PPT-The Diurnal Cycle of Tropical and Monsoon Convection
Author : min-jolicoeur | Published Date : 2017-07-31
Richard H Johnson Colorado State University T Ushiyama Andy Newman Brian McNoldy and Paul Ciesielski MAHASRI HyARC workshop 57 March 2009 DaNang Vietnam
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The Diurnal Cycle of Tropical and Monsoon Convection: Transcript
Richard H Johnson Colorado State University T Ushiyama Andy Newman Brian McNoldy and Paul Ciesielski MAHASRI HyARC workshop 57 March 2009 DaNang Vietnam Why do we care about the diurnal cycle. 3D Structure. Let’s Talk Genesis!. Review. Nolan, . Rappin. , and . Emanuel 2007; . Khairoutdinov. . and Emanuel 2013; . Zhuo. , Held, and Garner 2014. : TC genesis can occur on f-plane . without. extratropical. circulation. Steven Feldstein and Michael Goss. The Pennsylvania State University. IUGG, Prague, June 25, 2015. Questions. :. . 1. . What is the relationship between interference, Arctic sea ice, and tropical convection and how does it impact the . 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. vs. . Remote effect. Sourav Taraphdar. 1. Collaborators. :. 1. . Fuqing. Zhang, . Yonghui. . Weng. , Michael (Yue) Ying. 2. . Shuguang. Wang. 3. Juan . Fang. 1. Department of Meteorology, The Pennsylvania State University, . 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 . Let’s Talk Genesis!. Review. Nolan, . Rappin. , and . Emanuel 2007; . Khairoutdinov. . and Emanuel 2013; . Zhuo. , Held, and Garner 2014. : TC genesis can occur on f-plane . without. . a pre-existing cyclonic disturbance through:. C. yclone . A. ctivity . M. ediated by the African Monsoon. Objective. Quantify the impacts of North . Atlantic . & Mediterranean . (NAMED) . sea surface temperature (SST) on Atlantic tropical cyclone (TC) activity. 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. 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). . 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. GOES infrared . b. rightness temperatures (BT) . are . used to . objectively identify . overshooting tops in tropical . convection (TOTs). TOT heights are . assigned using TOT BT and NWP . profiles.. 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) . 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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