Hurricanes and Global Warming- Dr. Kerry Emanuel
Upcoming SlideShare
Loading in...5
×
 

Like this? Share it with your network

Share

Hurricanes and Global Warming- Dr. Kerry Emanuel

on

  • 4,161 views

Dr. Kerry Emanuel explains how Global Warming increased the power of hurricanes. Hurricane Katrina is discussed, with the conclusion that Katrina probably would not have had the power to break the New ...

Dr. Kerry Emanuel explains how Global Warming increased the power of hurricanes. Hurricane Katrina is discussed, with the conclusion that Katrina probably would not have had the power to break the New Orleans levees in a pre-Global Warming world. April 2009 webinar presented by the Southern Allicance for Clean Energy (http://www.cleanenergy.org/) and the Gulf Restoration Network (http://healthygulf.org/) SlideCast by John Atkeison of the Alliance for Affordable Energy. There is a very small amount of phone noise.

Statistics

Views

Total Views
4,161
Views on SlideShare
4,148
Embed Views
13

Actions

Likes
0
Downloads
31
Comments
0

5 Embeds 13

http://www.slideshare.net 6
http://www.blogger.com 2
http://www.techpolicyreview.com 2
http://www.e-presentations.us 2
http://www.slideee.com 1

Accessibility

Upload Details

Uploaded via as Microsoft PowerPoint

Usage Rights

© All Rights Reserved

Report content

Flagged as inappropriate Flag as inappropriate
Flag as inappropriate

Select your reason for flagging this presentation as inappropriate.

Cancel
  • Full Name Full Name Comment goes here.
    Are you sure you want to
    Your message goes here
    Processing…
Post Comment
Edit your comment
  • Are hurricanes becoming more powerful and destructive? Are these changes due to a natural cycle of hurricane activity or are they caused by human-induced climate change? Although this is currently a hot debate among scientists, new research suggests that the destructive potential of hurricanes is increasing due to the heating of the oceans. Image: Satellite image of Hurricane Floyd approaching the east coast of Florida in 1999. The image has been digitally enhanced to lend a three-dimensional perspective. Credit: NASA/Goddard Space Flight Center.
  • This graph shows the PDI of hurricanes in the 20 th century to represent the change of hurricane intensity. This curve has been smoothed as in the previous slides.  The hurricane wind speed data used to make this graph are considered unreliable prior to 1948, the year that aircraft surveillance of hurricanes began.
  • This graph is similar to the previous graph,  but the ocean surface temperature has been added for comparison. The low value of storm power in the early 1940s is thought to be due to the lack of reports from ships at sea because of the radio silence imposed during WWII.

Hurricanes and Global Warming- Dr. Kerry Emanuel Presentation Transcript

  • 1. Hurricanes and Global Warming Kerry Emanuel Massachusetts Institute of Technology
  • 2. Issues
    • Effect of climate change on tropical cyclone activity
    • Role of tropical cyclones in the climate system
  • 3. Approaches
    • The historical record
    • Physics
    • Models
  • 4. The Historical Record
  • 5. Global TC Frequency, 1970-2006 Data Sources: NOAA/TPC and NAVY/JTWC
  • 6. Better Intensity Metric: The Power Dissipation Index A measure of the total frictional dissipation of kinetic energy in the hurricane boundary layer over the lifetime of the storm
  • 7. Atlantic Storm Maximum Power Dissipation (Smoothed with a 1-3-4-3-1 filter) Power Dissipation Index (PDI) Years included: 1870-2006 Data Source: NOAA/TPC
  • 8. Atlantic Sea Surface Temperatures and Storm Max Power Dissipation (Smoothed with a 1-3-4-3-1 filter) Scaled Temperature Power Dissipation Index (PDI) Years included: 1870-2006 Data Sources: NOAA/TPC, UKMO/HADSST1
  • 9. 10-year Running Average of Aug-Oct NH Surface T and MDR SST
  • 10.  
  • 11. Tropical Atlantic SST(blue), Global Mean Surface Temperature (red), Aerosol Forcing (aqua) Mann, M. E., and K. A. Emanuel, 2006. Atlantic hurricane trends linked to climate change. EOS, 87, 233-244. Global mean surface temperature Tropical Atlantic sea surface temperature Sulfate aerosol radiative forcing
  • 12. Best Fit Linear Combination of Global Warming and Aerosol Forcing (red) versus Tropical Atlantic SST (blue) Mann, M. E., and K. A. Emanuel, 2006. Atlantic hurricane trends linked to climate change. EOS, 87, 233-244. Tropical Atlantic sea surface temperature Global Surface T + Aerosol Forcing
  • 13. Physics
  • 14. Energy Production: The Hurricane as a Carnot Heat Engine
  • 15. Annual Maximum Potential Intensity (m/s)
  • 16. Observed Tropical Atlantic Potential Intensity Data Sources: NCAR/NCEP re-analysis with pre-1979 bias correction, UKMO/HADSST1 Emanuel, K., J. Climate , 2007
  • 17. Effect of Increased Potential Intensity on Hurricane Katrina
  • 18. Projecting into the Future: Downscaling from Global Climate Models
  • 19. Today’s global climate models are far too coarse to simulate tropical cyclones
  • 20. Our 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.
  • 21. 200 Synthetic U.S. Landfalling tracks (color coded by Saffir-Simpson Scale)
  • 22. Calibration
    • Absolute genesis frequency calibrated to North Atlantic during the period 1980-2005
  • 23. Genesis rates Atlantic Eastern North Pacific Western North Pacific North Indian Ocean Southern Hemisphere Calibrated to Atlantic
  • 24. Seasonal Cycles Atlantic
  • 25. Cumulative Distribution of Storm Lifetime Peak Wind Speed, with Sample of 2946 Synthetic Tracks
  • 26. Captures effects of regional climate phenomena (e.g. ENSO, AMM)
  • 27. Global Percentage of Cat 4 & Cat 5 Storms
  • 28. Now Use Daily Output from IPCC Models to Derive Wind Statistics, Thermodynamic State Needed by Synthetic Track Technique
  • 29. 1. Last 20 years of 20 th century simulations 2. Years 2180-2200 of IPCC Scenario A1b (CO 2 stabilized at 720 ppm) Compare two simulations each from 7 IPCC models:
  • 30. Basin-Wide Percentage Change in Power Dissipation
  • 31. 7 Model Consensus Change in Storm Frequency
  • 32. U.S. Coastal Damage Potential
  • 33.  
  • 34. Summary:
    • Tropical cyclones are sensitive to the climate state, as revealed by historical (and geological) data
    • Observations together with detailed modeling suggest that TC power dissipation increases by ~65% for a 10% increase in potential intensity
  • 35.
    • New technique for downscaling climate models shows promise for predicting response of global tropical cyclone activity to climate change
    • Climate models may have systematic errors that compromise estimates of tropical cyclone response to global warming