PDF-and forecast products and predictionsfrom ocean and atmosphere adding

Earth Observation wwwesaintwwwesaint OLCI contains five cameras to continue the work of Envisat. strategies for coupled 4D-Var data assimilation using an idealised atmosphere-ocean model. Polly Smith, Alison . Fowler & Amos . Lawless. School of Mathematical and Physical . Sciences, . University of . 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. Mercury in the environment: . where does it come from?. Daniel J. Jacob, Harvard University. A brief human history of mercury poisoning. Qin Shi Huang,. 1. st. emperor of China. Mad hatters. Minimata. temperature difference. P. J. Minnett, A. Chambers & N. . Perlin. Rosenstiel . School of Marine and Atmospheric Science, . University . of Miami, . USA. Earth Observation for Ocean-Atmosphere Interactions Science Frascati, October 2014. 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…. ECNU, China. 3. . June 2011. Part. 3. Kathleen . Strabala. Cooperative Institute for Meteorological Satellite Studies. Space Science and Engineering Center. University of Wisconsin-Madison. MODIS Aerosol Product. 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.. 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 Atmosphere Systems Interact . to . Create Hurricanes. Questions. What is a hurricane. ?. What four . conditions are necessary for hurricane . formation?. What . happens as hurricanes approach land?. What is a . 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 . Average Atmospheric Composition. Permanent. Variable. SOURCE. (to atmosphere). SINK. (removal from atmosphere). N. 2. Fixed by soil bacteria. Fixed by ocean phytoplankton. Lightning. Denitrification by anaerobic . Conclusions Up Front:. Mid-Atlantic is home to the most advanced observing systems in the world. Much can be leveraged to support the Blue Ocean Economy. Well defined process to fill gaps. Greatest need is not for new technologies . and . Ocean Technology Transition ( OTT). . COMT and associated projects - infrastructure. Five new multi year projects, and one internal project. . University Corporation for Atmospheric Research - .