Transcript
Page 1: GEOG5839.01. Introduction to Dendrochronology

GEOG5839CHRONOLOGY

INTRODUCTION TO

DENDRO

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2012 Mar-May temperature anomaly!h"p://www.giss.nasa.gov/

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QUESTIONIs it unusual for the world to be this warm?

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Low reservoir

Source: Glen MacDonald

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QUESTIONIs there enough water in the Colorado River

to satisfy the expected need?

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QUESTIONWhen were these dwellings constructed

(and abandoned)and why?

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QUESTIONHow does weather and climate affect the risk and severity of forest fires?

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Source: U.S. Coast Guard, Lt. Brendan Evans

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QUESTIONHow often do natural hazards like floods occur,

and what factors make them more or less likely?

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Three li"le words achingly familiar on the Western farmer's tongue, rule life in the dust bowl of the continent – if it rains.“ ”

Associated PressApril 15, 1935

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There is nothing magical about the last one hundred years.“ ”

Dr. Balaji Rajagopalan University of Colorado

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CLIMATE HISTORY OF NORTH AMERICA

THOUSANDS OFYEARS AGO

0

MODERNOBSERVATIONS

LAST GLACIALMAXIMUM

20 16 48

YoungerDryas

Demise of LaurentideIce Sheet

Final Drainageof Lake Agassiz

12

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Tree at Chancellorsville

Source: Andy Frasse!o

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Tree-ring display at elementary school

Source: Tom Swetnam

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MUCH MORETHAN JUST

COUNTING TREE RINGS.

DENDROCHRONOLOGY IS

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A. E. Douglass University of Arizona

The trees composing the forest rejoice and lament with its successes and failures and carry year by year something of its story in their annual rings.”“

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Source: Baillie (1982)

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Source: Lane Johnson

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Source: Lane Johnson

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27

St.. George and Nielsen, The Holocene, 2003

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Giant sequoia 3,266 years

Source: Julie Jordan Sco!

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Source: Tom Harlan

Intermountain bristlecone pine 4,844 years

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Source: Ralph Sievert

The Seward Oak 330 years?

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Source: Danny Margoles

Eastern white cedar (in Minnesota) 560 years

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Tree-ring analysis is one of the most powerful tools available for the study of environmental change and the identification of fundamental relationships between tree growth and climate.

“ ”Ed Cook and Neil Pederson

Lamont-Doherty Earth Observatory

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I N T R O D U C T I O N T O D E N D R O C H R O N O L O G Y

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GEOG5839MAJOR TOPICS

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The science of dendrochronology uses information encoded into the annual growth rings of trees to address issues related to climate change, hazards, ecology and natural history.

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September 6

What are tree rings?

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Source: Paul Schulte

September 18

How does weather a#ect tree growth?

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h!p://esp.cr.usgs.gov/data/atlas/li!le/

September 20

The principle of cross-dating

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The Longest Tree-Ring Record In The Americas.

8,500 Years

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October 23

The history of dendrochronology

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October 18

Sampling strategies

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October 16

Dendroarcheology

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Source: Whitney Crawford

November 6

Dendroecology

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Source: Erica Bigio

November 8

Dendrogeomorphology

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GEOG5839LABORATORY ACTIVITIES

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Source: Fritz Schweingruber

Exercise

Tree anatomy

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Exercise(s)

Cross-dating

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Exercise

Signal processing

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GEOG5839ABOUT ME

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GEOG5839COURSE STRUCTURE

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In-class discussion

Project and final report

Laboratory exercises

Final exercise

25%

5%

40%

30%

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GEOG3839NEXT CLASS

Source: Fri!s Schweingruber


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