Black Carbon.

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Presentation transcript:

Black Carbon

Different Forms of Elements Elements are always pure, but do not always look the same Example: carbon diamond graphite

Forms of carbon, cont. BLACK CARBON carbon nanotubes

What is carbon? An element (number 6) 6 protons Sixth-most abundant element in the universe Typical forms Soot Graphite Diamond Fullerenes Essential for life Has 15 isotopes (varieties) Approximately ten million compounds contain carbon Common compounds Carbon dioxide - CO2 Methane - CH4 Vinegar - CH3COOH

What is black carbon? A product from incomplete combustion (burning) Soot Particles thousands of times smaller than the width of a human hair Can travel long distances on air currents Falls out of the air in 7-10 days due to rain, etc “Short-lived climate forcing” Causes warming

Where does black carbon come from? Top producers East Asia South America Western Africa Top sector (area/branch) Biomass burning Residential – biofuel Transport - road

Where is black carbon? A) Global distribution of black carbon emissions (tons/year) B) Estimated global radiative forcing due to black carbon (W/m2)

Why should we care about black carbon? Contributes to climate change (warming) in two ways Absorbing sunlight and heating air around it Falling on snow or ice, decreasing reflectivity, and increasing melting BC absorbs heat a million times more than CO2 Contributes to regional heating Disrupts rainfall patterns Reducing black carbon output could slow warming by 0.1 – 0.2 oC ENVIRONMENT

Why should we care about black carbon? Reductions would prevent 2.4 million premature deaths worldwide Particulate emissions from diesel exhaust (major source of BC) are linked to lung and heart disease, as well as cancer HEALTH

Feedback Loops Positive Feedback Negative Feedback Reaction enhances original stimulus “Runaway effect” Promotes instability and change Negative Feedback Reaction negates original stimulus Whether too high, or too low, negative feedback brings it back to a set point Promotes stability and constancy

Albedo and Arctic Climate  Which snow will melt faster? Why?  What is going to happen in this situation?

Albedo

Albedo Low albedo High albedo Albedo: the fraction of incoming radiation (light) that is reflected by a surface Scale from 0 – 1 (0% - 100%) Low albedo High albedo Reflects sunlight well Absorbs sunlight well Ice Forests Snow Oceans Sand Soil

Arctic Sea Ice What happens to incoming sunlight in each case? What does this mean in terms of the snow-albedo feedback loop?

Snow-Albedo Feedback Loop these loops show the same type of change (positive feedback) in two different ways

Black Carbon in the Arctic Black carbon falls on snow and ice  Albedo decreases More sunlight is absorbed Melting increases Is this a positive or negative feedback loop?

Summary

What can be done? Replace traditional cook and heat stoves in developing countries with clean-burning biomass stoves or alternate energy sources Install filters on diesel vehicles Create tighter restrictions on diesel vehicles Eliminate open field burning of agricultural waste

How well do changes work? Rate of decline = 1 – 13 = .33 g BC/kg diesel 2003 – 1967 per year Regulations were implemented in California to reduce emissions The black dots are the average black carbon emission over time

Sources http://education.jlab.org/itselemental/ele006.html http://education.jlab.org/itselemental/iso006.html http://www.nature.com/ngeo/journal/v1/n4/pdf/ngeo156.pdf http://online.santarosa.edu/homepage/cgalt/BIO10-Stuff/Ch21- Animal_Structure_Function/Feedback-Loops-Summary.jpg http://www.mcclatchydc.com/2011/05/05/113755/scientists-measure- arctic-soot.html http://www.eoearth.org/article/Black_Carbon_and_Climate_Change?t opic=49491 http://www.skepticalscience.com/soot-and-global-warming.html http://ac.els-cdn.com/S1352231007008631/1-s2.0-S1352231007008631- main.pdf?_tid=ad6773f6b4dda3b1ca25ed539b4c9465&acdnat=13425479 70_8c20062180cef755b59ded99f8e8a1ab

Image Sources http://blog.iqsdirectory.com/wp-content/uploads/files/graphite%204.jpg https://www.e-education.psu.edu/earth520/files/earth520/pencils_diamonds.jpg http://www.a1-diamond.com/ http://www.nap.edu/books/12951/xhtml/images/p2001c7c7g77001.jpg http://www.grc.nasa.gov/WWW/RT/RT2001/images/5410hepp1-f1.jpg http://www.climate.org/programs/images/smokestack.JPG http://www.dnr.state.md.us/education/envirothon/2004art/snow.jpg http://earthobservatory.nasa.gov/Features/SeaIce/images/sea_ice_polar_bear.jpg http://epa.gov/climatechange/images/indicator_figures/sea-ice-figure2.gif http://www.climate-emergency-institute.org/uploads/Arctic_albedo_1.png http://foreignpolicyblogs.com/wp-content/uploads/ice-albedo-feedback-process.jpg http://www.yesmagazine.org/images/issues/88/45Pandora_LoopIceTEXT.jpg http://www.talkingscience.org/wp-content/uploads/2010/09/WOE_150Albedo.gif http://www.nature.com/ngeo/journal/v1/n4/pdf/ngeo156.pdf http://politicalclimate.files.wordpress.com/2010/07/feedbacks-schematic.png?w=460 http://ipy.no/imagearchive/stort_hovedtekstbilde_greenland_402_None_full.jpg http://media.mcclatchydc.com/smedia/2011/05/06/22/20110506_ARCTICSOOT.large.prod_affiliate.91.jpg http://www.neptuneproducts.co.nz/site/rosmac/files/images/Environment/TruckSmoke109_1_1.jpg http://kpbs.media.clients.ellingtoncms.com/img/photos/2012/01/17/wood_stove_t614.jpeg?a3ca5463f16dc11451266bb717d38a6025dcea0e http://www.nasa.gov/images/content/159505main_biomass_burn_lg.jpg http://extras.mnginteractive.com/live/media/site36/2011/0415/20110415__EMISSIONS~p1.jpg http://2.bp.blogspot.com/-uJ_RbBOYMdE/T5XITZy_zAI/AAAAAAAAAdA/RQoCNc4e3To/s1600/Fire_-_Soot_on_a_Hand%5B1%5D.jpg http://3.bp.blogspot.com/_C5cFhlHoXiU/SgmoroodRmI/AAAAAAAAAVI/wdmfrqCbm3A/s400/soot.JPG http://news.stanford.edu/news/2010/july/images/soot_news.jpg http://c1ecolocalizercom.wpengine.netdna-cdn.com/files/2012/06/chicago-soot-swanksalot.jpg http://ac.els-cdn.com/S1352231007008631/1-s2.0-S1352231007008631-main.pdf?_tid=ad6773f6b4dda3b1ca25ed539b4c9465&acdnat=1342547970_8c20062180cef755b59ded99f8e8a1ab