PPT-Ice Melt, Sea Level Rise, and

SuperStorms Richard Nolthenius PhD A Condensed Digest of the Paper of Hansen Sato et al 2016 and and What are the Economic and Physics Constraints on our Options to Deal with Climate Change . Decline in the extent and thickness of Arctic sea ice is an active area of scientific effort and one with significant implications for ecosystems and communities.. Forecasting for seasonal timescales (i.e., the summer and into fall) is of particular interest to many stakeholders.. Derrick Lampkin (Penn State). David Schneider (NCAR). Characterizing and Predicting Surface Melt in Antarctica. Funded by the Office of Polar Programs,. National Science Foundation. Collaborative Research: Decoding & Predicting Antarctic Surface Melt Dynamics with Observations, Regional Atmospheric Modeling and GCMs. PLANNING FOR ACCELERATING SEA LEVEL RISE THROUGH THIS CENTURY AND BEYOND.. HAROLD R. WANLESS. hwanless@miami.edu. for . NAIC . Fall National Meeting . – Sea Level Workshop. Fontainebleau Hotel, Miami Beach. History of Sea Level Rise in Florida. 120,000 years ago 18,000 years ago Today. + 6 meters - 120 meters . Causes of Sea Level Rise. Thermal expansion of water. Oceanographic factors. O. cean circulation (Atlantic Ocean vs. Gulf of Mexico). Atmospheric pressure. Vertical land movements. Tectonics. Tectonic plates are rising and falling in different parts of the world from the weight of past glaciers (Glacial . Some basics . -- of ice, . -- Relation to sea level, . -- Ice reservoirs. Greenland. Antarctica. Continental glaciers globally. Arctic Ocean. . An Important Point . Archimedes Principle. Adam Reeder, P.E., CFM. Eric Coughlin, GISP, CFM. Agenda. 2. What’s . this . sea level . rise . study. ?. How did we conduct the study?. What kind of results did we get?. What do we tell the . stakeholders?. Kayla Berger, Rachel Case, Chase Garrison, Austin Greenhill, Angela Kennedy, Lena Midgette, Alissa Ralston, Fallon Woolford & Alexa Zwicker. Introduction. . Everglades National Park established in 1947. composition in equilibrium with the Fo-richest olivine is obtained. .. This approach may be VERY DANGEROUS…. Potential. Temperature. Follow this sequence:. Analyze with EMP olivine in basaltic rocks;. 2. and H. 2. O: Experimental data at 5.5 . GPa. and . 1200-1450°C. V.S. . Sobolev. Institute of Geology and . Mineralogy. . Russian Academy of Sciences. A.N. Kruk. .. A.G. . . Sokol. According to the existing models of kimberlite origin, free . 8. th. grade science unit. Source:. http://nsidc.org/cryosphere/seaice/characteristics/formation.html. Arctic or Antarctic. Antarctica- "land surrounded by water“. Arctic - "water surrounded by land" . Navigating. Navigating ocean currents and ice drift. In the past many people did not know that there was ice in the Arctic Ocean or that the ice moved. . We first learned this from finding objects that had drifted across the Arctic.. JPL’s . ISSM (Ice Sheet and Sea Level System Model). shows how the loss of ice mélange makes it easier for rifts in the ice to widen (. ice mélange and rifts shown in pink). Ice mélange remnants . States of matter. There are 3 states of matter, can you name them?. S……... L……... G…... What do we know about them?. video. (6) Melting and Freezing | BBC Bitesize | science - YouTube. Melting point.