GEOG5839.01. Introduction to Dendrochronology

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Tree rings tell us much more than just a tree’s age. They also provide clues that help us understand how our environment has changed in the past, and provide insights into how key processes in atmosphere, biosphere and geological systems operate over long timescales.

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GEOG5839CHRONOLOGY

INTRODUCTION TO

DENDRO

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

QUESTIONIs it unusual for the world to be this warm?

Low reservoir

Source: Glen MacDonald

QUESTIONIs there enough water in the Colorado River

to satisfy the expected need?

QUESTIONWhen were these dwellings constructed

(and abandoned)and why?

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

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

QUESTIONHow often do natural hazards like floods occur,

and what factors make them more or less likely?

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

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

Dr. Balaji Rajagopalan University of Colorado

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

Tree at Chancellorsville

Source: Andy Frasse!o

Tree-ring display at elementary school

Source: Tom Swetnam

MUCH MORETHAN JUST

COUNTING TREE RINGS.

DENDROCHRONOLOGY IS

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.”“

Source: Baillie (1982)

Source: Lane Johnson

Source: Lane Johnson

27

St.. George and Nielsen, The Holocene, 2003

Giant sequoia 3,266 years

Source: Julie Jordan Sco!

Source: Tom Harlan

Intermountain bristlecone pine 4,844 years

Source: Ralph Sievert

The Seward Oak 330 years?

Source: Danny Margoles

Eastern white cedar (in Minnesota) 560 years

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

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

GEOG5839MAJOR TOPICS

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.

September 6

What are tree rings?

Source: Paul Schulte

September 18

How does weather a#ect tree growth?

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

September 20

The principle of cross-dating

The Longest Tree-Ring Record In The Americas.

8,500 Years

October 23

The history of dendrochronology

October 18

Sampling strategies

October 16

Dendroarcheology

Source: Whitney Crawford

November 6

Dendroecology

Source: Erica Bigio

November 8

Dendrogeomorphology

GEOG5839LABORATORY ACTIVITIES

Source: Fritz Schweingruber

Exercise

Tree anatomy

Exercise(s)

Cross-dating

Exercise

Signal processing

GEOG5839ABOUT ME

GEOG5839COURSE STRUCTURE

In-class discussion

Project and final report

Laboratory exercises

Final exercise

25%

5%

40%

30%

GEOG3839NEXT CLASS

Source: Fri!s Schweingruber

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