PPT-Tropospheric ozone in global models

P Young V Naik J Brandt R Doherty A M Fiore C Geels M I Hegglin L Hu U Im R Kumar M Lin A Luhar L Murray D A Parrish D Plummer H E Rieder J Rodriguez J L Schnell M Schultz S . 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?. Tropospheric ozone observations. . Chapter Writing Team . (contributors so far):. . D. . Tarasick. (Lead), . I. . Galbally. (Co-Lead), G. . Ancellet. , A. . . Boynard. , . P. . Cristofanelli. , M. Coyle, A. newest Activity. :. Tropospheric Ozone Assessment Report (TOAR). Global metrics for climate change, human health and . crop/ecosystem research. Owen R. Cooper . CIRES, University of Colorado, Boulder, USA . Foreman Room 102. 1. Global Warming and Ozone Depletion take place in two different layers of the atmosphere: . Global Warming. Ozone . Depletion. Global Warming vs. Ozone Depletion: Causes. Global Warming: cars, factories, rice farming, landfills: . Updates from . PSU/GSFC/UMD. : Comparisons with . Observations. Anne Thompson, NASA-GSFC. 5 Jan 2015. Nikolay . Balashov (PhD Candidate) . & Greg Garner (Prof G. Young). All at PSU. Background & Principles of PSU/GSFC/UMD AQ Forecasting with Value of Information. Dalon Stone, Kenneth Bowman, Cameron Homeyer. - Texas A&M. Laura Pan, Simone Tilmes, Doug Kinnison - NCAR. Elliot Atlas - U. of Miami. START08 Project Team. UTLS Workshop, NCAR. 2009-10-20. START08 Field Campaign. NDACC . Lidar. Working Group Meeting. , NASA/JPL, Table Mountain, . CA, Nov. 5, 2013. http://nsstc.uah.edu/atmchem/. Shi . Kuang. 1. , Mike . Newchurch. 1. , . John Burris. 2. , Wesley Cantrell. 1. . Measurements indicate high ozone concentrations in the Great Basin.. Back trajectory analysis and satellite remote sensing will be used to shed light on the causes.. Great Basin National Park: 39.005 N 114.216 W.. – . what . else besides climate change. Daniel J. Jacob. Group photo (2013). Range of tropospheric chemistry problems. LOCAL . < 100 km. REGIONAL. 100-1000 km. GLOBAL. > 1000 km. Urban smog. 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.. . . Xiong. Liu and Kelly Chance. July 23, 2013. xliu@cfa.harvard.edu. Outline. Introduction. Ozone Profile and Tropospheric Ozone Algorithm: current implementation (OMI) and its adaption to TEMPO. Applications. Development of an Aura Chemical Reanalysis in support Air Quality Applications. R. Bradley . Pierce. (NOAA/NESDIS/STAR). Allen . Lenzen. , Todd . Schaack. . (UW-Madison SSEC). Project . Diego Loyola, German Aerospace Center (DLR). WMO/UNEP ORM 11 part 2. Virtual Meeting, July 21. st. , 2021. 2. CEOS AC-VC Introduction. Total Ozone Activities. Tropospheric Ozone Activities. Outlook. 3. 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).