PPT-Investigation of trends in tropical tropospheric ozone colu

satellite data using CCD KlausPeter Heue 1 Melanie ColdeweyEgbers 1 Andy Delcloo 2 Christophe Lerot 3 Diego Loyola 1 Pieter Valks 1 Michel van Roozendael 3 Elpida. tropospheric . ozone integrating recent model developments. Lu Hu . (. luhu@seas.harvard.edu. ). With. . Daniel Jacob, . Xiong. . Liu, Patrick Kim, . Katie Travis, Lin . Zhang . Acknowledgement: Johan . the Upper Troposphere - Lower Stratosphere. K. . Wargan, . S. . Pawson. , . M. . Olsen, . J. . Witte, . A. . Douglass. Global Modeling and Assimilation Office (GMAO). Chemistry and Dynamics Branch. NASA GSFC. P. . J. Young. , V. . Naik. , J. . Brandt, R. Doherty, A. M. Fiore, . A . Gaudel. , C. . . Geels. , M. I. . Hegglin. , L. Hu, U. . Im. , R. Kumar, M. Lin, A. . Luhar. , L. Murray, . J. . Neu. , D. . . 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. . Bureau of Meteorology – R&D Branch. Understanding the causes of . SH tropical expansion. Motivation. 1997-2013 Apr-Sept rainfall deciles. Why do we care about tropical expansion?. SWWA rainfall decline (from 1970s). Ozone Enhancement Due to Lightning . -- Observations and Models. Lihua. Wang. 1. st. TEMPO Applications Workshop. Huntsville, AL. July 12-13, 2016. Introduction. Lightning is a particularly . signifant. YAG Laser and Raman Cells (. A53Q – 0439. ) . J. T. . Sullivan (jsull1@umbc.edu). 1,2. , . T. J. . McGee. 2. , . G. K. . Sumnicht. 2,3. 1. . Department of Atmospheric Physics, University of Maryland Baltimore County (UMBC), Baltimore, MD, United States. . A . community-wide effort to quantify tropospheric ozone in a rapidly changing . world. Owen . Cooper. CIRES, . U. . of Colorado/NOAA Earth System Research . Lab., . Boulder. owen.r.cooper@noaa.gov. TEMPO Science Team Meeting, Harvard-Smithsonian Center for Astrophysics. 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. . – . 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. Undergraduate CoursesFall 2019ScheduleCOURSE TITLENUMBERSECCALLDAY/TIMEPTSSTAFFLOCBASIC LANGUAGE COURSESElementary German IGERM-UA10018543MWF 1100 12154ReichSilver 4060028544TRF930 1045SmithSilver 402 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. 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).