PPT-UPDATE FROM THE OCEAN MODEL WORKING GROUP

A Blend of Recent Activities and NearTerm Priorities OBJECTIVES Address some longstanding algorithmic shortcomings of the Parallel Ocean Program version 2 POP2 Continue to develop new or improve existing . Student Tasks and Roles. Objectives and Standards. Websites. For the Teacher. Assignments. Rubrics. Conclusion. Introduction: . In this unit students will explore ocean life. The different layers of the ocean and its various life forms will be discussed and learned about. Also, various levels of activities will be done.. T. Lebrun. 1. , H. Massol. 1. , E. Chassefière. 1. , A. Davaille. 2. , E. Marcq. 3. , P. Sarda. 1. , F. Leblanc. 3. , G. Brandeis. 4. . 1 . Univ Paris-Sud, Laboratoire IDES, UMR8148, Univ. Paris-Sud, CNRS, Bât. 504, Orsay, F-91405, France;. isopycnic. grids. Rainer Bleck, Shan Sun, . Haiqin. Li, Stan Benjamin. NOAA Earth System Research Laboratory. Boulder, Colorado. April 2016. Design . goals. :. (some reached, some pending). Global domain. -. Julian Oscillation. . . Toshiaki . Shinoda (Texas A&M . Univ.,. . Corpus Christi), . Weiqing. . Han (Univ. . of Colorado. ). ,. . Yuanlong. . Li (Univ. . of Colorado), . Chunzai. Wang (NOAA/AOML. MEDITERRANEAN SEA. NILE RIVER. CONGO RIVER. ZAMBEZI RIVER. NIGER RIVER. ATLAS MOUNTAINS. SAHARA DESERT. DRAKENSBURG MOUNTAINS. GREAT RIFT VALLEY. ETHIOPIAN HIGHLANDS. KALAHARI DESERT. MT. KILAMANJARO. How do different currents form. What is upwelling. What do ocean currents transfer. Predict. T F. Ocean currents are always cold. C. ontinents affect the direction of currents. Currents only flow near the surface of the ocean. La gamme de thé MORPHEE vise toute générations recherchant le sommeil paisible tant désiré et non procuré par tout types de médicaments. Essentiellement composé de feuille de morphine, ce thé vous assurera d’un rétablissement digne d’un voyage sur . From 100-200 m (600 ft) to the deepest part. Mesopelagic (to depth of 3300 ft -1000 m). Twilight. THE DEEP - Bathypelagic, Abyssopelagic & Hadopelagic. No sunlight at all. THE MESOPELAGIC. From 100-200 m to depth of 3300 ft (1000 m). U3D13 – Bell Ringer – 12/14. Short Answer Practice: Cloud Formation. Fill in the blanks of the explanation using the word bank:. Cloud, condenses, dew point, rise, humidity, expand, condensation nuclei, pressure. Greg . Seroka, . Scott Glenn, Travis Miles, . Yi . Xu. , Oscar . Schofield, Josh . Kohut. Rutgers University Coastal Ocean Observation Lab. March 5, 2014. 68. th. IHC. Image . Credit. : . NASA/NOAA GOES Project. For much of human history, knowledge of the ocean and its currents was not recorded for many reasons - most sailors could not write and information was passed orally.. European nations began systematic ocean explorations but kept information secret between the 15. Section 2: Life in the Oceans. Section 3: Ocean Resources. Salinit. y. - measure of the mount of dissolved salts and other solids in a given liquid. Thermocline. - marks the distinct separation between the warm surface water and the deep, cold water. ?. Subsurface flows and impacts on chemical . fluxes, . geotechnics. , slope failures.. Fluvial sources of sediment to the coastal ocean: vertical structure of flows, sediment load, and hydrodynamic properties of sediment delivered.. and . Ocean Technology Transition ( OTT). . COMT and associated projects - infrastructure. Five new multi year projects, and one internal project. . University Corporation for Atmospheric Research - .