PPT-Diurnal changes in turbulent Statistics

EFD Final Project Terrence Hess Daniel Alexander Mohammad Khan Neil Lareau 1 21 Apr 2011 Project Objectives Characterize the diurnal evolution of turbulent statistics for two dissimilar 24 hour periods. 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. 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. 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. . and. idealized glass . Shin-. ichi. . Sasa. 　（. Kyoto University). . . . 　. 　　　　　　　　　　　　 　　. 1. (ME EN 7960-. 003). Prof. Rob Stoll. Department of Mechanical Engineering. University of Utah. Fall 2014. Vorticity: or. Turbulent Flow Properties. Why study turbulence? Most real flows in engineering applications are turbulent. . (ME EN 7960-008). Prof. Rob Stoll. Department of Mechanical Engineering. University of Utah. Spring 2011. Vorticity: or. Turbulent Flow Properties. Why study turbulence? Most real flows in engineering applications are turbulent. . Richard H. Johnson. Colorado State University. T. . Ushiyama. (Andy . Newman , Brian . McNoldy. , and Paul . Ciesielski. ). MAHASRI/. HyARC. workshop, 5-7 March 2009, . DaNang. , Vietnam . Why do we care about the diurnal cycle?. the Impact of Islands on the Tropical Climate. Timothy W. . Cronin*, Kerry A. Emanuel. Program in Atmospheres, Oceans, and Climate, Massachusetts . Institute of . Technology. 77 . Massachusetts Avenue, Cambridge . 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 . 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.