class 8, past climates and society

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GEOG5426 Past climates, past societies

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Page 1: Class 8, Past Climates and Society

GEOG5426 Past climates, past societies

Page 2: Class 8, Past Climates and Society

By November 3

[Tentative] list of 10 articles related to your region and time period.

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November 24

Brief (15-minute) summaries of project topics.

(1) What are the most important features of the modern climate in your region?

(2) What proxies are available in your region, over the time interval specified? How are they related to climate? and

(3) How different were past climates from modern conditions? Why is that important?

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Scientists are sometimes like American tourists; [we] think that if we just speak English loud enough,

people will understand us.

“Kevin Finneram, editor in chief

Issues in Science and Technology

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Tip #1

Use images, not text

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Hear a piece of information, and three days later you'll remember 10% of it.

Add a picture and you'll remember 65%.”

John Medina

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LOWf re q u e n c y

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Tip #2

Design for the back row

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Make It BIG

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Make It BIG

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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.

Photograph of Lake Winnipeg from Gimli, Manitoba

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St. George et al., The Holocene, 2010

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St. George et al., The Holocene, 2010

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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

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characteristics of D2M ‘hotspots’

Not correlated with major modes

Do not track SST anomalies

Are not synchronized with each other

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Tip #3

Get to the point

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

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MURDERYOURDARLINGS.

“Sir Arthur Quiller-Couch

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“I’m more important that the next speaker.”

“I’m more important than this session.”

“I’m more important than my audience.”

What going over time really means

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Strive for continual improvement

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You must unlearn what you have learned.”“Yoda

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MEGADROUGHTintensity at least equivalent to modern multiyear droughts

duration longer than the several years to decade thereof

Seager et al., Journal of Climate, 2008

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Red River floods

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Red River valley

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

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River diversion

Main channel

Winnipegpopulation: 680,000

Photograph: Greg Brooks

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why are Red River floods so severe?

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why are Red River floods so severe?

geology &climate history!

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Level of Lake Winnipeg (metres)

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We do not think that the country below Fort Garry will ever be flooded again for experience shows clearly that each successive flood has indicated far less depth of the plains that its predecessors – a fact fully accounted by the rapid widening of the river channel.

”Anonymous, 1861

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Brooks (2003) Geomorphology

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how o!en does the Red River flood?

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Stratigraphy and limnology

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Photograph: Greg Brooks

Red RiverManitoba

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2008

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1875

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Photo: Erik Nielsen

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Photo: Erik Nielsen

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67Photo: Erik Nielsen

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Photo: Erik Nielsen

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70St.. George and Nielsen, The Holocene, 2003

Normal growth

Flood damaged

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St. George and Nielsen, The Holocene, 2003

350 years of Red River floods

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The forts now stand like a castle of romance in the midst of an ocean of deep contending currents, the water extending for at least a mile behind them, and they are thereby only approachable by boats and canoes.”

“Francis HeronHudson Bay Company, 1826

St.. George and Rannie, Canadian Water Resources Journal, 2003

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74Winnipeg floodway

expansion

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GEOG5426 Past climates, past societies

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Climate and the collapse of the Mayan CivilizationHaug et al., Science, 2003

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Intertropical Convergence ZoneThe region where the northeasterly and southeasterly

trade winds converge, forming an o"en continuous band of clouds or thunderstorms near the equator.

National Weather Service

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Photo: f-l-e-x

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Photo: Celso Flores

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Photo: npa!erson

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Haug et al., Science, 2003

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Haug et al., Science, 2003

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Aztec drought and “The Curse of One Rabbit”Therrell et al., BMAS, 2004

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Therrell et al., BAMS, 2004

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Therrell et al., BAMS, 2004

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photo: Howard Arno!

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Therrell et al., BAMS, 2004

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Therrell et al., BAMS, 2004

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November 10

Statistics in Paleoclimate