PPT-Influence of local and remote SST on North Atlantic tropical cyclone potential intensity

Suzana J Camargo Mingfang Ting and Yochanan Kushnir LDEO Columbia University GloDecH Meeting OCP LDEO December 14 2011 Atlantic PDI power dissipation index V 3 max . Satellite cl oud imageries are used along with other meteorological features to estimate t he intensities and the wind speed associated with these intense systems The satellite cl oud configurations expressed by T numbers have unique relati onship w 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. By. Dr. Mukta . Paliwal. CSE, IIT Bombay. Introduction. Tropical cyclones are low pressure systems that have thunderstorm activity and rotate counterclockwise.. Tropical cyclones form over all tropical oceanic areas except the South Atlantic and the Southeast Pacific. . 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, . Ethan Wright: UNC Asheville. Research Advisor: . Dr. Christopher . Hennon. 04/22/2015. Peak Intensity: 190 mph. Lowest Pressure: 870 . mb. Small eye size of 8 nm . Super Typhoon Tip (1979). Super Typhoon Winnie (1997). Madeline Frank. EAS 4480. Course Project. April 2016. Goals. 4 Ocean Basins:. . North Atlantic, East Pacific, West Pacific, . Indian. Determine the relationship (if any) between active and/or inactive tropical cyclone years among 4 Ocean basins. 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. 2223 May 2021 3 August 2021 NASA/TERRA MODERATE RESOLUTION IMAGING SPECTRORADIOMETER MODIS IMAGERY OF SUBTROPICAL STORM ANA AT 1507 UTC 22 MAY 2021 IMAGE COURTESY OF NASA EOSDIS WORLDVIEW Ana origina Nenad. . Leder. Faculty of Maritime Studies, . Ruđera. . Boškovića. 37, 21000 Split, Croatia, nenad.leder@pfst.hr. Zvonimir . Lušić. Faculty of Maritime Studies, . Ruđera. . Boškovića. 37, 21000 Split, Croatia. Past, Present, and Future Tropical Cyclone Activity Jacob Carstens 1 , Christopher Uejio 2 , and Allison Wing 1 1 Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallaha Why Should You Care? Forecasting Much progress in social science of response to warnings, requests to evacuate, etc. Forecasters are ambassadors to meteorology Opportunity to inform public Knowledge o Kerry Emanuel. Lorenz Center, MIT. . Motivations. Most current TC risk models are based on statistical algorithms for generating synthetic tracks and associated wind fields. . Statistical . T. Kerry Emanuel. Program in Atmospheres, Oceans, and Climate. MIT. Some Issues. What processes control rates of genesis of tropical cyclones?. What processes control the actual and potential intensity of TCs? . Kerry Emanuel. Lorenz Center. Department of Earth, Atmospheric, and Planetary Sciences, MIT. Program. Overview of hurricanes. Basic theory of hurricanes. What have hurricanes been like in the past, and how will they be affected by global warming?.