PPT-Estimating smoke emission using GOES satellite observations and HYSPLIT model
Author : marina-yarberry | Published Date : 2018-11-09
Tianfeng Chai 123 Hyuncheol Kim 123 and Ariel Stein 1 1 NOAAOARAir Resources Laboratory ARL 2 Cooperative Institute for Climate amp SatellitesMaryland CICSMD
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Estimating smoke emission using GOES satellite observations and HYSPLIT model: Transcript
Tianfeng Chai 123 Hyuncheol Kim 123 and Ariel Stein 1 1 NOAAOARAir Resources Laboratory ARL 2 Cooperative Institute for Climate amp SatellitesMaryland CICSMD 3 University of Maryland College Park MD. Useful reviews:. Waxman astro-ph/0103186. Ghisellini astro-ph/0111584. Piran astro-ph/0405503. Meszaros astro-ph/0605208. Useful links. http://www-astro.physics.ox.ac.uk/~garret/teaching/. http://www.cv.nrao.edu/course/astr534/. x. emission estimates using multiple species data assimilation with GEOS-. Chem. . adjoint. model. Xuesong Zhang, Dylan B. A. Jones, Martin Keller, Thomas W Walker, . Zhe. Jiang, Daven K . Henze. Judy Racusin. Penn State University. 2008 Nanjing GRB Workshop, Nanjing, China, June 23-27. Broadband Observations of the Extraordinary . Naked-Eye GRB 080319B. . J. L. . Racusin. , S.V. . Karpov. , M. . 5. th. TEMPO Science Team Meeting, Cambridge, MA. June 1, 2017. Sara M. Strachan. Idaho Dept. of Environmental Quality. sara.strachan@deq.idaho.gov. Wildfire smoke and air quality . forecasting: What we do . Tribal Air Monitoring Support Center. g. lenn.gehring@nau.edu. 541-612-0899. Hy. brid . S. ingle-. P. article . L. agrangian . I. ntegrated . T. rajectory model . WHAT??. I think I’ll call it . HYSPLIT. AQAST:. David Streets (ANL), Greg Carmichael (U. Iowa), Ben de Foy (Saint Louis U.), Russ Dickerson (U. Maryland), David Edwards (NCAR), Daven Henze (U. Colorado), Daniel Jacob (Harvard U.), Yang Liu (Emery U.), Zifeng Lu (ANL), Gabriele Pfister (NCAR). Using . the Navy Coastal Ocean Model . (. NCOM) 4D-VAR. Matthew J. Carrier, Hans E. Ngodock, . Scott . R. . Smith, Innocent . Souopgui. , and Brent Bartels. U.S. Naval Research Laboratory. Stennis Space Ctr., MS. Glenn . Rolph. OAR Air Resources Laboratory. June 21, 2016. Background Information. ARL Science Review, June 21-23, 2016. 2. ARL supports the 122 local National Weather Service’s Weather Forecast Offices (WFOs) with HYSPLIT atmospheric dispersion products to assist them with their decision support role in the local community.. What is observation?. Observations are made in science. They are made by using: . The 5 Senses . Taste. Smell. Touch. Hear . See . Two types of Observation. Qua. l. itative. Qua. n. titative. 1. Qualitative . . Tianfeng. Chai. 1,2. , Alice Crawford. 1,2. , Barbara Stunder. 1. , Roland Draxler. 1. , Michael J. Pavolonis. 3. , Ariel Stein. 1. . NOAA Air Resources Laboratory, College Park, MD. Cooperative Institute for Climate and Satellites, University of Maryland, College Park, Maryland. 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. M. embers:. Daniel Jacob (Harvard), lead; Arlyn Andrews (NOAA/ESRL); David Baker (CSU); Kevin Bowman (JPL); Riley Duren (U. Arizona); Randy Kawa (NASA/GSFC); Thomas Lauvaux (Penn State); Steve Lohrenz (U Mass Dartmouth); Thomas Nehrkorn (AER), Lesley Ott (NASA/GSFC), Ben Poulter (NASA/GSFC), Lisamarie Windham-Myers (USGS). the Indonesia 2015 peat fire season case study. Antonio G. Bruno. 1,2. , Jeremy J. Harrison. 1,2. , David P. Moore. 1,2. , Martyn P. Chipperfield. 3,4. , and Richard . J. Pope. 3,4. 1. University of Leicester, School of Physics and Astronomy, Leicester, UK (. Background:. In the past two decades, improved measurements of acceleration due to gravity have allowed for accurate detection of temporal gravity change. Terrestrial gravimeters can sense changes of gravity induced by elevation or mass changes, including local effects that may bias regional studies. Satellite instrumentation can detect large scale mass changes on a regular basis. The minimum resolution of the GRACE satellite is about 400 km, which is too large for the size of most, direct regional studies. Also, satellites are limited by their life of deployment. Both techniques can be scaled to (in)validate change models generated from other geophysical observations including water storage (underground and glacial), geoid definition, isostatic adjustments and tectonic activity. .
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