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Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

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Page 1: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Summary And Transition: Past, Present And Future Climates

Western Interior Paleontological Society

Paul E. Belanger, Ph.D.

WIPS 1ST VP

Page 2: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

ACKNOWLEDGEMENTSBob Raynolds

Jonathan Bujak

Dag Nummedal

Ian Miller

Peggy LeMone

Caspar Ammann …et al. that I did not mean to omit

Global Warming/Climate Change – Resource Issues – Alternatives Study Group:

FTP SITE: https://sslaccess.elkresources.net/files/

Page 3: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

THE PRESENT IS THE KEY TO THE PAST (LYELL) IS also

THE KEY TO THE FUTURE

Page 4: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

THE PAST

Page 5: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

FROM CSI TO GSI:GEOLOGICAL SAMPLE

INVESTIGATION

LET THE EVIDENCE SPEAK

FOR ITSELF

Page 6: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

WE CALL THIS EVIDENCE

“PROXY” DATA

Page 7: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

• Strandlines/shorelines• Moraines• Till• Kettle lakes, etc.

SOME OF THE EARLIEST PROXY DATA

WAS FROM TERRESTRIAL DEPOSITS

We may know what caused these today, but imagine back then?

Page 8: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

IT’S THE INTERPRETATION THAT’S NOT ALWAYS CORRECT

Darwin observed ancient Alpine shorelines:

interpreted as ocean shoreline

Agassiz – later correctly interpreted as ice-dammed lake-shore strandlines/shoreline

Page 9: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

• Jean Louis R. Agassiz

• “Father” of Glaciology

• 1807-1873

• Paleontologist

• Glaciologist

Page 10: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Photographic proxy data/evidence

Ruddiman, 2008

Page 11: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

EARLY PROXY DATA:

TREE RINGS

Page 12: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Pollen & Lake core data

Ruddiman, 2008

Page 13: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

PROXY DATA:

POLLEN DATA

Page 14: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

PROXY DATA:

LEAVES

Page 15: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Tree rings, corals, ice cores

Ruddiman, 2008

Page 16: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

PROXY DATA:

ICE CORES

Page 17: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

TERRESTRIAL DATA

North American:

Wisconsin

Illinoian

Kansan

Nebraskan

European:

Wurm

Riss

Mindel

Gunz

Page 18: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

LATER EVIDENCE CAME FROM

THE MARINE RECORD

NOT WITHOUT IT’S PROBLEMS,

BUT MORE COMPLETE

Page 19: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

CesareEmilani:

Paleontologist,Chemist

Father of Paleoceanography

Page 20: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Other Paleoceanographers

Wally Broecker

Thermal-haline

“conveyor” belt of circulation

Page 21: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Bill Ruddiman

Nick Shackleton

Other Paleoceanographers

Page 22: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Other Paleoceanographers

John Imbrie:

CLIMAP

Page 23: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

PROXY DATA:

CORE DATA

Page 24: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

PROXY DATA:

BENTHIC

FORAMS

Page 25: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

PROXY DATA:

PLANKTONIC

FORAMS

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Deep Sea Coring

Ruddiman, 2008

Page 27: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Wikipedia

Proxy data: stable isotopes

Page 28: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

- SO – WHAT CONTROLS

CLIMATE

Page 29: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Gerhard et al., 2001

Page 30: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

OF HUGE IMPORTANCE:

•DISTRIBUTION OF CONTINENTS WITH RESPECT TO LATITUDE

•OCEAN CIRCULATION

•OPENING OF THE DRAKE PASSAGE:

ISOLATING ANTARCTICA

•BARRIERS TO EQUATORIAL CIRCULATION:

CLOSING OF ISTHMUS OF PANAMA 3-5 Ma

Page 31: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

bipolar glaciation

geologically rare

possibly unique

we think of this as ‘normal’…but

Page 32: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Icehouse Earth

Page 33: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Milankovitchcycles

(forcing factors)

Page 34: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

MILANKOVITCH CYCLES ARE

REFLECTED IN THE GEOLOGIC RECORD

Page 35: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Wikipedia

Cenozoic Climate Record

Page 36: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Wikipedia

Climate Changes from Ocean Sediment Cores, since 5 Ma. Milankovitch Cycles

Page 37: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Brook, 2008 Nature

The Ice Record: MilankovitchEmpirical

Interpreted

Page 38: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Gerhard et al., 2001

Page 39: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

BUT IS THIS CORRECT?

Does CO2 always have a lesser role in controlling climate?

Page 40: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

HERE’S THE LONG TERM RECORD

Shellito

Fricke

Jacobs

Page 41: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Snowball Earth

~650 Ma

Page 42: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

WHAT CONTROLS THE LONG-TERM RECORD?

IS IT STRICTLY CONTINENTAL POSITIONS

AND OCEANIC CIRCULATION?

Page 43: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

TODAY WE SAW EOCENE EVIDENCE

OF A WARMER CLIMATE

Page 44: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

BallantyneShellito

Fricke

Jacobs

Page 45: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

In particular we saw a VERY DRAMATIC increase in temperature in an

environment of already HIGH CO2 VALUES when there was an additional

spike of Methane and CO2

Page 46: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Wikipedia

Proxy data: stable isotopes

Page 47: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP
Page 48: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Fossil Lotus

Courtesy K. Johnson

Page 49: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Living LotusCourtesy K. Johnson

Page 50: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

BUT MARY KRAUS DIDN’T TELL US ABOUT THIS GUY!

Page 51: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

RECENT FIND IN COLUMBIA

Page 52: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

HERE’S NEW COMPELLING DATA FROM THE EOCENE

Page 53: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Early Eocene supergreenhousewas followed immediately by abrupt global cooling

What forced this change?

Bujak, pers. Comm.

Page 54: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

ACEX – ARCTIC CORING EXPEDITION

Expedition 302 - Arctic Coring Expedition

August-September 2004

Page 55: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Lomonosov Ridge

Page 56: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

P/E World

No Polar Ice Caps

From Blakey (2007)

Page 57: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

ARCTIC EVENTS PROXY DATA

Brinkhuis et al,, 2006

Moran et al., 2006

Page 58: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

THE EVIDENCE DOCUMENTS AN

800,000 YEARS SEQUESTRATION

EVENT CALLED THE AZOLLA

EVENT

Page 59: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

ACEX results

• 1400 ft (420m) cored section

• good Paleocene Eocene section recovered

• cored the “Azolla event”

• cored the PETM

Bujak, pers. Comm.

Page 60: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

ACEX Azolla core

• >8 metre ACEX core with 90% Azolla

• Azolla occurs as laminated layers

• indicates Azolla deposited in situ

• bottom-water anoxia at ACEX site

Bujak, pers. Comm.

Page 61: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

?

Azolla eventbase middle Eocene49 Ma

Bujak, pers. Comm.

Page 62: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

the massive decrease in

atmospheric CO2?

Bujak, pers. Comm.

UNPRECEDENTED DROP IN CO2

Page 63: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

the fastest growing plant on the planet!

it can double its biomass in 2 to 3

days

Bujak, pers. Comm.

Page 64: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

the key is in Azolla’s leaf

structure

source: Carrapiço, 2002

Bujak, pers. Comm.

Page 65: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Not unlike the increase GHGs at Paleocene-Eocene causing a significant warming, there appears to be a strong suggestion that this Azolla sequestration of carbon GHGs for a period of about 800,000 years correlates to an ensuing cooling of the globe.

That is NOT to say tectonic events like the opening of the Drake Passage are not also of great significance – particularly in the isolation of Antarctica and its subsequent glaciation and contribution to global cooling.

Page 66: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP
Page 67: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

HERE’S THE LONG TERM RECORD

Shellito

Fricke

Jacobs

Page 68: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

FOR LONG-TERM CLIMATIC CHANGES

THE EVIDENCE SUGGESTS:

Page 69: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Royer et al., 2003

Geologic cycles: Climate through

the Phanero-

zoic—carbon is the culprit

Page 70: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

IMAGINE THIS:

IT’S ALSO TRUE FOR OTHER PLANETS

Page 71: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

No sinks: Runaway Greenhouse Effect

• 97% carbon dioxide• 3% nitrogen• Water & sulfuric acid

clouds• Temperature:

>800°F – more than twice as hot as Mercury

Venus

Page 72: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

The Many Time Scales of Climate Change• Daily to several years: Weather – not Climate

1oUNDER THE INFLUENCE OF solar, El Ninos, volcanism, INCREASE IN GHGs, etc. •Century: the climate change the IPCC and people everywhere are worried about, because it affects the economy of society, and tracks man’s direct impact

• Centuries to millennia – Dansgaard-Oeschger cycles; Heinrich events

1oUNDER THE INFLUENCE OF MILANKOVITCH CYCLES, although abrupt & rapid changes in CO2 (as occurred at the PETM) can be influential

• 20Ka to 400 Ka years – Milankovitch cycles - insolation due to earth’s orbital changes

1oUNDER THE INFLUENCE OF CO2

• 1Ma to many millions (Ma) years – Pennsylvanian ‘ice house’ and Cretaceous ‘greenhouse’ due to plate tectonic cycles of continental assembly and break-up and vertical movements. Cycling of CO2 into and out of earth

Page 73: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

The Many Time Scales of Climate Change(cont.)

Unique events: “Snowball earth” in late Proterozoic (and more?)Large volcanic eruptions (OAE-2 at C/T boundary)PETM – major heat spike release of methane clathrates

Message: Don’t confuse the causes of climate change at one time scale with the drivers of change at another.

Page 74: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

The Long-term carbon cycle and Earths climate:

Carbon cycles:Long-term carbon cycle (millions of yrs)

• Driver of long-term climate changes along with continental and ocean-circulation changes

• Responsible for Icehouses/GreenhousesShort-term carbon cycle (~1,000s to 1,000,000 yrs)

• CO2 currently amplifies glacial-interglacial contrasts

Long-term carbon cycle and today:• Burning fossil fuels is like setting off volcanoes >100

times faster than present eruptions rates• Running a global experiment, which in not analogous

to glacial-interglacials – BUT MAY BE ANALOGOUS to the PETM.

Page 75: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

THE PRESENT(and near future)

Page 76: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

THE PRESENT

So what’s going on today?

What’s going to happen in the short-term?

Page 77: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Today’s Unique Event: Anthropogenic Global Warming

Today

CO2 for thepast 400 ky

Pliocene levelsof 385ppm

Page 78: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

1946 – 1950

svs.gsfc.nasa.gov

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2002 - 2006Temperature

svs.gsfc.nasa.gov

Page 80: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Arctic Sea Ice Extent

If sea-ice continues to contract rapidly over the next several years, Arctic land warming and permafrost thaw are likely to accelerate.David Lawrence, NCAR

Satellite imagery of sea ice extent in September1979, and at a record low in September 2007. Source: NASA

Page 81: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP
Page 82: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

NOAA web site archives & Peter Tans

The State of Affairs

Page 83: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Wikipedia

Distribution of Warming: Polar/Cold Regions

Page 84: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP
Page 85: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP
Page 86: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

HOWEVER: THE LATEST DATA THRU 2007

SUGGESTS GREEN HOUSE GASES ARE MATCHING AND OVERTAKING

TSI VARIATIONS

NCAR: Caspar Amman, 2007

Page 87: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

LOWER VS. UPPER ATM.

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Page 89: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP
Page 91: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

CHOICES• DO NOTHING and adapt (there WILL be a REAL cost here too)

• MITIGATE (or attempt to) and adapt:– Sequester– Alternate energy sources– Geo-Engineering options– Etc.

• Promote population control: “wear a condom at every ‘conceivable’ moment”

• THINK about it

• But ultimately: CHOOSE WHAT TO DO IN LIFE BEFORE LIFE CHOOSES WHAT YOU DO

Page 92: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

THE FUTURE(Beyond the Anthropomorphic Period)

Page 93: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

FUTURE CLIMATE?

Crowley & Hyde, 2008

PAST

FUTURE

Page 94: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

FUTURE CLIMATE?

Crowley & Hyde, 2008

PAST

FUTURE

Higher

Lower

-

-

-

-Glacial

Interglacial

PAST

FUTURE

Higher

Lower

-

-

-

-Glacial

Interglacial

Page 95: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

FUTURE CLIMATE?

Crowley & Hyde, 2008

PAST

FUTURE

Page 96: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Look at the Trend:Any reason to think it might not

continue?

Time, Ma

Page 97: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

IN SUMMARY:THE PASTPRESENT

AND FUTURE

Page 98: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

BallantyneShellito

Fricke

Jacobs

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TOMORROW(AS IN 14 HOURS FROM NOW)

Page 100: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Western Interior Paleontological SocietyFounders Symposium

Sunday, March 15th 2009

NCAR/UCAR: NOAA:

Page 101: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

NCAR/UCAR GUIDES(Coordinated by Peggy LeMone)

BE THERE AT 8:30 a.m. / 1:00 p.m.2 Groups

Kyle Ham• Current Position: Education Specialist and Bilingual

Educator• University Corporation for Atmospheric Research

(UCAR)• Office of Education and Outreach

Teri Eastburn,• Coordinator, Public Programs• University Corporation for Atmospheric Research

(UCAR)• Office of Education and Outreach

Page 102: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

NOAA (National Oceanic Atmospheric Administration)

(Coordinated by Dan Winester) BE THERE AT 8:30 a.m. / 1:00 p.m.

Groups of 3

Don Mock, William Murtagh, George Sharman, & Sandy MacDonald:

NOAA; ESRL (Earth Systems Research Lab); SWPC (Space Weather Prediction Center); NGDC (National Geophysical Data Center)

Page 103: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

NOAA (cont.)

SOS: Science on a Sphere.  This a 3D display of global (and astronomic) projected onto a large sphere.  The audience can view and walk around the sphere to bet a global view of data sets.  NOAA has over 200 data sets, including time-varying ones.  Such data sets as atmospheric processes, plate tectonics, topography, lights at night etc. (40 minutes)

ESRL and other NOAA (Earth Systems Research Lab): (40 minutes)Greenhouse gas lab weather forecast officeWind profilerHigh performance computing centerOzone chemistry

SWPC:  Space Weather Prediction Center (20 minutes)Effect of solar storms on electrical transmission, broadcasts, animal navigationGeomagnetic disturbances

NGDC:  National Geophysical Data Center (20 minutes)Large array storageNight time lightsPaleoclimatology (Tree rings, ice cores, geologic cores)

Page 104: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

ACKNOWLEDGEMENTSBob Raynolds

Jonathan Bujak

Dag Nummedal

Ian Miller

Peggy LeMone

Caspar Ammann …et al. that I did not mean to omit

Global Warming/Climate Change – Resource Issues – Alternatives Study Group:

FTP SITE: https://sslaccess.elkresources.net/files/

Page 105: Summary And Transition: Past, Present And Future Climates Western Interior Paleontological Society Paul E. Belanger, Ph.D. WIPS 1 ST VP

Western Interior Paleontological Society

QUESTIONS?