PPT-Sensitivity of continental boundary layer chemistry

to a new isoprene oxidation mechanism Jingqiu Mao Harvard Fabien Paulot Caltech Daniel Jacob Harvard Paul Wennberg Caltech Ronald Cohen UC Berkeley and funding from NASA ACMAP temperature radiation land use. 2 Complete all information requested on the online form available at wwwcontinentaltirepromotionsca or this mail in form accurately and legibly and SURYLGH57347D57347FRS57347RI57347RXU57347UHWDLOHU57526V573475HFHLSW57347WKDW57347FOHDUO57347LQGLFD te brPage 1br DataLink Layer 1 DataLink Layer 2 DataLink Layer 3 DataLink Layer 4 DataLink Layer 5 DataLink Layer 6 brPage 2br DataLink Layer 7 DataLink Layer 8 DataLink Layer 9 DataLink Laye Pressure gradient is found from . freestream. (external) velocity . field. Boundary layer equation:. x. z. Effect of Pressure Gradient on the flow in a Boundary Layer. In the accelerating part of the stream,. . 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. . Chapter. 12-1. Pan-. gaea. . “. all. - earth. ” . Note: Our world today is actually a 2’nd or 3’rd generation “super continent” or “. pangea. ” !!!. . Alfred Wegener . 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. Ocean-continent. . convergent boundary. Plate of oceanic crust collides with plate of continental crust. Oceanic crust is . subducted. (goes under) continental plate.. Ocean-ocean convergent boundary. • What is “Inorganic Chemistry”?. . - descriptor or professional subfield. . - same as “General Chemistry”?. • Highlights from the inorganic timeline. . - Lavoisier: origin of modern chemistry. The MIDDLE Layer Lesson 4 GOAL: The Middle Layer The goal of this stage is to solve the Middle Layer while keeping the WHITE face intact. ( t he WHITE cross and WHITE corners ) For this lesson, Photochemical grid model estimates of lateral boundary contributions to ozone and particulate matter across the continental United States Kirk Baker U.S. Environmental Protection Agency Research Triangle Park, NC . (4). . . Residual Layer . About a half . -. hour before sunset the thermals cease to form (in the absence of cold air advection), allowing turbulence to decay in the formerly well-mixed layer. The resulting layer of air is sometimes called the residual layer. . Enter . Silently. Grab Materials. Begin Do Now. Write in your planner for the week. Open your notebook to the front of page 17. . I Do (5 min) . Topic: . Earth. Front Page 17 Title: “How to Make a Concept Map”.