PPT-Diurnal Cycle Modeling Related to SAGE III/ISS Products

Luke Oman lukedomannasagov SAGE IIIISS STM Oct 30 2019 1 Luke Oman 1 Sarah Strode 12 Ghassan Taha 12 and Mark Schoeberl 3 1 NASAGSFC Greenbelt MD USA 2 University Space Research Association Columbia MD USA. 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. Liu et al. 2010. Review By: . Gus . Alaka. and Doug . Stolz. 20 February 2014. ATS 780. Background. C. T. R. Wilson’s Hypotheses: . Thunderstorms . AND. electrified shower clouds are the “batteries” of the global DC electrical circuit. Adopted (with permission) and later tested by F. Whipple.. Kaustav. . Chakravarty. Richard H. Johnson. Paul E. . Ciesielski. Colorado State University. J. L. Davison. University of Louisville. Third Symposium on Prediction of the Madden-Julian Oscillation: Processes, Prediction and . 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?. 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. 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 . Tang, S., P. . Gleckler. , S. . Xie. , J. Lee, C. Covey, C. Zhang, M.-S. . Ahn. , 2021: Evaluating Diurnal and Semi-Diurnal Cycle of Precipitation in CMIP6 Models Using Satellite- and Ground-Based Observations. . of the UM in different parts of the world.. Humphrey Lean, Kirsty Hanley, Stuart Webster, Will Keat, Thorwald Stein, Todd Lane, Martin Jucker, Elizabeth Kendon and Giorgia Fosser. Met Office has run 1.5km UK version of Unified Model for about 10 years (UKV). . Shuaiqi Tang. Pacific Northwest National Laboratory, Richland, WA, USA. 6/18/2022. Collaborators: Shaocheng Xie, Cheng Tao, Hsi-Yen Ma, and many others. Outline. Common issues in simulating diurnal cycle of precipitation (DCP) . Claire . Bulgin. University. of Reading, National Centre for . Earth. Observation. Background. Every measurement we make (both in-situ or remotely sensed) deviates from the ‘true’ surface temperature due imperfections in the instrumentation and measurement process. Therefore, in order to use the data correctly, you must consider the uncertainty in the measurement.. 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.