PPT-Correlation Analysis of Glacier Melt

Are glaciers melting the same way By Matt Barr Introduction Rapid glacial melt occurred during the 20 th century with negative trends continuing into the 21 st century Glaciological method calculates mass balance of glaciers. Glacial Erosion. As glaciers travel over land, glacial ice can erode the underlying bedrock.. This erosion can happen by:. Plucking. A. brasion. Plucking. This occurs when melt water at the base of the glacier freezes in cracks and fractures the underlying bedrock.. 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. Third Pole Environment Workshop, 26-28. th. October, Kathmandu. Krishna . Lamsal. and Rijan . Bhakta Kayastha. naturekrish@gmail.com. , . rijankayastha@gmail.com. Introduction and Overview of the Problem. 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. What is Correlation Analysis?. Testing the Significance of the Correlation Coefficient . Regression Analysis. The Standard Error of Estimate . Assumptions Underlying Linear Regression. Confidence and Prediction Intervals. a measure of the extent to which two variables change together.. How well does A predict B?. The correlation may be positive, negative, or have no relationship.. Correlation. A . positive correlation . Summary of the measure of the characteristics of individuals in groups.. A descriptive statistic talks about a single characteristics within a given group. Lots of descriptive statistics are summarizing lots of characteristics but all within a given group.. 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 . It originates on land from the accumulation, compaction, and . recrystallization. of snow. .. A glacier appears to be motionless, but glaciers move very slowly.. Glaciers are dynamic weathering . and erosional . 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. provided by the. Department of Geological Sciences. Dr. Stefan Winkler. Department of Geological Sciences. University of Canterbnury. Hooker Glacier and Mt Cook/Aoraki. Does a glacier melt at night? . from . phoscorites. of the. Kovdor. massif. Anna . Redina. , . Cora . Wohlgemuth-Ueberwasser. , Julia . Mikhailova. , and Gregory . Ivanyuk. Kovdor. massif, location and composition. The . Kovdor. 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.