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Facts and Myths about Global Warming John R. Christy NWS Climate Services University of Alabama in Huntsville 20 June 2007

Facts and Myths about Global Warming John R. Christy NWS Climate Services University of Alabama in Huntsville 20 June 2007

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Facts and Myths about Global

WarmingJohn R. Christy

NWS Climate Services

University of Alabama in Huntsville20 June 2007

Consensus is not Science

Michael Crichton

Consensus is not Science

William Thompson (Lord Kelvin)

All Science is numbers

Michael Crichton

Some people will do anything to save the Earth ...

except take a science course.

Some people will do anything to save the Earth ...

except take a science course.

Greenhouse “Affect”, Rolling Stone

P.J. O’Rourke

Two Main observing systems for detecting

Greenhouse Gas effects

• Surface thermometers– Daily High Temperature– Daily Low Temperature– Daily Mean Temperature

(popular)

• Upper Air Temperatures– Balloon – Microwave emissions

"Global" Surface Temperature HadCRUT3

-0.8

-0.6

-0.4

-0.2

0.0

0.2

0.4

0.6

1850 1870 1890 1910 1930 1950 1970 1990 2010

Constructed from Mean Temperatures

Vertical Temperature Change due to Greenhouse Forcing in

Models

Model Simulations of Tropical Troposphere Warming:About 2X surfaceLee et al. 2007

Is Mean Surface Temperature an

Appropriate Index for the Greenhouse Effect?

TMean = (TMax + TMin)/2

Day vs. Night Surface Temp

Nighttime - disconnectedshallow layer/inversion. Temperature affected by land-use changes, buildings, farming, etc.

Daytime - deep layer mixing, connected with levels impacted by enhanced greenhouse effect

Night Surface Temp

Nighttime - disconnectedshallow layer/inversion. But this situation can be sensitive to small changes such as roughness or heat sources.

Buildings, heat releasing surfaces, aerosols, greenhouse gases, etc. can disrupt the delicate inversion, mixing warm air downward - affecting TMin.

Warm air above inversion

Cold air near surface

Warm air

The nighttime minimum is related to the delicate formation of the nocturnal boundary layer which can be easily disrupted, mixing warm air downward and sending temperatures up dramatically

Walters et al. (in press)

No. Alabama Summer TMax Temperatures

28

30

32

34

36

1890 1910 1930 1950 1970 1990 2010

Observations: -0.13 °C/decade

Christy 2002

Mean TemperatureSoutheast USA 1899-2003

-0.06

-0.04

-0.02

0.00

0.02

0.04

0.06

0.08

0.10

0.12

0.14

Observations BCM CCMA CCMA_T63 CSIRO GFDL_0 GFDL_1 IPSL MIROC3 MPI MRI

ModelsObservation

Christy et al. 2006, J. Climate

MODIS21 Jul 2002

Jacques DescloitresMODIS Land Rapid Response Team NASA GSFC

+ Valley Stations° Mountain Stns

•Christy et al. 2006, J. Climate

Manually digitized thousands of records

CA Valley and Sierra (Jun-Nov) 1910-2003

8

12

16

20

24

1910 1920 1930 1940 1950 1960 1970 1980 1990 2000 2010

°C

Valley TMax (less 10°C)Valley TMinSierra TMin

Christy et al. 2006Valley affected by irrigation and urbanization

Christy et al. 2006

Consistent with irrigationConsistent with irrigation and urbanization

Snyder et al. 2002

Sierras warm faster than Valley in model simulations

East Africa (Kenya/Tanzania)

-0.1

0.0

0.1

0.2

0.3

0.4

0.5

0.6

Trend 1979-2004

°C/decade

GISSHadCRUT3CRUT3vTMinTMeanTMaxUAH SatelliteBalloon HadAT (0.0)Balloon ECMWF (0.0)

East Africa: 5°S-Eq, 35-40°E(Nairobi, Mt. Kilimanjaro, Mt. Kenya)

Daytime warming rate 20% of Mainline Datasets in E. Africa

Christy et al. (submitted) uses 10 times the amount of surface data

Upper Air

0.00

0.01

0.02

0.03

0.04

0.05

0.06

1900-1999

°C/decade

GHCN ObsCSIRO (3)GISS (2)INM-CM3.0MIROC3.2 (4)NCAR CCSM3.0 (2)NCAR PCM1 (2)GCM Avg

Model vs. ObservationsTMin minus TMax

Preliminary study

Is Mean Surface Temperature an

Appropriate Index for the Greenhouse Effect?

Evidence indicates TMax is the better metric to serve as a proxy for monitoring deep atmospheric change

Pielke et al. 2007, Walters et al. 2007, Christy et al. (submitted)

Upper Air Temperatures

Upper Air Temperatures

• Recent claims suggest the upper air temperature record is in agreement with the surface and with climate models, so global warming theory must be right

• IPCC more or less supports this view

• UAH satellite data reportedly “flawed”

Vertical Temperature Change due to Greenhouse Forcing in

Models

Model Simulations of Tropical Troposphere Warming:About 2X surfaceLee et al. 2007

Christy and Spencer 2005Christy and Norris 2006Christy et al. 2007

Christy and Norris 2006Christy et al. 2007

-0.6

-0.4

-0.2

0.0

0.2

0.4

0.6

0.8

1.0

1978 1982 1986 1990 1994 1998 2002 2006

Global Bulk Atmospheric TemperaturesUAH Satellite Data

Warming rate 60% of model projections

Greenhouse Effect

Total Greenhouse Effect

• Water vapor and Clouds Dominate

• Total Greenhouse Effect is variable

• Climate models show strong water-vapor/cloud positive feedback with increased CO2

Greenhouse Effect

0

20

40

60

80

100

Percentage Greenhouse Effect

Water Vapor and Clouds

CO2

Other

Greenhouse Effect

0

20

40

60

80

100

Percentage Greenhouse Effect

Water Vapor and Clouds

CO2

Other

?

Tropical Temp. and Cloud Forcing (major part of total greenhouse effect) based on

latest satellite sensorsNegative feedback on monthly time scales

Spencer et al. (submitted)

-3

-2

-1

0

1

2

-0.2 0 0.2 0.4

Troposphere Temp Anomaly

LW+SW CRF (W/m2)

What aboutCold Places?

North Polar RegionsHadCRUT3

-5

-4

-3

-2

-1

0

1

2

3

1850 1880 1910 1940 1970 2000

Arctic 70-85NGreenland

Period of most polar ice observations

Greenland Summer Temperatures

1780-2005

3

4

5

6

7

8

9

1780 1820 1860 1900 1940 1980

JJA11-season average

Period of most polar ice observations

Greenland Borehole TemperatureDahl-Jensen et al. 1998

-32.5

-32.0

-31.5

-31.0

-30.5

0 500 1000 1500 2000

Greenland Borehole TemperatureDahl-Jensen et al. 1998

-35.0

-34.0

-33.0

-32.0

-31.0

-30.0

-29.0

-8000 -6000 -4000 -2000 0 2000

AlaskaHadley CRU 3 (°C)

Shift in 1977, but high natural variability

-4

-3

-2

-1

0

1

2

3

4

1900 1920 1940 1960 1980 2000

When Hemingway writes “Snows of

Kilimanjaro”—half of the “snows” are

already gone

X

-5

-4

-3

-2

-1

0

1

2

3

4

1955 1965 1975 1985 1995 2005

Arusha/Kilimanjaro

TMax

Mass Gain in 2006Molg and Kaser 2007

Regional Snowpack, Central Andes, 1951-2005Masiokas et al. 2006

Schneider et al. 2006

Antarctica

-3.5-3.0-2.5-2.0-1.5-1.0-0.50.00.51.01.5

1940 1955 1970 1985 2000 Thermometers

Ice Cores

Doran et al. 2002

Antarctica snowaccumulationtrends cm/yr

1992-2003

Davis et al. 2005

See also:Monoghan et al 2006Van de Berg et a. 2006

Evidence Thus Far

• Global surface temperature is rising, but in a way inconsistent with model projections of GHG forcing

• Overall decline in ice mass, with sea level rise of about 1” per decade

• Severe weather not becoming more frequent

Main Point:

I don’t see a disaster developing

But, suppose you do ….

Energy Technology1900: World supported

56 billion human-life years

Energy Technology1900: World supported

56 billion human-life years

2005: World supports 429 billion

human-life years

Kenya, East Africa

Energy Transmission

Energy System

Energy Use

Energy Source

All Science is Numbers

• The Human population currently uses energy at a rate of 14 terawatts to its considerable benefit.

All Science is Numbers

• The Human population currently uses energy at a rate of 14 terawatts to its considerable benefit.

• Most energy production relies on burning carbon (i.e. CO2 is released)

All Science is Numbers

• The Human population currently uses energy at a rate of 14 terawatts to its considerable benefit.

• Most energy production relies on burning carbon (I.e. CO2 is released)

• To replace 10% of this (i.e. 1.4 terawatts) requires 1000 nuclear power plants (1.4 gigawatt each)

IPCC “Best Estimate” Temp

0.0

0.5

1.0

1.5

2.0

2.5

3.0

199020002010202020302040205020602070208020902100

A1B

California AB 149326% CO2 reduction LDV 2016

0.0

0.5

1.0

1.5

2.0

2.5

3.0

199020002010202020302040205020602070208020902100

A1BCANo. EastUSA

Net Impact if all US 0.01°C 2100

Net Effect of 10% CO2 emission reduction to A1B Scenario

(~1000 Nuclear Plants by 2020)

0.0

0.5

1.0

1.5

2.0

2.5

3.0

199020002010202020302040205020602070208020902100

A1B Emissions

10% Reduction A1B

Net Impact 0.07°C 2050

OR A MORE RATIONAL APPROACH?

• In 50 years will we learn that the most cost-effective path was to adapt to changes we actually observed and measured, rather than try to outguess Mother Nature’s course?

• In 50 years will we be surprised not by climate change but by the inventive minds of our scientists and engineers as they discover profitable and affordable ways to generate energy without carbon emissions?