PPT-Isoprene emissions in Africa inferred from OMI HCHO

Author : luanne-stotts | Published Date : 2016-12-21

Eloïse Marais emaraisfasharvardedu D Jacob T Kurosu K Chance J Murphy C Reeves G Mills S Casadio D Millet M Barkley F Paulot J Mao AMS Conference Boston

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Isoprene emissions in Africa inferred from OMI HCHO: Transcript


Eloïse Marais emaraisfasharvardedu D Jacob T Kurosu K Chance J Murphy C Reeves G Mills S Casadio D Millet M Barkley F Paulot J Mao AMS Conference Boston. On that day the very 64257rst compliance period for the Qu57577bec cap and trade system began From now on businesses subject to the system must take into account the cost of emitting carbon in their decisionmaking process What is a cap and trade sys OMI cloud optical depth contributes to the observed positive bias in surface UV. Anders V. . Lindfors, . T. . . Mielonen. , M.R.A. . Pitkänen. , . A. . . Arola. , J. . Tamminen. Finnish Meteorological Institute. Min Huang. (. min.huang@jpl.nasa.gov. ), . K. W. Bowman (JPL), G. R. Carmichael (U Iowa), . M. Lee (JPL), D. K. . Henze. (CU-Boulder), T. Chai (NOAA/ARL) . A. J. . Weinheimer. (NCAR), R. C. Cohen (UC Berkeley). by oversampling of OMI data: Implications for TEMPO. Lei Zhu and Daniel J. Jacob. HCHO observations from space constrain emissions. of highly reactive volatile organic compounds (HRVOCs). HRVOCs. HCHO. Terpenes. are a large and diverse class of organic compounds, produced by a variety of plants, particularly conifers,. . though also by some insects. They are often strong-smelling. They may protect the plants that produce them by deterring parasites.. Jingqiu Mao (Princeton/GFDL). Yale University, 02/20/2014. Acknowledgement. Measurements: . William Brune (Penn State), Xinrong Ren (NOAA/UMD). Modeling: . Fabien Paulot (Harvard), Daniel Jacob(Harvard), Ron Cohen (UC Berkeley), Paul Wennberg(Caltech), Larry Horowitz(GFDL). .. urban . NO. x. emissions . from . Ozone Monitoring Instrument (OMI) satellite retrievals. Zifeng Lu, David G. Streets. Decision and Information Sciences Division. Argonne National Laboratory. Presented . Jhoon Kim. 1. , M.J. Kim. 1. , K. J. Moon. 2. GEMS Science Team. 3. , GEMS Program Office. 2.  . 1 . Department of Atmospheric Sciences, . Yonsei. University. 2. National Institute of Environmental Research, Ministry of . Eloïse. Marais . (emarais@fas.harvard.edu). 1. , . Daniel Jacob. 1. , Jennifer Murphy. 2. , Dylan Millet. 3. , Thomas Kurosu. 4. , Kelly Chance. 4. 1. Earth and Planetary Sciences, . Harvard . University, . Measurements of Volcanic SO. 2. Emissions into the UTLS. . Simon A. Carn. 1. ,. Kai Yang. 2,3. , . Nickolay. A. Krotkov. 3. , and Fred . J. . Prata. 4. . Michigan Technological University, Houghton, MI, USA. ACKNOWLEDGEMENTS: . . This work was funded by the . NASA ACMAP program and the South African National Research Foundation. OMI slant column (SC) HCHO. (original data for 2005-2009 at 1. Chem. . adjoint. model. Xuesong Zhang, Dylan B. A. Jones, Martin Keller, Thomas W Walker, . Zhe. Jiang, Daven K . Henze. , Adam E Bourassa, D A . Degenstein. and Yves J . Ronchon. IGC8. , May 2, 2017. 2. observations and the role of the upper troposphere. Rachel Silvern. Atmospheric Chemistry Modeling Group, Harvard University. TEMPO Science Team Meeting. June 7, 2018. Previous work showed 60% reduction of . years of global observations and comparison to ground-based and satellite data. DOAS workshop 2015, Brussels, July 2015. N. Theys. 1. ,. . I. De Smedt. 1. , . J. van . Gent. 1. , T. Danckaert. 1. , F. Hendrick.

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