PPT-Equatorial Oceanic Processes

Figure 143 Average currents at 10m calculated from the Modular Ocean Model driven by observed winds and mean heat fluxes from 1981 to 1994 The model operated by the NOAA National Centers for Environmental Prediction assimilates observed surface and subsurface temperatures From . According . to Alfred Wegener, the super-continent of Pangea began to break up 200 million years ago with the continents attaining the size, shape, and location where we see them today. This movement of continents has not yet come to an end. According to J. Tuzo Wilson, the breakup and drifting of the present continents . Carl H. Gibson. Departments of MAE and SIO, CASS, UCSD, La Jolla CA 92093-0411, . cgibson@ucsd.edu. ,. . http://sdcc3.ucsd.edu/~ir118. AOS seminar, Oct. 1, 2015, . Spiess. 330, 4 pm. Catastrophic Equatorial Icing. Yosef . Ashkenazy. Bluastein. Institute for Desert Research, . Ben-Gurion University. www.bgu.ac.il. /~. ashkena. Collaborators. : . Hezi. . Gildor. , Martin . Losch. , Francis A. Macdonald, Daniel P. . ATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION.S. DEPARTMENT OF COMMERCE Cover Photo - National Severe Storms Laboratory BASIC SPOTTERS Equatorial ocean. A short course on:. Modeling IO processes and phenomena . INCOIS. Hyderabad, India. November 16−27, 2015. References. 1) (HIG . Notes). . McCreary, J.P., 1980: Modeling wind-driven ocean circulation. JIMAR 80-0029, HIG 80-3, Univ. of Hawaii, Honolulu, 64 pp. Trooper, Vincent, Vanity. Facts. This zone is 0 meters to 200 meters deep!( about 600 feet!). Holds 90% of marine life. Sunlight reaches 660 ft. down. Can have photosynthesis. Nicknamed “Sunlit Zone”. Lesson. . Objectives:. To understand what occurs at different plate boundaries.. Success Criteria:. Create an annotated diagram of each plate boundary.. Plate 1. Plate 2. Continental crust. THE WORLD’S MAIN PLATE BOUNDARIES. Research Institute for Gulf of Mexico Studies. Texas A&M . University– . Corpus Christi. Student: Environmental Science MS program . Advisor:. Dr. Jim Gibeaut. Project title: . Sargassum. GLY 4310 - Spring, 2018. 2. Hot Spots, Trails, and . Aseismic Ridges. Figure 14.1. . Map of relatively well-established hotspots and selected hotspot trails (island chains or aseismic ridges). Hotspots and trails from Crough (1983) with selected more recent hotspots from Anderson and Schramm (2005). Also shown are the geoid anomaly contours of Crough and Jurdy (1980, in meters). Note the preponderance of hotspots in the two major geoid highs (superswells).. AGOA Eligible Countries Central African Republic Comoros Democratic Republic of Republic of Congo Cte dIvoire Eswatini Swaziland The Gambia Guinea-Bissau Mauritius Mozambique Namibia So Tom and Prncip Many regions close to the equator experience an equatorial climate. These . regions 0° - 10° N and S of the equator . include, the Amazon Basin (South America), the Congo Basin (Africa), Malaysia, Indonesia and some areas in northern . . EGU2020-9583, . Vienna, Austria. . Department of Geology & Geophysics, Indian Institute of Technology, . Kharagpur. 721 302, . India. S.K. . Bhowmik. & M. . Rajkakati. . Nagaland Ophiolite Complex. quatorial. . Atlantic. P. Brandt. R. J. . Greatbatch. , M. . Claus, S.-H. . Didwischus. , J. . Hahn. GEOMAR Helmholtz . Centre. . for. . Ocean. Research Kiel. 1. 2. Global Model Simulations. Oschlies. Objective & . Essential Question. LO: . I can describe oceanic landforms. . (5.E.3A.2). EQ: . What are the characteristics of continental and oceanic landforms?. Under the Sea. Ocean basin is the .