PPT-Tropospheric

ozone retrieval from uv vis spectrometery RAL Space Remote Sensing Group Richard Siddans Georgina Miles Brian Kerridge Barry Latter 21 st May 2014 TEMPO 2 nd Science Meeting Hampton VA. Table 2.1: SubstanceLife�me Descrip�on / SourcedioxideDecades to centuries about 20 per cent will persist for many No single life�me can be de�ned for carb Global distribution and radiative forcing Owen R. Cooper CIRES U. of Colorado/NOAA ESRL 1. Global distribution of troposphericozone 2. The increase of ozone since preindustrialtimes 3. Present and fu Fig. 1. Example simulated MSU Channel 2 diurnal cycles calculated fromhourly CCM3 output. These diurnal cycles are for the month of June. (a)and (c) are for a 2.5 x 2.5-degree box in the tropical P Intercomparison. Project (. GeoMIP. ). Giovanni . Pitari. . V. Aquila, . S. . Tilmes. , . I. . Cionni. , N. De Luca, Di . Genova. , and D. . Iachetti. Participating Models. Source of . geoengineering. instantaneous. linkages . between . cloud . vertical. . structure and . large. -scale climate . Ying Li. Colorado State University. Merged CALIPSO. /. CloudSat data. (. 2B-GEOPROF-LIDAR . product; June 2006–April 2011. Randall Martin. with . contributions from. Shailesh. . Kharol. , . Gray . O’Byrne, . Akhila. . Padmanabhan. , . Aaron van . Donkelaar. . 2013 China Emissions . Workshop, Beijing. 28 June 2013. Lok. Cohen et. al, 2007: Journal of Climate, 20, 5335-. 5343. Adam Turchioe 2 Dec 2013 ATM 525. Introduction. Stratosphere. -Troposphere annular-mode events are always preceded by an anomalous lower-stratospheric planetary wave activity flux, but lower-tropospheric wave activity signatures of these events are more difficult to find. 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 . Diabatic. Energy. . Sources. Baroclinic. Energy Sources. Adapted from Fig. 9 in . Beven. (2012). 30. th. Conference on Hurricanes and Tropical Meteorology. TCs. Subtropical cyclones. Frontal cyclones. 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. regime. Mitigation potential, incentives and strategies. Increased scientific and political attention. What are short lived climate forcers?. Source: . UNEP/WMO (2011. ) . Integrated Assessment of Black Carbon and Tropospheric . 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.