PDF-Correcting the MSU Middle Tropospheric Temperature for Diurnal Drifts

Fig 1 Example simulated MSU Channel 2 diurnal cycles calculated fromhourly CCM3 output These diurnal cycles are for the month of June aand c are for a 25 x 25degree box in the tropical P. Peter J Minnett, Robert H Evans and . Gui. Podestá. Meteorology and Physical Oceanography. Rosenstiel School of Marine and Atmospheric Science. University of Miami. Overview. Sea-surface temperature (SST) as an Essential Climate Variable (ECV), and Climate Data Record (CDR). 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. Qian Tan (USRA), . Mian. Chin (GSFC), Jack Summers (EPA), Tom Eck (GSFC), . Hongbin. Yu (UMD), . Caterina. . Tassone. (NOAA. ), Yan Zhang (MSU), . EPA/AQS, NASA/AERONET, NOAA/NCDC . Outline. Diurnal variability of surface PM2.5. precipitation variability over the Gulf Stream and . the Kuroshio. Shoshiro Minobe . and Shogo . Takabeyashi. (Hokkaido University, Sapporo, Japan) . Outline. . Introduction. . Global View. . Gulf Stream . 2. Emissions during . CalNex. -LA: Magnitude and Sources. Sally . Newman. 1. , . Xiaomei. Xu. 2. , Sergio Alvarez. 3. , Bernhard Rappenglueck. 3. , Christine Haman. 3. , Barry Lefer. 3. , Charles Miller. 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. spectroradiometry. . Peter J Minnett. Meteorology and Physical Oceanography. Rosenstiel School of Marine and Atmospheric Science. University of Miami. 2. What is SST?. The infrared emission from the ocean originates from the uppermost <1mm of the ocean – the skin layer.. 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. . – . 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. 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. 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). x. . and NO. x. emissions over North America. . Daniel Jacob, Viral Shah, . Ruijung. Dang, Laura Yang. Shah et al., in prep.; Dang et al., in prep.. Lowest 2 km contributes only 30% of tropospheric NO.