PPT-Quantification of Regional Carbon Fluxes and Boundary Layer

William Ahue University of Wisconsin Madison Dept of Atmospheric and Oceanic Sciences Department Seminar 28 April 2010 Advisor Prof Ankur Desai What to Expect Motivation and Background. Kenneth Davis. 1. , . Arlyn. Andrews. 2. , Maria Cambaliza. 3. , Scott Denning. 4. , Liza Diaz. 1. , Kevin Gurney. 5. , Thomas Lauvaux. 1. , Natasha Miles. 1. , Stephen Ogle. 4. , Antonio Possolo. 6. . Drag force. The surrounding fluid exerts pressure forces and viscous forces on an object. .. The components of the resultant force acting on the object immersed in the fluid are the drag force and the lift force. . Convection in the boundary layer occurs to transport heat moisture, and momentum from surface to free atmosphere. Two common scenarios:. 1) Daytime solar heating 2) cold-air outbreaks, lake effect. National Snow and Ice Data Center, University of Colorado. Tingjun. Zhang. Kevin Schaefer. Tim . Schaefer. Lin Liu. Me. Alessio. . Gusmereli. Permafrost Primer. Skiklomanov [2007]. Permafrost:. G. Michael Clarkson and Fred B. Schneider. Cornell University. RADICAL. May 10, 2010. Goal. Information-theoretic. Quantification of. programs’ impact on. Integrity. of Information. (relationship to database privacy). Lecture One. Paul . Constantine. March 29, 2011. What is UQ???. Uncertainty Quantification – ME470. Paul Constantine. Combining computational models, physical observations, and possibly expert . judgment . based on . 234. Th budgets in the Atlantic Sector of the Southern Ocean along 40S [GEOTRACES Cruises D357 and JC068]. By Katsiaryna Pabortsava, Dr. Patrick Martin, Dr. Richard Sanders, Prof. Richard Lampitt . Michael Clarkson and Fred B. Schneider. Cornell University. IEEE Computer Security Foundations Symposium. July 17, 2010. Goal. Information-theoretic. Quantification of. programs’ impact on. Integrity. Houze. , . Jr. *. University of . Washington, *PNNL. PNNL. Richland, WA. 27 September 2016. Development of shallow, precipitating clouds during MC3E. AMIE/DYNAMO . Early . suppressed. 1) Cloud lines oriented parallel to wind direction and (initially) to low-level shear. Viscous effects confined to within some finite area near the boundary → . boundary layer. In unsteady viscous flows at low . Re. (impulsively started plate) the boundary layer thickness . δ. . grows with time. Emily Moder – Grand Energy Challenges. Background. Basics of boundary layer fluid mechanics. Turbulent structures – vortices. Navier. -Stokes Equation:. Experiment Setup. Goal: create a simulation of a thermally stable boundary layer, and measure the fluid dynamics properties of the system. In a flow, the boundary layer represents a (relatively) thin layer of fluid that is nearest the solid boundary. 87-351 Fluid Mechanics. [ physical interpretation: what are we doing today? ]. The behaviour of the boundary layer is very different from that of the fluid above it. Using Ground Based and in Situ Airborne Observations Collected during the CLARIFY 2017 and LASIC Field Campaigns to Explore Synoptic, Dynamical and Aerosol Constraints on Precipitation. Paul Barrett (Met Office) . . Andrew . Turnipseed. Measuring and Monitoring Forest Carbon in the Americas . Manitou . Experimental Forest. September 15, 2011. It is NCAR's mission to plan, organize, and conduct atmospheric and related research programs in collaboration with the universities and other institutions, to provide state-of-the-art research tools and facilities to the atmospheric sciences community, to support and enhance university atmospheric science education, and to facilitate the transfer of technology to both the public and private sectors..