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INTRODUCTION TO DENDROCHRONOLOGY

Class 1, introduction to dendrochronology

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The annual growth rings from trees provide us with an incredibly powerful and adaptable tool to study Earth’s history. The rings tell us much more than just the age of tree. 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.This course will teach students the fundamental principles of dendrochronology through a combination of formal lectures, class discussion and laboratory exercises. Students will work in the University of Minnesota’s Center for Dendrochronology, where they will learn how to collect, prepare and date tree-ring specimens. By the end of the course, they will be able to explain both the key concepts underlying dendrochronology and discuss how evidence from tree rings is used to address contemporary issues in natural history, resource management and Earth Systems Science.

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Page 1: Class 1, introduction to dendrochronology

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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2010 Dec-Nov temperature anomaly h"p://www.giss.nasa.gov/

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NASA global temperature record h"p://www.giss.nasa.gov/

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QUESTIONIs it unusual for the world to be this warm?

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Water transfers in the American southwest

Courtesy Glen MacDonald

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Low reservoir

Photograph: 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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Photograph: Greg Brooks

Red RiverManitoba

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AP Photo/U.S. Coast Guard, Lt. Brendan Evans

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QUESTIONHow often does the Red River

produce extreme floods?

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Tree at Chancellorsville

Photograph: Andy Frasse!o

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Tree-ring display at elementary school

Photograph: Tom Swetnam

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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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Same environmental conditions

Similar growth pa"erns

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25

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1900 1910 1920 1930

Two Douglas-fir cores from Eldorado Canyon, CO

Graphic: Jeff Lukas, INSTAAR

THE PRINCIPLE OF CROSS-DATING

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Photo: Howard ArnottFrost damage Photograph: Howard Arno!

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Fire scars

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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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Photo: Chris MullinsGiant sequoia 3,266 years Photograph: Chris Mullins

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Bristlecone pine 4,844 years Photograph: Tom Harlan

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White pine 1714

Photo: Kurt Kipfmueller

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Photo: Danny Margoles

White cedar 1452

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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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Fundamentals Tree-ring anatomy Photograph: Kevin Anchukaitis

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Fundamentals Weather, climate and tree growth Photograph: dr_tim_1956

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Fundamentals History of dendrochronology

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Fundamentals Statistical tools for tree-ring analysis

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Applications Drought risks Photograph: Library of Congress

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Applications Fire ecology Photograph: Don Falk

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Applications Natural hazards and landscape processes Photograph: Erica Bigio

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Applications Forest ecology Photograph: Whitney Crawford

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43Applications Maritime archeology

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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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Who am I?

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Tree-ring display at elementary school

Photograph: Tom Swetnam

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Photo: Calvin Ferris Kurt Kipfmueller University of Minnesota

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umndendro.umn.edu

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GEOG3839 Nuts and boltsGEOG5839

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Links to course syllabus, scheduleat h!p://umn.edu/~stgeorge under ‘Teaching’

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GEOG3839

Mid-term

Exercises (4)

Final exam

30%

40%

30% GEOG5839

Mid-term

Exercises (4)

Project

20%

40%

40%

G R A D I N G W E I G H T S

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Trees are among the oldest living things on our planet. Many trees can live for several centuries and a few exceptional specimens have survived for more than 5,000 years. In part because of their great age, the annual growth rings from trees provide us with an incredibly powerful and adaptable tool to study Earth’s history. The 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.

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. Because tree vitality is strongly influenced by local environmental conditions, major events such as a change in climate, insect a!ack or severe flood o"en create a distinct ‘fingerprint’ in the tree’s rings. By studying these signatures in the rings, we can develop an annual record of past environmental events extending back several centuries or millennia.

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Links to course syllabus, scheduleat h!p://umn.edu/~stgeorge under ‘Teaching’

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Readings!Smith and Lewis (2006), Dendrochronology

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What can you expect to learn?

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DENDROCHRONOLOGY is much more than just counting tree rings