PPT-Surface-flux driven water mass transformation analysis in E3SM simulations

Hyein Jeong Adrian K Turner Xylar S Asay Davis Darin S Comeau Stephen F Price Milena Veneziani Mark R Petersen Matthew J Hoffman Todd D Ringler Luke Van Roekel Andrew Roberts Jonathan Wolfe and Ryan Abernathey. Levi . Lúcio. , McGill University. The NECSIS Project. “. NECSIS is focused on the advancement of a software methodology, . called Model-Driven Engineering (MDE), that can yield dramatic . i. mprovements in software-developer productivity and product quality.. Irminger. Sea, R/V Knorr. , . October 2008 . Kjetil Våge . Kent Moore . Steingrímur. Jónsson. H. éðinn. . Valdimarsson. Water mass transformation in the Iceland Sea. . - the Denmark Strait Overflow Water. Failure of slopes depends on direction of groundwater flow, but in many cases surface parallel flow is an adequate assumption. Failure also depends on a balance between the intensity and duration of rainfall. What is evaporation?. How is evaporation measured?. How is evaporation estimated?. Reading: Applied Hydrology Sections 3.5 and 3.6. With assistance from Dan Siegel and Marcy Litvak. Evaporation. What is evaporation?. 5-yr running means (. Smith et al. 2015. ). Spurious ocean data?. CERES. ERBS/recon. Reanalysis/recon. Surface temperature hiatus despite continued upper ocean heating (. Durack. . et al. . 2014. , . & . proto . Active Regions. Bob . Stein – Michigan State U.. Lagerfjärd. – Copenhagen U.. Å. . Nordlund. – . Niels. Bohr Inst.. D. . Georgobiani. – Michigan State U.. 1. The Simulation. Mass, Momentum, Energy. Begin with the Reynolds Transport Theorem. Mass – continuity equation. Momentum – Manning and Darcy . eqns. Energy – conduction, convection, radiation. Reading: Applied Hydrology Sections . Mass, Momentum, Energy. Begin with the Reynolds Transport Theorem. Momentum – Manning and Darcy . eqns. Energy – conduction, convection, radiation. Energy Balance of the Earth. Atmospheric water. model . intercomparison. project (FAFMIP). Steering committee. :. Jonathan Gregory (U Reading and Met Office),. . Stephen . Griffies. . (GFDL),. . Detlef. Stammer (U Hamburg), Oleg . Saenko. (. model . intercomparison. project (FAFMIP). Steering committee. :. Jonathan Gregory (U Reading and Met Office),. . Stephen . Griffies. . (GFDL),. . Detlef. Stammer (U Hamburg), Oleg . Saenko. (. How is evaporation measured?. How is evaporation estimated?. Reading: Applied Hydrology Sections 3.5 and 3.6. With assistance from Dan Siegel and Marcy Litvak. Evaporation. What is evaporation?. How is evaporation measured?. Mark Taylor. mataylo@sandia.gov. E3SM Machine Roadmap . CPUs: . BER purchased dedicated systems. Anvil, . CompyMcNodeFace. : 6.2M node-hours per year. Great machines for moderate resolutions – fastest performance. Begin with the Reynolds Transport Theorem. Momentum – Manning and Darcy . eqns. Energy – conduction, convection, radiation. Energy Balance of the Earth. Atmospheric water. Reading: Applied Hydrology Sections . 2. Diffusion of A from pore mouth to internal catalytic surface. 3. Adsorption of A onto catalytic surface. 4. Reaction on surface. 5. Desorption of product B from surface. 6. Diffusion of B from pellet interior to pore mouth.