Lecture 24: Survey of the Last Glacial Maximum Part IV, p. 205-206; Chapter 12 (p. 209-224)

Lecture 24: Survey of the Last Glacial Lecture 24: Survey of the Last Glacial MaximumMaximum

Part IV, p. 205-206; Chapter 12 (p. 209-

224)

(21 k yrs ago)

• Continental ice sheets greater than 3 km (1.8 miles) thick covered parts of North America and Eurasia

• Sea ice around Antarctica and in the North Atlantic was considerably more extensive

CN Tower, Toronto, Canada

Survey of The Last Glacial Maximum Ch. 12, p. 209-224

Differences between LGM and Today

The Bering Land Bridge

1. Land-sea configurationglacial ice high albedosmaller oceans for transferring heat

2. Insolation is similar to today

• Ice covered ~25% of modern land area (about half of North America)

• Temperature ~ 4-8°C lower than today• Sea level 120 m (or 400 ft) lower than today• Windier; dustier; Strong overturning; restricted

fauna/flora• CO2 = 180 ppmv now 381 ppmv (in

2006)• CH4 = 350 ppbv now 1751 ppbv (in 2006)• N2O = 185 ppbv now 310 ppbv

Cordilleran Ice Cheet

Laurentide Ice Sheet

The North American ice sheet was the largest of the N.H. ice sheets.

Scandinavian Ice Sheet

Permafrost

Regions of Northern Hemisphere Ice Sheets

The lateral extent of the ice sheets?

The northern limits?

The thickness of the ice sheets?

Thick?

How Large Were the Ice Sheets?

Thin?

Glaciers Transform Landscape

Norway (near Jostedalsbreen glacier)

Glaciers abrade rocks!

Glaciers make U-shape valleys!

Mount Hood Wilderness

Bhutan Himalaya

Glaciers form lakes!

Glaciers Transform Landscape

Grind / scrape / dislodge

Freeze-thaw process

Carry toward margins

Ice sheets erode land!

Ice sheets are prolific producers of debris in all sizes.

Winds carry deposits downwind.

Glaciers Transform Landscape

Ice sheets erode land!

Pollen Percentages and Climate on the Continents

Prairie grasses and herbs are most abundant where rainfall is low.

Tree pollen is more common in wetter eastern regions.

Spruce trees are common in the colder north, oak in the warmer south.

Glacial and Present-day Climate in SW USA

Today the southwester US is dry!

At the LGM, the southwest was wetter.

because of the southward displacement of the jet stream brought increased rain and cloud.

Glacial and Present-day Climate in Europe

Europe was completely transformed during LGM.

Today: extensive forest covers (conifer and deciduous)

LGM: mostly tundra and grass-covered steppes, with Scandinavian ice sheet in the north and forests scattered in the south

Glacial Climate in Asia

Glacial and Present-day Biomes

Present-day Tree Cover

LGM Tree Cover

The Earth’s Climate History1. Over the last century, the earth’s surface temperature has increased by

about 0.75°C (about 1.35°F).

2. Little Ice Age = 1350 A.D. – 1850 A.D. (N.H. temperature was lower by 0.5°C, alpine glaciers increased; few sunspots, low solar output)

3. Medieval Warm Period = 950 A.D. – 1,250 A.D. (N.H. warm and dry, Vikings colonized Iceland & Greenland)

4. Holocene Maximum = 5,000-6,000 ybp (1°C warmer than now, warmest of the current interglacial period)

5. Younger-Dryas Event = 11,000 ybp (sudden drop in temperature and portions of N.H. reverted back to glacial conditions)

6. Last Glacial Maximum = 18,000 ybp (maximum North American continental glaciers, lower sea level exposed Bering land bridge allowing human migration from Asia to North America)

7. We are presently living in a long-term Icehouse climate period, which is comprised of shorter-term glacial (e.g., 18,000 ybp) and interglacial (e.g., today) periods. There were four periods of Icehouse prior to the current one.

8. For most of the earth’s history, the climate was much warmer than today.