PPT-Mirror migration of ocean-bottom node data:

Atlantis Gulf of Mexico Department of Earth And Atmospheric Sciences University of Houston Emin Emrah Pacal Advisor Dr Robert Stewart AGL Research Presentations amp Update Meeting 2012. x Dedicated migration experts provide unique product knowledge and experience 57479 Oracle Migration Factory dashboard provides complete guidance and visibility into the process every step of the way KEY BENEFI TS x Faster and more accurate migratio brPage 3br mirror mirror object reconstruction beam virtual mirror photo film brPage 5br film virtual image brPage 6br incident light line of view initial position loaded position Richard Sapon-White. Oregon State University. May 8, 2015. ELUNA 2015. About Data, Structure, and Maintenance. Two Examples. Lessons (To Be) Learned. Sharing information. 2. Overview. The . fault, dear Brutus, is not in our stars. Dr. Michael J Passow. Earth2Class Workshops for Teachers. Lamont-Doherty Earth Observatory. michael@earth2class.org. . Scientific Ocean Drilling. Started in 1960s and continues today. Cores and geophysical data have revealed much about our planet. mirror, along the bottom and then up through the second half-silvered mirror? If we movethe mirrors slightly we will find that now all the photons are seen by the side detector. Doesthis mean that no for Elastic . Cloud Platforms. Aaron J. . Elmore, . Sudipto Das. , . Divyakant. . Agrawal. , . Amr. El . Abbadi. Distributed Systems Lab. University of California Santa Barbara. Serve thousands of applications (tenants). Samuel Ranta, 23.11.2015. Ingredients of archival disaster: multiple platforms, multiple formats, no compatibility. Who controls the past controls the future. Who controls the present controls the past.. Richard Sapon-White. Oregon State University. May 8, 2015. ELUNA 2015. About Data, Structure, and Maintenance. Two Examples. Lessons (To Be) Learned. Sharing information. 2. Overview. The . fault, dear Brutus, is not in our stars. System. Stuart A. . Cunningham. Scottish Association for Marine Science. Stuart.Cunningham@sams.ac.uk. . Barbara Berx. 1. , Eleanor Frajka-Williams. 2. and Mark Inall. 3. 1. Marine Laboratory Science, Aberdeen. Ceramic Analysis at the Gehring Site. Ashley Cisneros. Introduction. American Bottom during . the Middle Woodland Period. (BC 150- AD 350). Possible “Shatter Zone”?. Struever 1964. Fortier (2006) points to . HOW DO OCEAN GLIDERS WORK? Ocean gliders sink and “glide” downward from the sea surface – when its computer triggers a piston that draws in some seawater and therefore extra weight. Near the bottom, a reverse action causes the glider to rise and “glide” upward towards the surface. As the glider saw-tooths its way through the ocean it measures ocean properties (e.g., temperature) . Every few hours, the glider pauses at the surface and transmits its data via satellite back to the laboratory – thus providing us with a Terms:. Plane mirror- a smooth reflecting surface. Virtual image- images formed by a plane mirror. CANNOT be projected onto a screen. Real image- images that can be projected onto a screen (. ie. . pin hole camera). Historical review............................................................................................................................3 ......................................................... Objectives of this session. Hardware Setup. Configure your device in HYPACK Hardware. Analog Setup. Installing NIDAQ software. Configuring connection. Surveying. Adjusting imagery. Adjusting display.