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Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

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Page 1: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Global warming andSea Level Rise:

Best estimates by 2100

John KingProfessor of Oceanography

Page 2: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Global Warming:What is it?

• The increase in the measured temperature of the earth’s oceans and near-surface air.

Page 3: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Measured temperature increases since 1860

Global annually averaged surface temperatures, based on NASA GISS surface temperature analysis

Page 4: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Global Warming:What’s causing it?

• The increase of these gases causes “The Greenhouse Effect.”

• Human activities add CO2 and other gases to the atmosphere.

Page 5: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Sun’s energy passes through the atmosphere, warming the earth.

Some of the energy is reflected back into space.

Greenhouse gases in the atmosphere trap some of the heat. More gases = more heat.

The Greenhouse Effect

Page 6: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Indicators of human influence on the atmosphere

Page 7: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Changes in Temperature, Sea Level and Northern Hemisphere Snow Cover

Courtesy of IPCC, 2007

Page 8: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Global Warming:Why does it matter?

Global warming causes climate changes that will affect:

• natural ecosystems

• availability of food and water

• global economies

• frequency of extreme weather

events

• human health and lifestyle

Page 9: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Increased CO2 emissions = climate change

Rising Temperatures

Changes in Precipitation

Rising Sea Level

Increasing CO2

Page 10: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Global effects of climate change and sea level rise

Page 11: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Effects of Global Warming:Rising temperatures

Page 12: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Rhode Island climate “migration”

Courtesy of the Union of Concerned Scientists

Page 13: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Rising Temperatures

Courtesy of the Union of Concerned Scientists

Page 14: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Global and Continental Temperature Change

Courtesy of IPCC, 2007

Page 15: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Changes in annual average temperature in the Northeast

Page 16: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Effects of Global Warming:Rising sea level

Page 17: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography
Page 18: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Four contributions to sea level rise

1. Thermal expansion of seawater

2. Melting of glaciers and ice caps

3. Ice sheet surface mass balance• snowfall - melting

4. Ice sheet surface dynamical imbalance

• increased flow rate

Page 19: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Projected globally averaged surface warming &sea level rise at the end of the 21st century

Courtesy of IPCC, 2007

Page 20: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Sea Level Rise: Observed vs. Projected

Interval Model Prediction Observed

mm/year

1993 - 2003 2.6 3.1

1961 - 2003 1.2 1.8

mm/year

Page 21: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Sea Level Rise: Observed = Projected

observed

projected

Page 22: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

2007 - IPCC sea level rise estimate

1. Thermal expansion of seawater .......... 28 cm

2. Glaciers and ice caps ......................... 12 cm

3. Mass balance ..................................... - 3 cm

4. Increased flow ................................... + 3 cm

Total: 40 cm

Range of Estimates: 18-59 cm

Page 23: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

ReferenceBy 2100

(feet)Total Rise

(feet)Overpeck,et al., 2006 > 3 13 - 20

Rahmsorf,2007

1.6 - 4.6

- - -

Pfeffer,et al., 2008

2.6 - 6.6

- - -

Sea Level Rise: New Estimates

Page 24: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Reference Additions to global rise predictions

Yin,et al., 2009 + 8 inches

Hu,et al., 2009

+ 12 - 20inches

Total global +regional

2.3 - 8.3feet

Increased sea level rise estimates for New England

Page 25: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Greenhouse Gases in Ice Cores

From Brook, E. J., 2005. Science , 25 vol. 310. no. 5752, pp. 1285 - 1287

Present day

Page 26: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

What does 3 feet of sea level rise look like?

Page 27: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Effects of Global Warming:Rising sea level in Rhode Island

Page 28: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Quonochontaug Pond 5’ sea level rise:Model by Nathan Vinhateiro, GSO-URI

Flooded areas shown with light blue shading

Page 29: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Quonochontaug Pond 5’ sea level rise detail:Model by Nathan Vinhateiro, GSO-URI

Flooded areas shown with light blue shading

Page 30: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Quonochontaug Pond 5’ sea level rise detail:Model by Nathan Vinhateiro, GSO-URI

Flooded areas shown with light blue shading

Page 31: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Planning Needs for Rhode Island

1. Seamless digital terrain model LIDAR survey of coastline High-resolution bathymetry of coastal

waters

2. Inundation model Storm surge with wave regime

superimposed Better understanding of coastal erosion

style and rate Expanded Rhode Island sea level and

coastal erosion monitoring program

Page 32: Global warming and Sea Level Rise: Best estimates by 2100 John King Professor of Oceanography

Possible explanation for why human-induced global warming is still “controversial”