Variable
Process or coupling
+/-
+/-
+ increases state variable- decreases state variable
“feedback loop”
Ice-Albedo Feedback
Initial Forcing(e.g. GHG)
Temperature
Ice melts, dark soils exposed
Example of a positive feedback
+ Albedo -
+
More solar radiation absorbed
Water Vapor-Temperature Feedback
Initial Forcing(e.g. GHG, solar radiation)
Temperature+
Water Vapor +
+
More evaporation, saturation vapor pressure increase
Increased Greenhouse effect
Atmosphere—Protector of the Oceans?
water trap
If H2O reaches top of atmosphere it is blown apart by UV radiation
H atoms escape to space, never to return
Probable cause for no H2O on Venus
IR Flux-Temperature Feedback
Initial Forcing(e.g. GHG)
Temperature
Example of a negative feedback
+ Outgoing IR flux increases+
-
Phytoplankton-DMS-Marine Cloud Feedback
Initial Forcing(decreased clouds)
Solar Radiation(Temperature)
+ Biogenic Sulfur Emissions
+
-
Charlson, Lovelock, Andreae, Warren“C.L.A.W.” Hypothesis
Photosynthesis
+
aerosols and cloudiness+
Cloud Forcings and Feedbacks
Low altitude thick clouds
Stratus
High altitude thin ice clouds
Cirrus
Aircraft emit particles (and particle precursors) which can nucleat clouds.
This activity gives rise to a
Posi
tive
radia
tive
for..
.
Neg
ativ
e ra
diat
ive
fo...
43%
57%1. Positive radiative
forcing2. Negative
radiative forcing
Aviation Contrails—Positive Forcing
October 2004
Clouds and Climate—a complex problem
Cirrus: Not so reflective, but absorb and emit at cold T
Low Clouds: Absorb IR but emit like warm surface. Reflective
Clouds and Cloud Feedbacks
Initial Forcing(e.g. GHG, solar radiation)
Temperature
Temperature
+
+
Low Clouds+
High Clouds+
-
+
Atmosphere holds more water
Atmosphere holds more water
Uncertain!
Increased greenhouse effect
Albedo
+
Predicted Changes in Cloud Forcings
Figure 10.11
IPCC 2007
Sunspots – Cyclic Changes in Solar Output
~11 year Sunspot Cycle
Radiative Forcing by Solar Cycle
The solar cycle forcing has increased from -0.1 to 0.2 W/m2 since 1900. This forcing can explain ____ of 1oC increase in global Avg. T
since 1900
60
- 70%
40
- 50%
20
- 30%
5%
75%
20%
1. 60 - 70%2. 40 - 50%3. 20 - 30%
False Assertions: Sun – Global Warming
Originally from WSJ Article written by two chemists named Robinson
WRONG Solar Cycle
WRONG T record
False Assertions: Sun – Global Warming
Correct cycleLaut 2003
T Response After Major Eruptions
FAQ 8.1, Figure 1
Natural and Anthropogenic Forcings
Figure 6.13
El Nino Southern Oscillation-ENSO
Neutral Walker Circulation
Neutral
El Nino/La Nina State Flip-Flop
El Nino/La Nina Circulation Patterns
Very Strong El NinoStrong La Nina
ENSO “Periodicity”
El Niño years
La Niña years
El Nino Global Impacts
El Nino Impact on Fish
Normal El Nino
Climate History
18O Ratios in Sediment and Ice Core
Pleistocene Glacial and Interglacials
Reconstruction of land and sea ice 21,000 years ago (last glacial maximum)
February
July
Records of NH GlaciationsGeological Records: glacial deposits, scarring, larger scale
Cordilleran Ice SheetLake MissoulaSpokane Floods (from Lake Missoula)
Milankovitch—Before sediment cores
Predicts glacial and interglacial transitions based on variations in Earth’s orbit
His results suggested many such transitions in ~ 1 million yrs (he was right)
—at the time, no observable records show that many, so his work widely criticized
Milutin Milankovitch
Milankovitch Continued
“I do not consider it my duty to give an elementary education to the ignorant, and I have also never tried to force others to use my theory, with which no one could find fault.”
While lacking patience for critics, he did not lack confidence
Milutin Milankovitch
Orbital Forcing Summary
FAQ 6.1, Figure 1
Eccentricity
Tilt
Precession
IPCC 2007
Orbital Forcing Summary Cartoon
• orbital forcings
Currently NH summer takes place at aphelion, in about 12,000 years, NH summer
will occur at perihelion. At this time, SH seasonality will be
stro
nger
wea
ker
54%
46%
1. stronger2. weaker
Solar Insolation at 65N and Glaciation
Recent UW Research
Time rate of change of ice volume and solar insolation
The Key For Glaciation
Solar insolation in NH summer appears to be key maintaining glaciation. Ice sensitive to melting!
Initial ForcingWeaker NH summer insolation
T- Albedo
+
-
Ice Coverage
+
Positive Feedback—Destabilizing Climate
Same old ice-albedo feedback, just different initial forcing
Questions—In Class Activity
1. Given the behavior of CO2 and CH4 is there a positive or negative feedback with T?
2. Provide a feedback involving marine biota which might explain CO2’s behavior.
3. Suppose marine biota are the cause of CO2’s behavior, is this support for or against Gaia theory?
4. When’s the next glacial maximum? Do you think we’ll get there?
Eccentricity: More to Less Circular
Obliquity: More or Less Seasonality
Precessional Cycle: Tilt and Eccentricity
Current situation