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Climate Change, Texas, and the Limits of Confidence
John Nielsen-Gammon Dept. of Atmospheric Sciences Texas A&M University
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Global Surface Temperature (3)
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Pattern of Temperature Trend
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Regional Temperatures, 1-2000 (PAGES 2013)
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Multiple datasets & analyses (AR5 WG1 FAQ2.1)
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Mass change, ice sheets (AR5 WG1 Figs 4.13d-4.14d)
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Changes in Water and Ice (AR5 WG1 FAQ2.1)
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Global Surface Temperature (3)
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Global temperatures
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Global temperatures
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Global Energy Balance, Part 1
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Scientific Principles
Energy Imbalance implies a net gain or loss of energy Typical annually averaged energy imbalances are << 1% of the energy flow
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Global Energy Balance, Part 1
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 1
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 1
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 1
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 1
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 2
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 2
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 2
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 2
Sun Atmosphere Each arrow = 20 W/m2 Earth
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Global Energy Balance, Part 3
Sun Atmosphere To maintain heat flow into atmosphere, Earth must warm too Earth
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Detection and Attribution
Identify trend: detection Compare with distinct patterns in space and time caused by different forcing agents Apportion role of different forcing agents: attribution
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Evolution of Estimated Forcings (AR5 WG1 Fig. 8.18)
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Global temperatures
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Texas vs Globe
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Texas 5-yr Avg vs Globe
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Short definition: Weather that’s newsworthy Long definition: two kinds
Extreme Weather Short definition: Weather that’s newsworthy Long definition: two kinds Weather that’s extremely unlikely Weather that’s unhealthy or damaging (The same event often fits both definitions)
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Melissa Phillip, Houston Chronicle
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April 18, 2016
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August 28, 2017
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August 28, 2017 August 29, 2017
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Example #1: Heat and Cold
IPCC SREX
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The Three Pillars of Sound Attribution
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The Three Pillars of Sound Attribution
A clear historical trend
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The Three Pillars of Sound Attribution
Consistent model projections A clear historical trend
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The Three Pillars of Sound Attribution
Consistent model projections A clear historical trend A sound physical basis
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Example #2: Heavy Rain
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Climate change’s thermodynamic impact: the size of the pipe
The Faucet Climate change’s thermodynamic impact: the size of the pipe + 7% per °C Climate change’s dynamic impact: turning the handle
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The size of the pipe matters most when the faucet is wide open
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95% confidence interval using effective degrees of freedom estimated following D. A. Griffith & Z. Zhang (1999): Computational Simplifications Needed for Efficient Implementation of Spatial Statistical Techniques in a GIS, Geographic Information Sciences, 5:2, , DOI: /
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20% increase ~ 30% trend
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Arid Wet
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Harris County: 34”
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Example #3: Hurricanes
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Hurricanes: The Balance of Evidence
Increase in peak intensity (1.5 pillars) Decrease in frequency (1 pillar) …but spatially variable (1.5 pillars)
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Did Harvey stall because of climate change?
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National climate assessment News items
Resources IPCC.ch Special report on extremes (SREX) Fifth assessment report, working group 1 (AR5 WG1) National climate assessment News items AP + USA TODAY + NYTIMES ~ Network news
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The climate is changing Over the long haul, it’s us
Summary The climate is changing Over the long haul, it’s us Future changes are hard to pin down Some impacts are easy It’ll get warmer, it’ll rain harder Some impacts are hard More droughts? Fewer hurricanes?
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John W. Nielsen-Gammon n-g@tamu.edu 979-862-2248
Contact Information John W. Nielsen-Gammon
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