PPT-Diurnal Variability of Aerosols Observed by Ground-based Ne

Author : lindy-dunigan | Published Date : 2016-03-26

Qian Tan USRA Mian Chin GSFC Jack Summers EPA Tom Eck GSFC Hongbin Yu UMD Caterina Tassone NOAA Yan Zhang MSU EPAAQS NASAAERONET NOAANCDC Outline Diurnal

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Diurnal Variability of Aerosols Observed by Ground-based Ne: Transcript

Qian Tan USRA Mian Chin GSFC Jack Summers EPA Tom Eck GSFC Hongbin Yu UMD Caterina Tassone NOAA Yan Zhang MSU EPAAQS NASAAERONET NOAANCDC Outline Diurnal variability of surface PM25. in . Near. -Surface Salinity. Kyla Drushka. 1. , . Sarah . Gille. 2. , Janet . Sprintall. 2. . kdrushka. @. apl.uw.edu. 1. Applied . Physics Lab, Univ. of . Washington . 2. Scripps Inst. of Oceanography. of . Salinity. Kyla Drushka. 1. , . Sarah Gille. 2. , Janet Sprintall. 2. . kdrushka@apl.uw.edu. 1. Applied Physics Lab, Univ. of Washington . 2. Scripps Inst. of Oceanography. Aquarius Science Team Meeting. Carl Mears. Remote Sensing Systems. Why do we care about . the diurnal cycle?. Most polar orbiting satellites drift in local measurement time – need estimate of diurnal cycle to adjust for this.. Model validation studies. Yu-Fen Huang. Hendricks E. A., B. d. . Mcnoldy. , and Wayne H. Schubert. Introduction. TC intensity change is caused by environmental, oceanic, and internal dynamical factors. (Wang and Wu 2004). . An important internal process is the dynamic instability. . Seasonal . V. ariations . of . Nitrogen . O. xides Within . S. nowpack . A. ir . and the . Overlying . A. tmosphere . at Summit, Greenland. C. Toro. 1. , R.E. Honrath. 1. †. , L.J. Kramer. 1. , D.Helmig. S. . Fadnavis, . K. . Semeniuk, . L. . Pozzoli, . M. G. . Schultz, . S. D. . Ghude, . S. . Das. ACP, 2013. CO2, CO, VOCs, BC, SO2,NOX …….. . CO2. CO. H2O. PAN. BC. CH4. OC. SO2. NOX. HCN. Emission: . in Hainan Island. Lei Zhu. Paul . Markowski. , . Zhiyong. . Meng. and . Fuqing. Zhang. Research purpose. T. ry to understand the climatology . of . diurnal. . precipitation cycle in Hainan Island. Oliver Elison Timm ATM 306 Fall 2016. Information. ATM 306 . ES 232. Schedule. Monday, Wednesday. 11:00am-12:20pm. Office hours:. Mon 12:30-1:30pm. Thu 9:15-10:15am. Or by appointment. Contact. oelisontimm@albany.edu. Circulations in the ABL, and the MJO . Richard H. Johnson. Colorado State University. West Pacific Warm Pool, early Dec 1992 (. Xin. Lin). & Paul . Ciesielski. , Jennifer . Cotturone. , Andy Newman, Brian . Technical Issues. Side Event. Bangkok, 21. st. April 2015. Dr. . Helen Tope. Principal Consultant,. Energy International Australia. and. Co-Chair Medical Technical Options Committee. Disclaimer: The . Luke Oman. luke.d.oman@nasa.gov. SAGE III/ISS STM – Oct. 30, 2019 . 1. Luke Oman. 1. , Sarah Strode. 1,2. , . Ghassan Taha. 1,2. , and Mark Schoeberl. 3. 1. NASA/GSFC, Greenbelt, MD, USA. 2. University Space Research Association, Columbia, MD, USA. over Sumatra Island, Indonesia, on. synoptic disturbances and its relation to. the Madden-Julian Oscillation. Ayako SEIKI, Satoru YOKOI, and Masaki KATSUMATA. (JAMSTEC, Japan). Seiki et al. (2021), JMSJ. 1. Mian Chin. NASA Goddard Space Flight Center, USA. Huisheng. . Bian. University of Maryland at Baltimore County/NASA GSFC, USA. Qian Tan. Bay Area Environmental Research Institute/NASA Ames, USA. Ghassan Taha. Use NOAA Unique Combined Atmospheric Processing System (NUCAPS) Satellite Soundings to observe the tropical cyclone (TC) diurnal cycle. infrared (IR) and microwave (MW) soundings. Three case studies: Hurricanes Dorian (2019), Florence (2018), Irma (2017).

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