PDF-Table 5-2. Ozone Depletion Potentials (ODPs) for long-lived halocarbon

Author : debby-jeon | Published Date : 2017-03-01

12 10 082 073 081 34 30 CFC113 08 085 081 082 34 30 CFC114 10 058 050 37 30 CFC115 06 057 026 34 32 Annex AII 1301 100 159 152 190 61 57 halon1211 30 79

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Table 5-2. Ozone Depletion Potentials (ODPs) for long-lived halocarbon: Transcript

12 10 082 073 081 34 30 CFC113 08 085 081 082 34 30 CFC114 10 058 050 37 30 CFC115 06 057 026 34 32 Annex AII 1301 100 159 152 190 61 57 halon1211 30 79. Layer. Depletion. “. Life’s Support System Depletion. ”. Outline of Presentation. What is the Ozone layer?. How is ozone created and destroyed?. What is the Ozone hole?. What are the causes of Ozone Depletion?. The . ozone layer. is a layer in . Earth's atmosphere. which contains relatively high concentrations of . ozone. (O. 3. ). . This layer absorbs 97–99% of the . Sun. 's high frequency . ultraviolet light. the progression of the Ozone hole over the antarctic from 1970 to 1997.. Some effects on plant and animal tissue as UV radiation increases. decrease in agricultural yields and a decrease in overall forest productivity. AND CURRENT STATUS. GLY 4241 - Lecture 8 . Fall, 2016. Mount Pinatubo Eruption, 1991. 2. 3. 1997 Montserrat Eruption. 4. Sulfur Dioxide Conversion. 5. Aerosol Optical Depth Analyses. BRW is Pt. Barrow, Alaska. ˚ 1˚. Tomislav Prokopec, . ITP Utrecht University . GR21, 12 Jul . 2016. S. Park, T. . Prokopec. , R.P. Woodard, ``Quantum Scalar Corrections to the Gravitational Potentials on de Sitter Background,'' arXiv:1510.03352 [gr-qc] . Ozone produced from the interaction of hydrocarbons and oxides in the presence of sunlight. At ground level, ozone is a pollutant; in the upper atmosphere it protects earth from excess radiation from sun. in Austria. 02 June 2015 // Gerald Kalt. Biomass Policies . workshop: . Lessons . learned and policy challenges . in a mature bioenergy . market. , . Vienna, 2 June 2015. Comparison. . with. . current. multicomponent systems. Konstantin . Gubaev. Skolkovo. Institute of Science and . Technology (. Skoltech. ). Russia. Motivation. What . MD simulation is capable of doing?. Empirical potentials: . 10. AddressNo969WenyiRoadHangzhou310000ChinaPhone8618616109836MailqinqinxuyemeOBJECTIVEPositionappliedSoftwareEngineerResearchinterestsDistributedcomputingdataminingEDUCATIONBACKGROUNDMSinAdaptiveDistribu The . ozone layer or ozone shield . is a region of Earth's stratosphere that absorbs most of the Sun's UV radiation. . It contains high concentration of ozone (O3).. It is a pale blue gas at room temperature.. Retrievals . from . Joint UV and Visible . Measurements by the . TEMPO. Juseon Bak, Xiong Liu, Chris Miller, Kelly Chance. ,. John Houck, Ewan O’Sullivan, Caroline R. . Nowlan. , G. Gonzalez . Abad @ . Quick recap…. ". The ozone layer. " refers to the ozone within stratosphere. over 90% of the earth's ozone resides. Ozone is an irritating, corrosive, colourless gas with a smell. O. 3 . formed by . Roy F. Baumeister. University of Queensland & . Florida State University. What is Self-Control?. Overriding responses, changing oneself. Thoughts, emotions, impulses, performance. What is Self-Control?. N. 2. O . under the. Vienna Convention for the Protection of the Ozone Layer and/or . Montreal Protocol on Substances that Deplete the Ozone Layer. Peter M. Grabiel. Institute for Governance & Sustainable Development (IGSD).

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