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Projection of Global Climate Change

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Page 1: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Projection of Global Climate Change

Page 2: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Review of last lecture

• Rapid increase of greenhouse gases (CO2, CH4, N2O) since 1750: far exceed pre-industrial values determined from ice core measurements spanning the last 650,000 years. Lead to strong radiative heating.

• Mainly caused by CO2 fossil fuel use.

• The developed countries and developing countries contribute almost equally to the emissions of GHGs.

• Observed change of mean: air temperature, ocean temperature, melting of arctic sea ice, Greenland ice sheet, snow and glaciers, rising of sea level.

• Observed change of extreme events: extreme precipitation events, heat waves, strongest hurricanes

Page 3: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

The most common atmospheric circulation structure

L

H

H

L

HeatingCoolingor No Heating

Imbalance of heating Imbalance of temperature Imbalance of pressure Wind

Radiation Convection Conduction

Latent/Sensible

BiosphereLand/Ocean/Ice/

Stratosphere Feedback

Greenhouse Gases

Pollution

Clouds Precipitation (Latent heat)

Page 4: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Coupler .

Land

Sea Ice

Atmosphere

Ocean

Framework of Earth System Model

Biogeochemistry

• Include 5 components: atmosphere, ocean, land, sea ice, biogeochemistry• Based on the conservation laws of mass, energy, momentum, water vapor and other

chemical species (e.g. CO2, CH4)• Based on future assumptions of external forcing (GHG concentrations, solar

variability, pollution, land use changes)

Page 5: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Can the GCMs Reproduce the 20th Century Temperature Trend?

The GCMs can reproduce the 20th century temperature trend

The warming is caused by anthropogenic forcings!

Page 6: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Simulations for Different Regions: Warming is caused by anthropogenic forcings

Page 7: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Our choice of the future: Emission scenarios

Page 8: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Projected Change in Global Mean Temperature

Page 9: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Global map of projected change Temperature: Largest warming over Arctic, larger over land

Precipitation: Increase in tropics/poles, decrease in mid-latitudes

Page 10: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Video: Six Degrees Could Change the World

• https://www.youtube.com/watch?v=R_pb1G2wIoA

(Carbon footprint 20:00-)

Page 11: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Number of Days over

100 oF

Page 12: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Vertical Structure of Projected Warming (Averaged over each latitude)

Atmosphere:

Tropical amplification (Glaciers, disease, …)

Polar amplification (Ice, sea level)

Ocean: Large warming goes down to ~1000 m (ecosystems)

Page 13: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Projected change of sea ice and ocean

Page 14: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Projected Change in Global Sea Level

Page 15: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Other examples: • Nile Delta – 1m rise affects 6,000,000 people• Florida, Louisiana - population centers, wetlands, tourism

1.5m rise expected 150 years from now(United Nations Environmental Program)

Page 16: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

New York City under a 3-5m sea level rise

Page 17: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Projected Change in Precipitation: Increase in tropics and high latitudes, decrease in

mid-latitudes

Page 18: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Impacts on fresh water

Page 19: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Impacts on ecosystems

4.0 oC

3.0 oC

Poison ivy loves CO2

Page 20: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Attribution of Projected Temperature Change: Mainly caused by anthropogenic forcings

Page 21: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Summary

• Global climate models: Earth system models (5 components)• Global climate models can reproduce the observed warming

in the 20th century. The warming is largely caused by human activities.

• Projected change: mean temperature (largest warming over Arctic, larger over land), mean precipitation, sea level, extreme temperature, extreme precipitation, fresh water, ecosystems

• Future climate scenarios show that reducing greenhouse gas emissions can substantially mitigate warming in the latter half of this century.

Page 22: Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial

Work cited• http

://intercongreen.com/2010/03/15/green-building-ebbs-slightly-in-recession-but-sentiment-remains-strong/

• http://nimbuseco.com/2013/01/deforestation-and-pollution-facts/ • http://greenbalkans.org/category.php?language=en_EN&cat_id=63 • http://www.nrcs.usda.gov/wps/portal/nrcs/detail/ia/newsroom/releases/?cid=

nrcs142p2_011847 • http://www.csiro.au/en/Portals/Multimedia/On-the-record/Megan-Clark-presentation-2

0090526-generating-industries/Post-Combustion-Carbon-Capture.aspx

• http://economistsview.typepad.com/economistsview/2005/09/the_consumer_dr.html • http://nca2009.globalchange.gov/human-health • http://yosemite.epa.gov/ee/epa/eerm.nsf/vwAN/EE-0564-112.pdf/$file/EE-0564-

112.pdf • http://livinggreenmag.com/2012/06/13/climate-change/scientists-warn-that-earth-is-

close-to-climate-tipping-point/ • http://www.cnn.com/2013/05/29/opinion/mystreet-digital-anthropology/ • http://commons.wikimedia.org/wiki/File:World-airline-routemap-2009.png