PPT-Diurnal radiation cycle impact on the genesis of Hurricane Karl (2010)

Christopher Melhauser and Fuqing Zhang The Pennsylvania State University Department of Meteorology Group Meeting April 11 2013 Focus How does the diurnal radiation cycle impact the . Dea Doklestic . G&G 570 Class . Project. Heat Budget Group Presentation, June 16, 2011. Questions. How do clouds influence surface heat budget?. How are turbulent heat fluxes influenced during overcast conditions?. 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. ITCZ changes and radiatively forced warming. in . aquaplanet. simulations. Timothy . Merlis. , Ming Zhao, and Isaac Held. Motivation/Approach. Most modeling . studies . project decreases . in the globally averaged frequency of tropical . 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 . 1 2SAB and the U S Air Force Weather Agency AFWA Microwave satellite imagery from NOAA polar-orbiting satellites the NASA Tropical Rainfall Measuring Mission TRMM the NASA QuikSCAT the NASA Aqua the 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. . 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. 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.