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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
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)
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
Global map of temperature change: Largest warming in Arctic (“Arctic amplification”)
Larger warming over land than ocean
Projected Change in Global Temperature: Significant warming
The spread comes from uncertainties in climate feedbacks
Main climate feedbacks for global warming
• Ice albedo• Lapse rate (temperature)• Water vapor • Cloud• Aerosol• Carbon cycle
Lapse rate feedback
Surface
Tropopause
Surface warming
Same lapse rate
Larger Longwave flux
Warming of whole troposphere
Cooling down of surface temperature
Video: Carbon Cycle
• http://www.youtube.com/watch?feature=player_detailpage&v=U3SZKJVKRxQ
Abrupt climate change and history/politics- Collapse of Maya civilization and Chinese
ancient dynasties
Droughts
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
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/
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