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This presentation explores the potential driver of Atlantic thermohaline circulation and its effects on hurricane activity in the Atlantic basin and United States landfalls. It concludes that multi-decadal variability in sea surface temperatures and sea level pressures is likely driven by changes in the strength of the Atlantic Thermohaline Circulation (THC).
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North Atlantic Ocean Multi-Decadal Variability Phil Klotzbach Department of Atmospheric Science Colorado State University Climate Diagnostics and Prediction Workshop October 23, 2007
Outline • Potential driver – Atlantic thermohaline circulation • Effects on Atlantic basin hurricanes • Effects on United States hurricane landfalls • Conclusions
160oW 20oE
SURFACE 500 METERS
Salt Water Density Fresh Water Density
H H 3 1 2 Courtesy of John Marshall (MIT)
NADW Tropics THC - Strong THC - Strong 20 Sr 20 Sr Negative buoyancy Positive buoyancy NADW THC - Weak THC - Weak 10 Sr 10 Sr Positive buoyancy Negative buoyancy
STRONG THC WARM
SSTA + SSTA - + – – SLPA – + SLPA + gyre - gyre + + – STRONG THC WEAK THC
FAST SLOW FAST SLOW Thermohaline Circulation Rate of Salt Buildup from (E-P) - River = 0 Salt Anomaly (S1) (S1) (S1) YEARS 30 60 90 120
THC STRONG CAT 3-4-5 TRACKS THC WEAK CAT 3-4-5 TRACKS
1950-1964 1997-2006 25 YEARS13 Major Hurricanes 1970-1994 25 YEARS3 Major Hurricanes 54 55 THC STRONG THC WEAK 85 54 55 54 60 89 59 04 50 92 05 04 50 60
Conclusions • Multi-decadal variability in Atlantic basin sea surface temperatures and sea level pressures exists and is likely driven by changes in strength of the Atlantic thermohaline circulation • Atlantic basin tropical cyclone activity (and especially major hurricane activity) is much more frequent during strong THC years • Florida peninsula and East Coast landfalls are dramatically altered by THC phase changes