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Weather and Climate Extremes John W. Nielsen-Gammon Texas State Climatologist

John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

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Page 1: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Weather and Climate Extremes

John W. Nielsen-Gammon Texas State Climatologist

Page 2: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

What’s a Weather or Climate Extreme?

Page 3: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

What’s a Weather or Climate Extreme?

• Something unusual • Something high-impact

Page 4: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Why Do People Care About Weather or Climate Extremes?

Page 5: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Why Do People Care About Weather or Climate Extremes?

• Something unusual • Something high-impact

Page 6: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 7: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

40

-10

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80

0

1989

Page 10: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

80

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1949

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80

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1930

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1899

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115

90

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9.05

Page 21: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Weekly number of flood reports through November

Page 22: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 23: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

0

5

10

15

20

25

Page 24: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

20

25

30

35

15

10 5

0

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0

1

Page 27: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 28: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 29: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 30: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 31: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 32: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 33: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

World record: 21.93” in 2h 45m, Woodward

Ranch, D’Hanis, Texas

Page 34: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Extreme Weather and Climate Change

Page 35: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

The Four Pillars of Attribution of Trends to Climate Change

The greater the number of solid pillars, the greater the scientific confidence that cause and effect has been identified

Presenter
Presentation Notes
The ‘pillar’ slides are adapted from the 2016 NAS report on extreme event attribution, except that I added my own judgment on coastal flooding because the NAS report did not address it.
Page 36: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

The Four Pillars

Solid observed

trend

Page 37: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

The Four Pillars

Solid observed

trend

Known reason for

change

Page 38: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

The Four Pillars

Solid observed

trend

Known reason for

change

Good modeling

ability

Page 39: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

The Four Pillars

Solid observed

trend

Known reason for

change

Good modeling

ability

No outside

influences

Page 40: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

IPCC SREX

National Centers for Environmental Information

Page 41: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

IPCC SREX

National Centers for Environmental Information

Page 42: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

IPCC SREX

National Centers for Environmental Information

Page 43: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

National Centers for Environmental Information

Page 44: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

National Centers for Environmental Information

Page 45: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Climate change turned a 96°F day into a 100°F day

National Centers for Environmental Information

Page 46: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Climate change turned a 96°F day into a 100°F day

Climate change turned a 4°F above normal day into an 8°F above normal day

National Centers for Environmental Information

Page 47: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Climate change turned a 96°F day into a 100°F day

Climate change turned a 4°F above normal day into an 8°F above normal day

Climate change increased the odds of at least 100°F from 1:50 to 1:7

National Centers for Environmental Information

Page 48: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Texas Precip thru 2016: +8.5%

Page 49: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

The Four Pillars

Solid observed

trend

Known reason for

change

Good modeling

ability

No outside

influences

Page 50: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Texas Rainfall

Solid observed

trend

Known reason for

change

Good modeling

ability

No outside

influences

✔ ✖

Page 51: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 52: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Texas Rainfall

Solid observed

trend

Known reason for

change

Good modeling

ability

No outside

influences

✔ ✖ ✖

Page 53: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Texas Rainfall

Solid observed

trend

Known reason for

change

Good modeling

ability

No outside

influences

✔ ✖ ✖ ✔

Page 54: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Texas Very Heavy Rainfall

Solid observed

trend

Known reason for

change

Good modeling

ability

No outside

influences

✔ ✔ ✔

Page 55: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

What makes rainfall different from very heavy rainfall?

Page 56: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

IPCC AR5, WG1, Fig. 2.8

56 (50,62)

Tweaked from:

Presenter
Presentation Notes
I find that treating IR radiation as net radiation eliminates many opportunities for misunderstandings and misconceptions, including all that ‘back-radiation’ nonsense and the erroneous idea that the key effect of greenhouse gases on surface temperature comes through downwelling radiation. Overarching concept here: heat from the Sun flows mainly to the Earth’s surface. Heat escaping from the Earth comes mainly from the atmosphere (primarily the troposphere). Heat flows from the Earth’s surface to the troposphere, closing the loop. This is why the troposphere generally gets cooler with altitude, and the rate of cooling with altitude is mostly set by thermodynamics. (The stratosphere gains heat mainly from direct absorption of sunlight, so its temperature isn’t interconnected with what’s happening at ground level.)
Page 57: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

The Faucet

• Warmer air can carry more water = bigger pipe + 7% per °C

• The effect of weather patterns = turning the handle

Presenter
Presentation Notes
Thermodynamic vs. dynamic influences of climate change
Page 58: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

The Faucet

• The size of the pipe matters most when the faucet is wide open

Presenter
Presentation Notes
Extreme rainfall is dominated by the thermodynamic influence. This is confirmed by observed magnitude of changes in extreme rainfall amounts.
Page 59: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

National Centers for Environmental Information

Page 60: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

National Centers for Environmental Information

Page 61: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

National Centers for Environmental Information

Page 62: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

National Centers for Environmental Information

Page 63: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Presenter
Presentation Notes
Based on spatial precipitation analyses, so underlying data is county-average daily precip, not point precip. Shown is literally the smoothed annual odds of a “one-year” rainfall event, but just explain that “1” is the expected long-term value assuming no trend. Note that the two counties south of Harris (Galveston and Brazoria) have a negative trend. Harris County has the largest positive trend but it seems to be a local outlier (Also, other big cities in Texas don’t have large positive trends.)
Page 64: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Statewide Extreme Rainfall Analysis

• For each county & each year: – Find stations with nearly-complete data – Pick the one with longest period of record

• Stitch together daily precipitation into one long time series

• Find events exceeding threshold • Sort chronologically, find date of middle event

Page 65: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Time

Page 66: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Time

Page 67: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Time

Events less frequent Events more frequent

Page 68: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Time

Events less frequent Events more frequent

new frequency old frequency

length of first period length of second period =

Page 69: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

*about once every 5000 days

Presenter
Presentation Notes
Presumably most of the spatial variation is due to the lack of statistical robustness in extreme rainfall statistics. In other words, one shouldn’t expect extreme rainfall in Harris County to continue increasing at an unusually rapid rate…indeed, a rebound to a temporarily flat trend is much more likely. But there’s a clear underlying upward trend. This is unpublished research, but peer-reviewed research does find an overall upward trend of similar magnitude for the south-central United States.
Page 70: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
Page 71: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Probable Maximum Precipitation

• The maximum amount of precipitation physically possible for a given basin over a given duration

• Used for critical infrastructure design – Dams – Nuclear power plants

Page 72: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather
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Page 74: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Hurricanes

National Centers for Environmental Information

Page 75: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Problems with Smaller-Scale Extreme Weather Phenomena

• Lack of stability in data record • Low signal-to-noise ratio • No direct information from climate models

National Centers for Environmental Information

Page 76: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Smaller-Scale Extreme Weather Phenomena

Solid observed

trend

Known reason for

change

Good modeling

ability

No outside

influences

✖ ✖ ?

Page 77: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Problems with Smaller-Scale Extreme Weather Phenomena

• Low signal-to-noise ratio – Natural (and random) variability drives

individual events and clusters – Small trends have large monetary impact – Once clear trend is detectable, it’s too late

National Centers for Environmental Information

Page 78: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Hurricanes: The Balance of Evidence

• Increase in peak intensity (1.5 pillars) • Decrease in frequency (1 pillar)

– …but spatially variable (1.5 pillars)

National Centers for Environmental Information

Page 79: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

National Centers for Environmental Information

Page 80: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

National Centers for Environmental Information

Page 81: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Change in hurricane frequency

National Centers for Environmental Information

Page 82: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Summary

• Extreme weather – Extremely unusual – Extremely impactful

• Texas gets extremes • Climate change affects extremes

– Not always worse – Often very hard to tell

Page 83: John W. Nielsen- Gammon Texas State Climatologisttxmn.org/wp-content/blogs.dir/1/files/2016/01/N-G_Montgomery.pdfJohn W. Nielsen- Gammon Texas State Climatologist . What’s a Weather

Contact Information

• John W. Nielsen-Gammon • [email protected] • 979-862-2248 • http://climatexas.tamu.edu • http://climatechangenationalforum.org • http://www.cpc.ncep.noaa.gov