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Global Warming and the Global Warming and the Dominican RepublicDominican Republic
Kerry EmanuelKerry Emanuel
Program in Atmospheres, Oceans, Program in Atmospheres, Oceans, and Climateand Climate
Department of Earth, Atmospheric Department of Earth, Atmospheric and Planetary Sciencesand Planetary Sciences
MITMIT
ProgramProgram
• History of the earth’s climateHistory of the earth’s climate
• The science of global warmingThe science of global warming
• Possible effects of climate change on the Possible effects of climate change on the Dominican RepublicDominican Republic
The Faint Young Sun Paradox: Why The Faint Young Sun Paradox: Why didn’t the Earth Freeze?didn’t the Earth Freeze?
The Snowball EarthThe Snowball Earth
A detailed record of the earth’s climate has A detailed record of the earth’s climate has emerged over the last few decades, from analyses emerged over the last few decades, from analyses
of ice cores and deep sea sedimentsof ice cores and deep sea sediments
Ice Cover, Last Glacial Maximum Ice Cover, Last Glacial Maximum (~18,000 years ago)(~18,000 years ago)
Paleo reconstructions of temperature change Paleo reconstructions of temperature change over the last 2000 yearsover the last 2000 years
Year
Instrumental Record
Estimates of Global Mean Surface Temperature Estimates of Global Mean Surface Temperature from the Instrumental Recordfrom the Instrumental Record
Some Characteristics of Climate Some Characteristics of Climate ScienceScience
• Described by some as the most difficult scientific problem ever faced
• Draws on all the major scientific disciplines:– Chemistry, geology, atmospheric science,
oceanography, solar physics, orbital mechanics, biology
– Climate prediction also requires understanding of economics, politics, human psychology
• Very much a frontier science
John Tyndall (1820-1893)
The Greenhouse EffectThe Greenhouse Effect
Tyndall’s Discovery:
Oxygen (O2) and Nitrogen (N2), which together comprise about 97% of the atmosphere, are transparent to solar and infrared radiation
If that’s all there were: 40
1(1 )4sT a S
= Stefan-Boltzmann constant
a = Planetary albedo
= Solar constant
0S
255 0sT K F
But certain trace gases interact strongly with radiation:
H20 (water vapor)
CO2 (carbon dioxide)
CH4 (methane)
Clouds also interact strongly with radiation. Together, they yield:
288 60sT K F
Elements of the Greenhouse EffectElements of the Greenhouse Effect
If the Only Feedback Were If the Only Feedback Were Temperature, Doubling Carbon Temperature, Doubling Carbon Dioxide would Increase Surface Dioxide would Increase Surface Temperature by about 1.1 Temperature by about 1.1 ooC.C.
Feedbacks in Climate ModelsFeedbacks in Climate Models
Water vapor Cloud Surface albedo
Lapse rate Water vapor + lapse rate
Climate Climate Forcing Forcing
by Orbital by Orbital VariationsVariations
Milutin Milanković, 1879-1958
Climate Forcing and ResponseClimate Forcing and Response
Black: Time rate of change of ice volumeBlack: Time rate of change of ice volume
Red: Summer high latitude sunlightRed: Summer high latitude sunlight
Strong Correlation between High Latitude Summer Strong Correlation between High Latitude Summer Insolation and Ice VolumeInsolation and Ice Volume
P. Huybers, Science, 2006
Causes of Recent Climate Causes of Recent Climate ChangeChange
Variation in Variation in carbon dioxide carbon dioxide and methane and methane over the past over the past 20,000 years, 20,000 years, based on ice based on ice core and other core and other recordsrecords
Contributions to net radiative forcing change, 1750-2004:Contributions to net radiative forcing change, 1750-2004:
Distribution of temperature change, 1901-2005Distribution of temperature change, 1901-2005
Global Climate Models: Global Climate Models: How Good Are They, and What How Good Are They, and What
Do They Tell Us about The Do They Tell Us about The Future?Future?
Global Climate ModelingGlobal Climate Modeling
• General philosophyGeneral philosophy:– Simulate large-scale motions of atmosphere,
oceans, ice– Solve approximations to full radiative transfer
equations– Parameterize processes too small to resolve– Some models also try to simulate
biogeochemical processes– First GCMs developed in 1960s
Equations solved by discretizing Equations solved by discretizing to finite volumesto finite volumes
Unresolved physical processes Unresolved physical processes must be handled parametricallymust be handled parametrically• Convection
• Thin and/or broken clouds
• Cloud microphysics
• Aerosols and chemistry (e.g. photochemical processes, ozone
• Turbulence, including surface fluxes
• Sea ice
• Land ice
• Land surface processes
Global mean temperature Global mean temperature (black) and simulations (black) and simulations using many different using many different global models (colors) global models (colors) including all forcingsincluding all forcings
Same as above, but Same as above, but models run with only models run with only natural forcingsnatural forcings
Projected Warming:Projected Warming:
Climate Risks to the Climate Risks to the Dominican RepublicDominican Republic
Warming RisksWarming Risks
• Rising sea level• Concentration of rainfall into fewer but more
intense events...more drought, floods• Increased incidence of some tropical diseases• Increased production of allergens• Increased mortality from heat waves• Increased consumption of electricity• Increase in violent hurricanes• Ocean acidification, increased species
extinctions
Sea Level, 1860-2003Sea Level, 1860-2003
Reconstructed
Tide Gauge
Satellite altimetry
Arctic Minimum Sea Ice ExtentArctic Minimum Sea Ice Extent
Greenland Greenland surface elevation surface elevation
change, 1989-change, 1989-20052005
Hurricane Power is Changing in Concert with Hurricane Power is Changing in Concert with Tropical Ocean TemperatureTropical Ocean Temperature
Today’s global climate Today’s global climate models are far too coarse to models are far too coarse to simulate tropical cyclonessimulate tropical cyclones
Our ApproachOur Approach• Step 1: Seed each ocean basin with a very large
number of weak, randomly located cyclones
• Step 2: Cyclones are assumed to move with the large scale atmospheric flow in which they are embedded
• Step 3: Run a coupled, ocean-atmosphere computer model for each cyclone, and note how many achieve at least tropical storm strength
• Step 4: Using the small fraction of surviving events, determine storm statistics.
200 Synthetic U.S. Landfalling tracks (color 200 Synthetic U.S. Landfalling tracks (color coded by Saffir-Simpson Scale)coded by Saffir-Simpson Scale)
Present Climate: Spatial Present Climate: Spatial Distribution of Genesis PointsDistribution of Genesis Points
Observed
Synthetic
Now Use Daily Output from IPCC Now Use Daily Output from IPCC Models to Derive Wind Models to Derive Wind
Statistics, Thermodynamic State Statistics, Thermodynamic State Needed by Synthetic Track Needed by Synthetic Track
TechniqueTechnique
1. Last 20 years of 20Last 20 years of 20thth century century simulationssimulations
2.2. Years 2180-2200 of IPCC Years 2180-2200 of IPCC Scenario A1b (COScenario A1b (CO22 stabilized at stabilized at
720 ppm)720 ppm)
Compare two simulations each Compare two simulations each from 7 IPCC models:from 7 IPCC models:
Change in Destructiveness of HurricanesChange in Destructiveness of Hurricanes
Return PeriodsReturn Periods
Sample Wind SwathSample Wind Swath
Sample Storm SurgeSample Storm Surge
Sample Rain SwathSample Rain Swath
Sample Rain Rate at Santa DomingoSample Rain Rate at Santa Domingo
Change in Landslide RiskChange in Landslide Risk
SummarySummary
• Earth’s climate has changed radically and often abruptly through time
• Primary culprits:– Changing insolation, through solar evolution and
orbital variations– Changing concentrations of trace greenhouse
gases– Changing concentration of aerosols: Volcanic
eruptions
• Evidence for human-induced climate change now very compelling
• Principle risks of Global Warming to the Dominican Republic:– Increased incidence of flash floods– Ocean acidification and damage to marine
ecosystems– Coastal flooding owing to sea level rise– Increased frequency and severity of
hurricanes, including storm surge and fresh-water flooding
Possible Benefits of Warming:Possible Benefits of Warming:
• Fewer deaths from exposure
• More vigorous plant growth
• Increase of arable land at high latitudes
• Increased mining potential in current permafrost regions
• Arctic waterways become navigable
• Reduced heating costs
Changing Distributions of PrecipitationChanging Distributions of Precipitation