PDF-THE WORLD OCEAN CIRCULATION EXPERIMENT WOCEANDTHE JOINT GLOBAL OCEAN

1 WOCE was conceived in late1970snot so easy to recapture thinking of the time. 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 Susan Howard. Earth & Space Research. Basically – why and how the ocean and atmosphere MOVE!. www.ametsoc.org . There are many scales of motion: . From . BIG. . to . very small. Today – I will just cover the basic large scale, GLOBAL circulation.. It’s clever entrance and escape . Sarah Woodhouse. The Carbon Cycle. Trees breathe too. Into the Sea. The ocean alone contains 36,000 . giga. tons of carbon mostly in the form of bicarbonate ion which aids in the pH balance. . ROSES . – . Interdisciplinary . Research in Earth Science (IDS. ). Linking Greenland ice sheet mass loss to . decadal. circulation changes in . the ocean and atmosphere. Patrick Heimbach. *. , MIT. 10 years of AMOC measurements from the RAPID program and a view to the future. Gerard McCarthy, Darren . Rayner. , Ivan . Haigh. , Joel . Hirschi. and David . Smeed. . National Oceanography Centre. Introduction to the physical climate system. Oliver Elison Timm ATM 306 Fall 2016. Lecture 1. Ocean Circulation. Objectives. Provide an overview of the ocean circulation. Surface currents. Wind-driven circulation. (AOSS 480 // NRE 480) . Richard B. Rood. Cell: 301-526-8572. 2525 Space Research Building (North Campus). rbrood@umich.edu. http://. aoss.engin.umich.edu. /people/rbrood. Winter 2015. February . 10, . (AOSS 480 // NRE 480) . Richard B. Rood. Cell: 301-526-8572. 2525 Space Research Building (North Campus). rbrood@umich.edu. http:/. /. clasp. .engin.umich.edu. /people/rbrood. Winter . 2016. February . . 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 . EFFECT OF TEMP > EFFECT OF SALINITY. OCEAN LAYERS. SURFACE MIXED ZONE – less dense upper ocean, temp and salinity change often. TRANSITION ZONE – fairly constant density, acts as barrier between surface and deep zones. Ocean Current Layers. Surface Currents. . – . top . 10% of the ocean; upper 400 m. Deep Currents . – lower 90% of the ocean. Properties . of . Ocean . Water . How they impact ocean currents. Temperature. science plan: https://. www.iqoe.org. /sites/default/files/files/. IQOE_Science_Plan-Final.pdf. Prof. Steve Simpson, co-chair IQOE Science Committee. University of Bristol (UK). How have human activities affected the global ocean soundscape compared with natural changes over geologic time?. Andrey Proshutinsky. Physical Oceanography Department. AOMIP young scientists school. Tuesday October 20, 2009. 1. Major themes:. Wind blows – ice goes: synoptic scales of variability. Seasonal changes and effects. Andrey Proshutinsky. 1. , Eiji Watanabe. 2. , Elena Golubeva. 3. , Christophe Herbaut. 4. , Marie-Noelle Houssais. 4. , . Jiayan. Yang. 1. , Jinlun Zhang. 5. , . Yevgeny. Aksenov. 6. and Beverly de Cuevas.