PPT-Uncertainties in the atmospheric oxidation of biogenic vola
Author : min-jolicoeur | Published Date : 2016-06-15
Jingqiu Mao PrincetonGFDL Yale University 02202014 Acknowledgement Measurements William Brune Penn State Xinrong Ren NOAAUMD Modeling Fabien Paulot Harvard Daniel
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Uncertainties in the atmospheric oxidation of biogenic vola: Transcript
Jingqiu Mao PrincetonGFDL Yale University 02202014 Acknowledgement Measurements William Brune Penn State Xinrong Ren NOAAUMD Modeling Fabien Paulot Harvard Daniel JacobHarvard Ron Cohen UC Berkeley Paul WennbergCaltech Larry HorowitzGFDL. Phys. Accuracy and Precision. The . accuracy. of a measurement tells you how close the measurement is to the “true” or accepted value. . The . precision. of a measurement tells you something about the . Problem Solving class 1 for Physics 1A and Higher Physics 1A. What are problem solving classes?. These form a bridge between lecture material, labs and the exam.. In some problem solving classes you will be introduced to material covered in the lab part of the course.. Sequestration (. tCDR. ): . Multifunctionality . for global resilience. Convener. : Rüdiger Grote. Institute . of. . Meteorology. . and. . Climate. Research (IMK-IFU, KIT), Garmisch-Partenkirchen (. Aims. To be able to calculate the percentage uncertainty of a measurement. To be able to combine these uncertainties to evaluate the overall uncertainty in a derived result. A Speed camera takes two images of a moving car and works out speed by calculating distance/time. How do you think this image would help somebody appeal their fine in court?. A Practical Guide. What you should already know well. What you need to know, . and use. , in this lab. More details available in handout ‘Introduction to Experimental Error’ (2. nd. Year Web page).. The oxidation state is a measure of the degree of oxidation of an atom in a substance and it is the fundamental key to understanding redox reactions, reaction mechanisms, catalysis, etc. I Lecture 15. Thanks to Colette . Heald. for many of the slides in this lecture. A “typical” smoggy day. OZONE PRODUCTION IN TROPOSPHERE. Photochemical oxidation of CO and volatile organic compounds (VOCs). Jared Brewer, Emily Fischer, . Christoph. Keller, Makoto Kelp,. Matt Bishop, A.R. . Ravishankara. Special thanks to:. Melissa . Sulprizio. , Bob . Yantosca. j. ared.brewer@colostate.edu. This work was supported by NASA Award . What are problem solving classes?. These form a bridge between lecture material, labs and the exam.. In some problem solving classes you will be introduced to material covered in the lab part of the course.. Calcareous Ooze. Biogenic . calcareous ooze composed . of precipitated CaCO. 3. (usually calcite, but occasionally aragonite) shells of microscopic plankton . Planktonic foraminifera. Coccolithophore. Biogenic . Amines in Fermented Soybean Foods. Professor Jae-. Hyung. . Mah. Department of Food and Biotechnology. Korea University. August 12, . 2015. 4. th. International Conference and Exhibition on. . with Monte Carlo random trials. Alexander Kramida. National Institute of Standards and Technology,. Gaithersburg, Maryland, USA. . Parameters in atomic codes. Transition matrix elements. Slater parameters. EARTH SURFACE. gravity. random. motion. Weight of all air molecules is propagated to surface by random motion of molecules. Random motion of molecules causes pressure to be applied in all directions. Guus . Velders. The Netherlands. (. RIVM. ). Guus. . Velders. 2. Focus on Ozone-Depleting Substances. Projections of gases controlled by the Montreal Protocol. CFCs, halons, HCFCs, carbon tetrachloride, methyl chloroform, CH.
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