Glaciers - Know the different types of glaciers Cirque: small glaciers that occupy cirques (small bowl-shaped depressions at mountain tops) valley: when cirque glaciers flow down valley, sometimes joining together, to form “long” glaciers flowing through valleys. calving: any glacier that flows into a lake or ocean, and breaks off (calves) Into icebergs piedmont: any glacier that flows out of a valley And onto a flat area, allowing the glacier terminus to spread out outlet glacier: valley glaciers that drainice caps or ice sheets Ice field: Like an ice cap, but more nunataks poking through, really a lotof connected cirque and valley glaciers - Know what glacier mass balance means. Accumulation zone: all added mass. Mostly this is winter snowfall that doesn’t melt the following summer. Ablation zone: all lost mass. Mostly (1) ice melting and (2) calving of icebergs. Equilibrium Line: where they meet- Know warm based versus cold based glaciers, why the difference, and how it relates to water Cold based Glaciers: The bottom of the glacier is below 0 degrees C. No water, no sliding, no erosion, Glacier sides stay in place, middle slides/extends down middle. Warm based Glaciers: contain water at base of glacier. Causes abrasion leading to striation (sliding therefore erosion) ALSO Ifthe scratching agent is fine particles, thenthis leads to glacial polish - Glacier flow – ice deformation and basal sliding, how do these conditions relateto thermal regime (warm vs. cold based). Evidence for sliding? (striations and polish) 1. Internal Deformation: cold based. Move like silly putty (self deforming after time/temp change) glacier develop bands called Ogives= 1 per year 2. Sliding at Base: the base slides on a thin film of water. Sliding causes abrasion which leaves scratches called striations - Know Glacier plumbing: Supraglacial lake: streams flowing underneath a glacier (high pressure→ melting) Moulin: the hole that surface water fallsinto. It is a pipe that carries the water tothe glacier bed. Subglacial streams: - Know a few specific glaciers, Columbia, Grinnell, Jakobshav Columbia: (Alaska) one of the fastest moving glaciers, retreating since 1982, (13 mill tons of ice break off everyday) Chasing Ice movie. Grinnell: (Montana) between 1966-2005 it lost 40% of its acreage. (retreating) Jakobshav: (West Greenland) produces 10% of all greenland icebergs. Studied for over 250 yrs. (The ice stream's speed-up and near-doubling of ice flow from land into the ocean has increased the rate of sea level rise by about 0.06 millimetres (0.0024 in) per year) Fastest flowing glacier in the world. Up to 15 km/yr = 5.6 ft/hourSea Level - Eustatic vs. local sea level change Eustatic: refers to change in global ocean reservoir Local: refers to the sea lvl at any one location - Causes of local sea level change to be different than global sea level change if enough ice melted to increase eustatic sea lvl by 1 ft local sea levels may not feel it instantly, because ocean circulation currents may change, tectonic plates subside etc. - Isostatic uplift, raised beaches, glaciers melting Isostatic uplift: The uplift of Earth’s crust after removal of an ice load. Raised Beaches: are evidence of local sea level rise. Glaciers Melting: - Subsidence, tectonics/earthquakes Subsidence: when soft sand compacts and land falls to lower lvl along with buildings and things on it. Clicker Q: Why are rates of sea levelrise higher in New Orleans? Local effects of subsidence combined with eustatic sea level rise. - History of sea level rise (last ice age, last century) Clicker Q: How much lower was sea level during the last ice age? About 400 feet (120 m) Last century GMSL increased 4-8in - Causes of sea level rise (thermal expansion, glacier melt, ocean currents, floating ice?) Thermal Expansion: when water heats up, it expands. Glacier & Ice Melt: NOT SEA ICE OR GLACIER ICE Ice sheets: Ocean Currents: (& Subsidence) - Predicting the future, RCP scenarios, expected sea level rise 2100 AD RCP Scenarios: “RepresentativeConcentration Pathways” .97 m expected sea level rise in 2100 AD RCP 8.5 - Different countries’ CO2 emissions,rankthe top 5 1. China 2. USA 3. EU 4. India 5. Russia Clicker Q: Where does the US currently rank in terms of CO2 emissions? Number 2, Behind ChinaLocal Impacts - Global warming impacts across US, in Buffalo region/New England Clicker Q: The “polar vortex” is caused by the weakening of the winter jet stream FALSE Global Warming and Politics - Hockey stick controversy The rate of modern warming is unprecedented & Modern warmingreversed natural cooling Clicker Q: Arctic amplification decreases the equator-pole temperature gradient - the “hiatus” in global warming The CRU hack on personal emails of scientists with internal information used to disprove science legitimacy accusing scientists of - examples of tactics used by global warming deniers - Cherry picking information (global 10yr periods of earth cooling that happens) - Geoengineering The deliberate and large-scale intervention in the Earth’s climatic system - solar radiation management vs. CO2 removal, examples of each Solar Radiation Management: Surface-based: Using pale-colored roofing materials to change surface brightness, orgrowing high-albedo crops. Troposphere-based: for example, marinecloud brightening, which would sprayfine sea water to whiten clouds and thus increase cloudreflectivity. Space-based: space sunshade—obstructingsolar radiation with space-based mirrors, dust, etc. NEGATIVES: 1. Expensive! Grandiose! 2. Hard to predict regional changes 3. Doesn’t address other impacts of CO2 CO2 Removal: Carbon capture & storage (store in ground) and create enegry source Carbon air capture: remove CO2 from air then put air back (carbon capture pod, gadget) Carbon Farming: afforestation/reforestation instead of DEforestation, grow a shit ton of trees, they absorb CO2, remove trees so it won’t decay and release CO2 again (problem: forest would need to be gigantic, will take up agriculture space that’s used for food, need to actually grow tons of trees) Ocean Fertilization: including iron fertilization of oceans (problem, with ocean circulation, CO2 could pop back up in
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