PPT-Coupled ocean-atmosphere modeling on horizontally icosahedr

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. 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 . Eric . Prebys. , FNAL. Coupled Harmonic Oscillators. USPAS, Knoxville, TN, January 20-31, 2014. Lecture 12 - Coupled Resonances. 2. Equations of motion. Define uncoupled frequencies:. Try a solution of he form:. Building an idealised coupled system. Polly Smith, Amos . Lawless, Alison Fowler*. School of Mathematical and Physical Sciences, University of Reading, UK. * funded by NERC. Outline. Recap. objectives. Coupled Atmosphere-Ocean . Data . Assimilation. Strategies with an . EnKF. and a Low-Order Analogue of the . Climate System. Robert Tardif . Gregory J. Hakim . Chris Snyder. University of Washington. Objects Projected Horizontally. Horizontal projectile motion:.  . horizontally . the velocity . (. ) is . always constant . (. . = 0. ). vertically the initial velocity (. y. ) is always zero. vertically . 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 Composition of the Atmosphere The atmosphere is comprised of a variety of gases: Major Constituents (99%): Nitrogen (N): 78% Oxygen (O 2 ): 21% Trace Constituents: Other: 1% calls. CW2015. Kristian. S. . Mogensen. Marine Prediction . Section. k.mogensen@ecmwf.int. Overview of talk:. Baseline:. The focus of this talk is going to be on coupling of IFS and WAM to NEMO. Motivation. Presented By Suru . Saha. (EMC/NCEP). Contributors: . Jack Woollen, Daryl Kleist, Dave . Behringer. , Steve Penny, . Xingren . Wu, Bob . Grumbine. , Mike . Ek. , . Jiarui. Dong, . Shrinivas. . Moorthi. Brandon Kerns*, . Shuyi. S. Chen, . Chiaying. Lee, and . Falko. . Judt. RSMAS/University of Miami. I. nterdepartmental . H. urricane . C. onference Miami, Florida 28 February – 3 March 2011 . Asynchronous I/O. Navy ESPC (global coupled model). COAMPS (regional coupled model). Radiative transfer model (experimental). [New] NEPTUNE (global atmosphere). [New] NAAPS/aerosol model. Space Science Division . Participationin COREs(Coordinated Ocean-ice Coupled OceanCoupled Ocean--Ice Models Ice Models within the CSM Frameworkwithin the CSM Framework -HYCOM PanAm2.1 (hybri-Normally 2-26 vertical layers-CI AABBCCDD 191 ABCD E EEAB CDABCD 191 SIZE TABLEwaist **Lower waist RegularUK Size6XL30R36R40R46RSwedish sizeC60C62C64B WaistD Inside leg Chest sizesUK Size RegularUK Size10R 16R 20RSwedish sizeB W