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 . Lecture 3: Dynamics.. Earnings. Drug announcements. News. Mike Lipkin. Columbia University (IEOR). 134CHAPTER13.ASTROPHYSICALJETSwinds:jetsmightbepressure-driven,radiation-driven,Alfven-wave-driven,orshock-driven.Nooneissurehowjetsarecollimated;bythetimetheyarevisibletoobservers,theyarealreadytight Intercomparison. Project (. GeoMIP. ). Giovanni . Pitari. . V. Aquila, . S. . Tilmes. , . I. . Cionni. , N. De Luca, Di . Genova. , and D. . Iachetti. Participating Models. Source of . geoengineering. 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 . 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. 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 . 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. 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 . 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. 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.. Climatology. is . the study of Earth’s climate and the factors that affect past, present, and future climatic changes.. Climate describes annual variations of temperature, precipitation, wind, and other weather factors.. Driven Well Construction Features Assembled lengths of two inches to three inches diameter metal pipes are driven into the ground A screened well point located at the end of the pipe helps drive the Examples of the both fine-scale and larger-scale signature of climate and climate history include:. Effect of differences in climate on landforms . Relict . topography formed by now inactive . processes.. . . 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.