PPT-A distributed glacier model for RASM
Author : debby-jeon | Published Date : 2016-04-27
Jeremy Fyke Bill Lipscomb Los Alamos National Laboratory Goal Simulate the coupled evolution of Arctic glaciers and ice caps within RASM Evolving land ice area
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A distributed glacier model for RASM: Transcript
Jeremy Fyke Bill Lipscomb Los Alamos National Laboratory Goal Simulate the coupled evolution of Arctic glaciers and ice caps within RASM Evolving land ice area A ffects vegetation extent and albedo. deGeer. Moraines . Erica . Doody. What is a . deGeer. moraine?. Small moraine ridges that occur in clusters parallel to each other. Usually found in coastal marine settings. First identified by Gerard . What are the processes of glacial erosion?. They erode by two main processes. As a glacier moves down a valley, it creates pressure on the land which creates heat. This melts part of the glacier. This water runs into small cracks, it the refreezes as it gets colder (freeze-thaw). modelling. Jeremy . Fyke. (LANL). Bill Lipscomb (LANL). Bill Sacks (NCAR). Valentina. . Radic. (UBC, Canada). Synopsis. RCP8.5 Greenland Ice Sheet (GIS) sea level rise contribution predictions. Glacier model initialization on RASM model grid. supply. Dennis P. Lettenmaier. Department of Geography. University of California, Los Angeles. CAS-NASA Workshop . on the use of earth observations to address. . glacier change and associated hazards. With Seismology. Fabian Walter. 2009 – Dr. sc. ETH Zürich. 2004 – MSc University of Colorado, USA. 2002 – BSc Brigham Young University, USA. Host: Laboratory of Hydraulics, Hydrology and Glaciology . Finish South Asia. Nepal: Everest Region. Glacier Lake Outburst Floods. 1999 Slides. Summary of Observed Glacier Changes. Sketch Maps Due on Wednesday!. For . Next Class: Read Chapter 13 (pp. 588-598). Deposition:. AIM:. Erosional and Depositional systems. Do Now: In your notebooks…. 1) Define the two terms below in your own words.. 2) Explain how the two terms work together.. The movement/transport of material from one place to another. Erosive forces . Glacier. persistent . body of dense ice that is constantly moving under its own . weight.. It . forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many . l. a. c. i. e. r?. KEY IDEAS & QUESTIONS. To identify and describe landforms created by glacial . deposition.. To explain . how landforms . of glacial . deposition are formed – moraine, drumlins and . Prairie School. Earth Science. Glaciers: Moving Ice. When you take a handful of snow and squeeze it, you are creating a product that is similar to that of glaciers. . Glacier: fast moving, large mass of ice. . Glacier Movement. Deposits by Glaciers. The Ice Age. Glaciers and Global Warming. Glacial Rebound . …………………. Snow. Line. …………………... Glaciers form in areas covered by snow, where more snow falls than melts each year.. Chris Miller photo. USGS. 2008. Unknown photographer. Courtesy of NPS Historic . Photograph Collection. Harpers Ferry Center. 1920. The 1920 photo shows National Park Service Director, Steven Mather, on Piatt Path near present day. Taku Glacier 2 Calculate the gradient of the Taku Glacier from 1000 ft T. Frank. 1. , H.. Å. kesson. 2,3. , B. de Fleurian. 4,5. , K.H. Nisancioglu. 4,5. 1. Department of Physical Geography, Stockholm University, Sweden. 2. Department of Geological Sciences, Stockholm University, Sweden.
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