PPT-Measuring the Antarctic Ozone Hole with the new Ozone Mappi

Author : kittie-lecroy | Published Date : 2016-09-02

Natalya Kramarova Paul Newman Eric Nash PK Bhartia Richard McPeters Didier Rault Colin Seftor Gordon Labow OMPS meeting June 6 2013 Objectives Can OMPS reasonably

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Measuring the Antarctic Ozone Hole with the new Ozone Mappi: Transcript

Natalya Kramarova Paul Newman Eric Nash PK Bhartia Richard McPeters Didier Rault Colin Seftor Gordon Labow OMPS meeting June 6 2013 Objectives Can OMPS reasonably represent the Antarctic ozone hole. and verification of the connections between ozone depleting substances and the ozone hole. A.R. (Ravi) Ravishankara. NOAA, ESRL/Chemical Sciences Division. Boulder CO, USA. Co-Chair, SAP. Some . personal . Department of Environmental Sciences. Rutgers University, New Brunswick, New Jersey USA. robock@envsci.rutgers.edu. http://envsci.rutgers.edu/~. robock. . Climate Dynamics. 11:670:461. Ozone Hole Lecture, . 2012. Craig S. Long. 1. Larry Flynn. 2. , Bryan Johnson. 3. NOAA. 1-NWS/NCEP/Climate Prediction Center. 2-NESDIS/STAR/Satellite Meteorology & Climatology Division. 3-OAR/ESRL/Global Monitoring Division. EVSC 1300. Spring 2016. Average. vertical. temperature. structure. of atmosphere. Average. vertical. temperature. structure. of atmosphere. NO. x. + VOCs + sunlight .  . Ground-level ozone. Figure18-9 p528. Or, “We Don’t Do That Anymore”. Our Route to Sustainability. Man Must Subdue Nature. Manifest. Destiny. Get across the continent as fast as we can. John. Muir – “Blow away”. Kill(. er. ) Whales?. . Susan Solomon. Richards Professor of Atmospheric Chemistry and Climate Science, MIT. Based on work with many including Diane Ivy, Justin . Bandoro. - (MIT). Doug . Kinnison. , Mike Mills, Ryan Neely, Rolando Garcia - (NCAR), . 2. Ozone – Two Faces. Troposphere – Bad Ozone. Pollution . Photochemical smog. . Eye irritant. Stratosphere – Good Ozone. Blocks some UV radiation. Hole caused by depletion due. to ODC’s . 9. th. Ozone Research Managers Meeting. Geneva . 14. th. -1. th. . May 2014. Matt Tully. Bureau . of . Meteorology, Australia . 9. th. Ozone Research Managers Meeting. Geneva, 14. th. -16. th. May, 2014. Department of Environmental Sciences. Rutgers University, New Brunswick, New Jersey USA. robock@envsci.rutgers.edu. http://envsci.rutgers.edu/~. robock. . Climate Dynamics. 11:670:461. Ozone Hole . Ozone Depletion(Chapter 25). Ozone Properties. Ozone (O. 3. ). is a triatomic form of oxygen found mostly in the lower half of the atmosphere. Highly reactive strong oxidant. Tropospheric pollutant produced by photochemical reactions. 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.. Stratosphere. Ozone Concentration (ppm). SGC . Fig. 3-11. . OZONE: Sources. Ozone is produced naturally in photochemical reactions in the stratospheric ozone layer --“good ozone” -- is . decreasing. 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 . found?. The . ozone layer . is the layer of the atmosphere at an altitude of 15 to 40 km (stratosphere) . What is Ozone?. Ozone. . is a molecule made of three oxygen atoms. What is the function of the ozone layer.

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