PPT-EART163 Planetary Surfaces
Author : giovanna-bartolotta | Published Date : 2016-03-09
Francis Nimmo Last Week Shapes geoid topography How do we measure shapetopography GPS altimetry stereo photoclinometry limb profiles shadows What is topography
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EART163 Planetary Surfaces: Transcript
Francis Nimmo Last Week Shapes geoid topography How do we measure shapetopography GPS altimetry stereo photoclinometry limb profiles shadows What is topography referenced to . The MEINL Planetary Tuned Gongs ABOUT THE PLANETARY GONGSThe MEINL planetary tuned Gongs arefrequency. These gongs are handcrafric and soothing.They are available in 24/61cm up to 36/91cm Extra-solar planetary systems. Lecture . 16. Other theory. Tidal Hypothesis. Early attempt to explain the dichotomy of planets.. Problem?. tidal force strong enough to “draw out” a filament from stars will effectively disperse it before it could condense into planets!. Francis Nimmo. Last Week – Impact . Cratering. Why and how do impacts happen. ?. Impact velocity, comets vs. asteroids. Crater . morphology. Simple,complex,peak. -. ring,multi. -ring. Cratering. . Module 5. Session Topics. Orthographic projections of inclined and . single-curved . surfaces. Drawing isometric sketches from orthographic views of objects with inclined . and single-curved surfaces. Module 1. Session Topics. Surfaces and Solids of Revolution. Degree of Revolution. Hollow Objects. Visualizing Revolution. Surfaces and Solids of Revolution. Surfaces and Solids of Revolution are formed when a 2-D shape is revolved about an axis. Mechanical Forms. Bang & Olufsen BeoSound 3000. The Mechanical Forms. Cubes, cylinders and their Boolean results are easy to machine. Mechanical forms lack the subtle, interesting changes in silhouette and high-lights which free-forms possess. Paper 50. The Planetary Princes. Paper 50 - Video study group link. Paper 49 The Inhabited Worlds. We would like to give a special thanks to Don Estes for the use of the information from his Chart The Origin, History and Destiny of Universe Reality. We would also like to thank the creator of . Virtual Planetary Laboratory - University of Washington. Adding nitrogen to the planetary greenhouse. A: Pressure Broadening due to N. 2. gas. B: Visible absorption of planetary radiation by NO. 2. Unfortunately, I must depart Wednesday evening, so if you are . Francis Nimmo. Last Week – Shapes, . geoid. , topography. How do we measure shape/topography?. GPS, altimetry, stereo, . photoclinometry. , limb profiles, shadows. What is topography referenced to? . Module 5. HigherEdServices.org. Session Topics. Orthographic projections of inclined and single-curved surfaces. Drawing isometric sketches from orthographic views of objects with inclined and single-curved surfaces. What is . vorticity. ?. Many meteorological web sites include some form of . vorticity. contours on the 500-mb charts. Why. ? How does having contours of vorticity help a meteorologist understand the atmosphere. Peter Fawdon. Department of Earth and Planetary Sciences, Birkbeck, University of London, UK. Centre for Planetary Sciences at UCL/Birkbeck, UK. Joel Davis. Department of Earth . Sciences. , . UCL, . Rodney G. Roberts. Anthony . Maciejewski. Presenter: . Karthik. . Sheshadri. Introduction. =J. Solution is of the form. , with JG=I.. For a repeatable strategy, no end effector movement => no joint movement.. Francis Nimmo. Course Overview. How did the planetary surfaces we see form and evolve? What processes are/were operating?. Techniques to answer these questions:. Images. Modelling. /Quantitative analysis.
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