PPT-Climate-Driven Changes in Tropospheric Oxidant (O

3 HO x Abundances GlacialInterglacial Rapid Climate Change Glacial     Modelbased hypothesis During large climate transitions variability in the O 3 HO x ratio is determined by . 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 134CHAPTER13.ASTROPHYSICALJETSwinds:jetsmightbepressure-driven,radiation-driven,Alfven-wave-driven,orshock-driven.Nooneissurehowjetsarecollimated;bythetimetheyarevisibletoobservers,theyarealreadytight 1979–2010). ~3 STCs/year. Strong TT . Weak TT . Trough induced . N = 105. STC Climatology (. 1979–2010). N = 34. Strong TT . Weak TT . Trough induced . STC Climatology (. 1979–2010). N = 56. Strong TT . 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. 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 . 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. Sueper. Jimenez Group, CU Boulder, . April . 1, 2014. 1. 2. The main output of the OFR panel are, in general two plots: the relative and absolute oxidation enhancement as a function of oxidation age/OH enhancement.. – . 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. Climate prediction is coming of age?. El Nino. + Southern Oscillation. = ENSO. Man induced climate change. Impacts on Water Resources may be significant. Changed Climate. Advanced Warning. Goal?. A basic quantitative understanding of how the global climate system works, to allow informed assessment of climate based forecasts and their role in hydrology and water resources systems.. . . 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.