Climate Science 101: Warmer Things. Meghana Ranganathan and Ellen Lalk

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Transcription:

Climate Science 101: Warmer Things Meghana Ranganathan and Ellen Lalk

Research: methane production by microbes kilometers below the ocean floor Introductions: Ellen Lalk 1st year PhD student in Chemical Oceanography Rémi Bigonneau Penguin enthusiast Previously studied Chemistry and Archaeology at WUSTL

Past Research: evaluating ENSO forecasts at Columbia/IRI Introductions: Meghana Ranganathan 1st Year PhD Student in Atmospheric Science Current research: using neural networks and machine learning to quantify climate uncertainty Images: http://insideclimatenews.org/sites/default/files/styles/icn_full_wrap_wide/public/climate%20chart_0. png?itok=gqft5alq https://iri.columbia.edu/wp-content/uploads/2017/12/figure4-1.gif https://blog.wdtinc.com/hubfs/blog-files/elnino-vs-lanina-noaa.jpg?t=1513787240214

Topic Overview 1. What is climate 2. What Affects Earth s Temperature 3. A Look Into Past Climate 4. Environmental Changes from Climate Change

Definitions 1. Weather: Things like precipitation, wind, and humidity that we experience at a given time in a specific location 2. Climate: average weather over a long period of time for a given region; the statistics of weather 3. Climate Variability: natural variation in climate that occurs over months or decades 4. Climate Change: a systematic change in long term state over multiple decades Credit: NASA

The Climate System: Overview Image from: http://www.atmosedu.com/geol390/figures/figure%2001-05-bottom.jpg

Sun: What Factors Affect Earth s Temperature? Images: https://static.pexels.co m/photos/2422/skyearth-galaxyuniverse.jpg https://www.nasa.gov/ sites/default/files/thum bnails/image/pia0027 1.jpg

Factor 1: Insolation Image: https://bam.files.bbci.co.uk/bam/live/content/znyjtfr/large http://easyscienceforkids.com/wp-content/uploads/2013/06/elliptical-orbits.jpg

Factor 2: Albedo Images: https://pmdvod.nationalgeographic.com/ng_video/11/923/150827-nasa-mapping-greenland-icesheet-vin.jpg https://www.nasa.gov/sites/default/files/thumbnails/image/pia00271.jpg

Factor 3: Atmosphere A black body absorbs all incoming radiation TRUE black bodies don t exist - instead they have albedo: Images: http://ib.bioninja.com.au/_media/greenhouse-effect_med.jpeg http://planetforlife.com//images/blackbodyearth.jpg http://ozonedepletiontheory.info/images/electromagnetic-spectrum.jpg

Factor 3: Atmosphere Some reflected energy gets trapped in the atmosphere by greenhouse gases. Why are some gases greenhouse gases? Images: http://ib.bioninja.com.au/_media/greenhouse-effect_med.jpeg http://planetforlife.com//images/blackbodyearth.jpg

Factor 3: Atmosphere Images: http://ib.bioninja.com.au/_media/greenhouse-effect_med.jpeg http://marketbusinessnews.com/wp-content/uploads/2016/05/greenhouse-gases-most-common.jpg

CO2 Sources and Sinks Sarmiento and Gruber Ocean Biogeochemical Dynamics

Factor 4: The Ocean The ocean acts like a giant sponge, absorbing: ¼ of anthropogenic CO2 emission 90% of additional warming due to the greenhouse effect Credit: Dudarev Mikhail / Fotolia The surface ocean moves North, cool, traps more gas from the atmosphere, and then sinks to the deep The ocean recirculates and eventually these buried emissions will resurface

Factor 5: Orbital Changes (Milankovich Cycles) Images: https://static.skepticalscience.com/images/milankovitch_cycles.jpg https://www.periodni.com/gallery/milankovitch_cycle.png

Example: Eemian Period What made the Eemian period so much warmer than today? -Milankovitch Cycles! -Feedbacks! Images: https://i.pinimg.com/originals/aa/1b/e9/aa1be9c5cba3b9a63979a3e4a2bfb6f4.jpg https://6000generations.files.wordpress.com/2013/05/eemian-and-holoceneinterglacials.png

What does the past tell us? Images: https://simpleclimate.files.wordpress.com/2012/04/edc.jpg http://www.cosmographicresearch.org/images/glacial_maximum_map2.jpg

Modern Climate: The Hockey Stick Is Earth more vulnerable to abrupt climate change now than before? http://news.psu.edu/sites/default/files/styles/threshold- 992/public/hockeystick.gif?itok=d3wvICuj https://upload.wikimedia.org/wikipedia/commons/thumb/2/2d/greenland_gisp2_alley.png/6 40px-Greenland_gisp2_alley.png

Modern Climate: The Hockey Stick Is Earth more vulnerable to abrupt climate change now than before? Images: http://news.psu.edu/sites/default/files/styles/threshold- 992/public/hockeystick.gif?itok=d3wvICuj https://upload.wikimedia.org/wikipedia/commons/thumb/2/2d/greenland_gisp2_alley.png/6 40px-Greenland_gisp2_alley.png

Climate change causes 5 critical environmental changes 1. Warming temperatures of the Earth s surface and oceans 2. Changes in the global water cycle 3. Declining glaciers and snowpack 4. Sea level rise 5. Ocean acidification

1. Surface and Ocean Temperature Change Warming is occurring almost twice as fast as the rate of warming in the previous century

Ocean Temperature and Coral Habitats

2. Changes in the Global Water Cycle - As the atmosphere warms it is able to hold more water vapor - The past century has experienced distinct geographical changes in total annual precipitation

3. Glacier and Snowpack Decline Across the globe nearly all glaciers are decreasing in area Melt water affects seawater level and salinity Earlier spring runoff More frequent and severe flooding

4. Sea Level Rise Warmer water expands, so the ocean increases in volume Melting glaciers and snowpack A 2 m sea level rise would swamp 187 million people This is an upper bound prediction for 2100

Sea Level Rise: Boston Credit: Project 360

5. Ocean Acidification 10.1126/science.aaa6882 The surface ocean equilibrates with the atmosphere Increase of pco2 in the atmosphere consumes the carbonate ion, which decreases its saturation state This impedes the effectiveness of the carbonate pump

Chisholm et al 2000 The Biological Pump Contributors: Soft Tissue Pump Organic matter formed by photosynthesis Dead cells and fecal pellets aggregate and sink Carbonate Pump CaCO3 shells formed by plankton and mollusks Important sink of CO2 from the atmosphere!!!

Ocean acidification= less carbonate formation Dissolution of coral environments Less Biodiversity

Potential Solutions to Ocean Acidification? Geoengineering - Iron Fertilization - Adding alkalinity These have significant economic and ecological costs. Best solution: Stop adding CO2 to the atmosphere

2006 2009 2013 The Aral Sea: anthropogenic environmental and climate change 1977 1986 1999

Anthropogenic Impacts: Increases of agriculture in the 20th century used up all the water coming down the mountains before it could reach the sea Farmers grew water intensive crops Excessive use of agricultural pesticides Island in the center was used at a biological weapons development site (smallpox, plague, etc)

Climate Change Effects: Sea surface temperature (SST) changes Hotter summers, colder winters Exposed seabed results in dust storms Issue for respiratory health Rising salinity kills fish Decimates fishing villages Destroys fishing and canning industry Cultural loss of traditional food

Books Organizations Documentaries

EXTRA SLIDES

How Do We Know About Past Climates? Images: https://climate.nasa.gov/internal_resources/1205/ https://upload.wikimedia.org/wikipedia/commons/thumb/2/2e/cor al_outcrop_flynn_reef.jpg/1200px- Coral_Outcrop_Flynn_Reef.jpg https://ldsmag.com/wp-content/uploads/2016/09/tree-rings.jpg https://eapsweb.mit.edu/sites/default/files/8679459790_36196d6 197_b.jpg http://static.wixstatic.com/media/c309ff_2bc8d6f43cac442aaefe1 ee0eeb34a6e.jpg/v1/fill/w_396,h_296,al_c,lg_1,q_80/c309ff_2bc 8d6f43cac442aaefe1ee0eeb34a6e.webp

Climate Cycle Examples El Nino Southern Oscillation (ENSO) Timescale of 2-4 years Glacial-Interglacial Cycles Timescale of 20,000 years

Factor 3: Atmosphere Imagse: https://d1o50x50snmhul.cloudfront.net/wp-content/uploads/2007/05/dn11639-1_767.jpg http://marketbusinessnews.com/wp-content/uploads/2016/05/greenhouse-gases-most-common.jpg