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Climate feedbacks for global warming
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Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Dec 13, 2015

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Page 1: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Climate feedbacks for global warming

Page 2: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Review of last lecture

• Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the Walker circulation? Two types of ocean upwelling

• Mean state: ocean-atmosphere feedback

• ENSO: Which region has warm SST anomaly during El Nino? 4-year period.

• Existing ENSO theories

• AMO and thermohaline circulation

Page 3: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Global connections

Page 4: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

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 5: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

How do human activities change the global climate?

Human beings are changing the global climate system in three different ways:

• Change land cover (deforestation and afforestation)• Release or cleanse pollutants (aerosols)• Release or cleanse greenhouse gases

Page 6: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Observed Change in Global Temperature: Significant warming

Page 7: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Global map of temperature change: Largest warming in Arctic (“Arctic amplification”)

Larger warming over land than ocean

Page 8: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Projected Change in Global Temperature: Significant warming

Page 9: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Projected Change in Global Temperature: Significant warming

The spread comes from uncertainties in climate feedbacks

Page 10: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Main climate feedbacks for global warming

• Ice albedo• Lapse rate (temperature)• Water vapor • Cloud• Aerosol• Carbon cycle

Page 11: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Ice albedo feedback

Page 12: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Lapse rate feedback

Surface

Tropopause

Surface warming

Same lapse rate

Larger Longwave flux

Warming of whole troposphere

Cooling down of surface temperature

Page 13: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Water vapor feedback

Page 14: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Cloud feedback

Strongerwarming effect

Stronger cooling effect

Page 15: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Aerosol feedback

Page 16: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Video: Carbon Cycle

• http://www.youtube.com/watch?feature=player_detailpage&v=U3SZKJVKRxQ

Page 17: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Global carbon cycle

Page 18: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Carbon cycle feedback

Page 19: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Carbon cycle feedback Example 1: Permafrost thaw

Page 20: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Carbon cycle feedback Example 2: Biosphere

Page 21: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Carbon cycle feedback sources

Page 22: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Feedback strength in climate models

Water vapor Cloud Albedo Lapse rate

Page 23: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Projected Change in Global Mean Temperature

Page 24: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Abrupt climate change and tipping point– Lesson from Earth’s climate history

Page 25: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Termination of the Younger Dryas cold event and last ice age 11,600 years ago

Page 26: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Abrupt climate change and history/politics- Collapse of Maya civilization and Chinese

ancient dynasties

Droughts

Page 27: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Bifurcation and tipping point

Page 28: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Examples of tipping points

Page 29: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Interactions among tipping points

Page 30: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Summary

• Large spread in projected temperature change comes from uncertainties in climate feedbacks

• Main climate feedbacks for global warming: albedo, lapse rate, water vapor, cloud, aerosol, carbon cycle

• Feedback strength in climate models: cloud feedback causes the largest uncertainty

• Past abrupt climate change

• Tipping points

• Future abrupt climate change

Page 31: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Works cited• http://www.jpl.nasa.gov/images/earth/20100325/atlantic20100325-full

.jpg

• http://www.nasa.gov/centers/goddard/news/topstory/2004/0315humidity.html

• http://sitemaker.umich.edu/section2_group1/arctic_issues__permafrost

• http://www.all-creatures.org/hope/gw/02_Arctic-Antarctic.htm

• http://www.fedre.org/en/content/global-permafrost-zones-high-resolution-images-google-earth

• http://www.onlyzerocarbon.org/arctic_feedback.html

• https://www.marietta.edu/~biol/biomes/tropdry.htm

• http://www.nwf.org/Wildlife/Threats-to-Wildlife/Global-Warming/Global-Warming-is-Causing-Extreme-Weather/Wildfires.aspx

• http://www.opb.org/news/blog/ecotrope/qa-how-to-reduce-wildfire-severity-even-in-a-warmer-climate/

Page 32: Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.

Work cited• http://www.ncdc.noaa.gov/paleo/ctl/abrupt.html

• 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-20090526-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