PPT-EVPP 110 Atmosphere and Ocean Circulation –

Activities 1 5 6 11 Succession 3A Week of November 5 th 2018 Ver 13 Last updated 1142018 11127 PM Atmosphere and Ocean Circulation Activity 1 Fluid Behavior of . 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. . Ferrel. cell. Ferrel. cell. Polar cell. Fig 1. Earth’s radiation budget. What do ‘surplus’ and ‘deficit’ refer to?. What wavelength ranges are for shortwave and . longwave. ? What are their sources?. 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. Geosc040, Lecture . 9 . Feb9, 2016. Somewhere . Beyond The . Sea, . Sinatra. Ocean Avenue. Yellowcard. . Thanks to . Caitlyn N. and . Alexandra B.. Thermohaline. circulation. On-line . Assignments 4 & 5 . 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. Rusty, a carbon atom, welcomes you to the atmosphere. Rusty is currently in a molecule of CO. 2. in the atmosphere, but that is soon going to change.. . You get to decide where Rusty will go next on his adventure. It’s your choice…. Fast . vs. Slow Carbon Cycles. There’s a “Fast” cycle, and a “Slow” cycle. Fast Carbon Cycle. – rapid interchange between . surface ocean. , atmosphere, and top layer of soil and biosphere. Time scales of days to ~decade.. AOS 101 Weather and Climate. Lisha. M. . Roubert. University of Wisconsin-Madison. Department of Atmospheric & Oceanic Sciences. Today’s Lab. Today we will be using the tank lab to simulate the general circulation of the atmosphere. . 7 . Survivorship – . Activities . 1-2. Week of . November 11 . 2018. Version . 1.3. . Last updated: . 11/11/2018 9:23:26 PM. Atmosphere and Ocean Circulation . –. Activity . 7 – Temperature and Humidity at the . Oceanic Biogenic Volatile Organic Compounds (BVOCs): formation processes and ocean-atmosphere exchange Hang Qu Ruixiong Zhang April 16 2014 Outline Introduction OVOCs f ormation processes Ocean-atmosphere exchange 1 WOCE was conceived in late-1970snot so easy to re-capture thinking of the time: Polly Smith, Alison . Fowler & Amos . Lawless. School of Mathematical and Physical . Sciences, . University of . Reading, UK.. Introduction (1). Typically, . initial conditions for coupled atmosphere-ocean model forecasts . 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.