PPT-Ocean Break-out Summary

MODIS Science Team Meeting 9 May 2012 Bryan Franz and the MODIS Ocean Science Team R20100 MultiMission Ocean Color Reprocessing Highlights consistent algorithms and methods for all sensors. 1 CD6 SE Fig 1 CD XT SE Fig 1 CD8 SE Fig 1 CD ransport brPage 3br 325 1015 Reading 325 325 Fig 3 17 59 57 Fig 2 1 1 1 brPage 4br Cyrus CD 6 SE 2 CD 8 SE 2 CD XT SE 2 CD T TRANSPORT User Instructions 1 IMPORTANT Read before operating this equipme brPage 1br OUT 12 OUT 34 OUT 56 OUT 7 OUT KICK SNARE OM OM HI GAN UKELELE ZITHER BANJO ELEC GTR OUST GTR OH R OH L OWBELL GAN HI VO AL BASS DIRE BASS MP SOFT S N R SOFT S N L AN G S NTH THERE Rockefeller Jr Memorial PKWY Big Hole NB Cowpens NB Fort Donelson NB Fort Necessity NB Moores Creek NB Petersburg NB Stones River NB Tupelo NB Wilsons Creek NB Kennesaw Mountain NBP Richmond NBP Brices Cross Roads NBS Chickamauga and Chattanooga NMP Safety Break Safety Break Safety Break Safety Break Safety Break Safety Break Lap Swim (2) Open Swim (2) Lap Swim (2) 10:00am-4:25pm Open Swim (2) 12:10pm-2:30pm Safety Break Safety Break Safety Bre Vocabulary. Ocean Current. Coriolis Effect. Rip Current. Upwelling. Major Ocean Currents. An . Ocean Current. is a large volume of water flowing in a certain direction.. Wind-driven currents are called surface currents.. CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS OUT CUT THIS 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. Objectives. In this chapter, you will learn about:. Computer . files. Writing a program that reads from and/or writes to a file. Input file. Output file. The . data hierarchy. Control break logic. 2. 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. 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). 1 WOCE was conceived in late-1970snot so easy to re-capture thinking of the time: . Ocean Decade Research . Programme. on the Maritime Acoustic Environment (UN-MAE). Modeling and Prediction of Ocean Ambient Sound. . A Satellite activity of UN Ocean Decade Laboratories: A Prediction Ocean . We Get Our Food from the Ocean. We Do this both directly and indirectly. We eat fish that is harvested from the ocean. We also process harvested fish for livestock feed. . We get Valuable Minerals from the Ocean. A: Sunlight – Producers require sunlight for photosynthesis. Ocean life is determined by many factors:. B: Temperature – most animals live near the surface where it is warmer. Ocean life is determined by many factors:.