five things you can do right now to make your presentation a little bit better

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I used these slides as part of a webinar aimed at improving presentations at scientific conferences and workshops. I'll post a link to the video once it's available! _______________ The ability to deliver effective and engaging oral presentations is a critical skill for scientists in all disciplines. Unfortunately, despite the importance of clear communication, too many presentations at conferences and workshops are confusing, abstract and boring. In this seminar, Scott St. George (University of Minnesota) and Andy Frassetto (Incorporated Research Institutions for Seismology) will share a few tips that could make your professional presentations just a little bit better. In less than 30 minutes, Scott and Andy will talk s presentation planning, the differences between a good and bad visual aid, and point you towards several outstanding online resources. Become a presentation superstar!

TRANSCRIPT

Five things you can do right now to make your presentations a li!le bit be!er.

Sco! St. George, University of Minnesota

16 JANUARY 2003

Source: NASA

Source: NASA

... it is easy to understand how a senior manager might read this PowerPoint slide and not realize that it addresses a life-threatening situation. “ ”

Columbia Accident Investigation BoardAugust 2003

THIRTY MILLION

ACCORDING TO MICROSOFT, AT LEAST

POWERPOINT PRESENTATIONS ARE MADE EVERY DAY.

Source: Ian Parker, The New Yorker, May 28, 2001

THE USE OF THE POWERPOINT PRESENTATION HAS BEEN A DISASTER.

Prof. John SwellerUniversity of New South Wales

IT SHOULD BE DITCHED.“ ”

??

? ?

5THINGS YOU CAN DO RIGHT NOW TO MAKE YOUR PRESENTATIONS A LITTLE BIT BETTER

?Someone just asked you

to deliver a presentation.

DO FIRST?WHAT DO YOU

We don’t know where we get our ideas from. We do know that we do not get them from our laptops.“ ”

John Cleese

TIP ONEUnplug.

Source: Kurt Groetsch

TIP TWOMove your notes off-screen

Concluding Remarks

• Slow-axis anisotropy trends approximately NE-SW at the base of the crust.

• These findings are consistent with model for C-S fabric imparted by bottom to the SW shear

• Receiver functions show trademark signs of significant crustal anisotropy adjacent to the Central Sierra Nevada.

• Does lithosphere-scale deformation and removal leave an imprint on the crust? Can we detect these “delamination scars”?

Yes

“ ”WORDSWORDSWORDS

HamletAct 2, Scene 2

.

?What is the average reading speed for a literate adult (words per minute?)

Anatomical signatures from riparian trees can be used to extend flood records by several hundred years.

Flood hazards and tree rings

In the Red River basin, shifts in annual precipitation of roughly ten percent altered flood risks significantly during the last 350 years. Geological processes are not affecting flood hazards at relevant timescales.

The current design flood for the Red River valley was produced by an exceptional combination of extensive flooding in the northeastern Great Plains and unusual spring weather across central North America.

Paleoflood Records for the

Red River, Manitoba, Canada

Pictures beat text... because reading is so ine!cient for us. We have to identify certain features in the le"ers to be able to read them. That takes time.“ ”

Dr. John MedinaBrain Rules

Source: Amy Luxbacher

Source: Amy Luxbacher

3Do climate-sensitive trees (and other proxies) transform climate signals in predictable ways?

TIP THREEDesign for the back row.

“ ”I KNOW YOU

BUT...CAN’T SEE THIS,

MAKE IT BIG

MAKE IT BIG

Lake Winnipeg, Manitoba, Canada• Lake Winnipeg is the 11th largest

freshwater lake in the world

• The lake’s watershed includes territory in Alberta, Saskatchewan, Manitoba, Ontario, Minnesota and North Dakota

• Its tributaries include the Saskatchewan, Red, Winnipeg and Assiniboine Rivers.

• The lake drains northward into the Nelson River and contributes to Hudson Bay.

Drowned stumps along the foreshore of Lake Winnipeg

April 10, 2013IRIS Presentation Webinar

Depth StacksA) BR low elevations

B) BR core complexes (high elevation, highly deformed)

C) ATZ/CP (high elevation, mostly undeformed)

D) Volcanic fields (high elevation, recent activity)

Major changes in crust, upper mantle seismic character from BR to CP

A Live View

TIP FOURBe design-ful

0

2500

5000

7500

10000

Texa

s

Iow

a

Cali

forn

ia

Was

hing

ton

Min

neso

ta

Ore

gon

Illin

ois

New

York

Col

orad

o

Nor

th D

akot

a

1,2031,2441,2741,5571,7581,8101,8492,798

3,604

9,403

Win

d en

ergy

cap

acit

y (M

W)

State

Installed wind capacity in the United States

IRIS Presentation Webinar, April 10, 2013

Source: American Wind Energy Association

0

2,500

5,000

7,500

10,000

Texas Iowa California Washington Minnesota Oregon Illinois New York Colorado North Dakota

Installed wind capacity (megawa!s)

really decadalnot that

decadal

St. George and Ault, Journal of Geophysical Research - Atmospheres, 2011

FONTSWHICH

SHOULD YOU

CHOOSE?

I hear Comic Sans

is a classy font.

?When should you use Comic Sans?

Never never never never never never nevernever never never never never never nevernever never never never never never nevernever never never never never never nevernever never never never never never nevernever never never never never never nevernever never never never never never nevernever never never never never never nevernever never never never use Comic Sans.

Hel

THROUGH THE TREESTHE STORY OF PRAIRIE DROUGHT TOLD BY TREE RINGS

http://www.usbr.gov/lc/region/g4000/NaturalFlow/current.html

0

12,500,000

25,000,000

37,500,000

50,000,000

1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000

Population Growth of Colorado River Basin 1900-2000

CaliforniaOther 6 Basin States Combined

Population

Golf course in Las Vegas photo: K.Dewey, High Plains Climate Center

Low flow conditions since 2000 have coincided with increased consumption from a rapidly growing population and new demands for water for ecosystem health and recreation. Increases in consumptive use are projected to continue.

Slides are free!

SIMPLICITY IS THE

ULTIMATE SOPHISTICATION

“ ”Leonardo da Vinci

TIP FIVEGet to the point

?How long can you expect to keep your audience’s attention?

The secret of being a bore is to tell everything.“Voltaire

YOUR PROCESS OF DISCOVERY!DON’T DRAG ME THROUGH

In rock music, you have to burn from the first bar.“ ”Sting

??

? ?

You must unlearn what you have learned.Yoda

“ ”

Plan your talk on paper first.

Move your notes o# the screen.

Create visual aids that work for the back row.

Be mindful of basic design principles.

Get to the point.

5THINGS YOU CAN DO RIGHT NOW TO MAKE YOUR PRESENTATIONS A LITTLE BIT BETTER

David Montgomery University of Washington

The A!of Scientific Presentationspractical lessons for talking to your peers and the public

h"p://umn.edu/~stgeorge

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