PPT-Cyclones

What is a cyclone A cyclone is a violent rotating storm They are called hurricanes or typhoons in the northern hemisphere What conditions form cyclones Warm t ropical waters fuel the storms and . Historical Background The practice of naming storms tropical cyclones began years ago in order to help in the q uick identification of storms in warning messages because names are presumed to be far easier to remember than t Quantification for insurance and reinsurance. Andreas Schraft, Head Catastrophe Perils. Why insurers and reinsurers need catastrophe models . 2. loss payment. saves. capital. provides . capital. Insurer/reinsurer needs to ensure that:. Current Status. Institutions involved in Coastal Zone Management. Current Concerns. Current Policies, Programs and Projects. Likely implications of Climate Change on Coastal Zone. Strategies for Adaptation. 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. and the Possible Application to Equable Climates 12.842 Climate Physics and Chemistry Term Project Allison Wing Tropical cyclones are undoubtedly among the mostly deadly and destructive natural phen Fig. 2 shows the largest spatial differences occur between the older JRA-25 reanalysis when compared with the newer high resolution reanalyses (ERA-Interim) (top), particularly in the Southern Hemisphere (top right).. the Marine Boundary Layer. Henry Potter & Tripp Collins. Raphael Ramos, Neil Williams, Will . Drennan. , Hans Graber. Abstract. Materials & Methods. Results. Conclusions. Objectives. Future Work. ATMO 1300. Summer II . 2017. Extra-Tropical Cyclones and Anticyclones, Chapter 10. ATMO 1300. Summer II 2016. Norwegian Cyclone Model. Midlatitude. Cyclone Lifecycle. Strengthening and failure mechanisms. By Rick . Garuckas. and Andrew . Calvi. Role of Mid-latitude Cyclones. Reduce temperature gradients/. baroclinicity. .. Convert potential energy to kinetic energy . . 1. Although these processes bring the atmosphere closer to a balanced state, a perfectly balanced state is never achieved. . Geography of storm names. Atlantic . and eastern Pacific. : . “hurricanes” . Indian Ocean and Australia: . “cyclones”. Western Pacific, N. hemisphere: . “typhoons”. Western Pacific typhoons, 2011 . What are cyclones?. This . is . important . when we're talking about ocean storms because the location of the storm determines what we call it. I. f . the storm occurs in the Atlantic Ocean and Northeast Pacific, it's called a hurricane. If the exact same type of storm occurs in the Northwest Pacific, this is a typhoon. And if we find those same storms in the South Pacific and Indian Ocean, these are called tropical cyclones. . Are there any patterns on the wind direction animation?. Using evidence from the Sea Surface Temperature and Wind Speed map can you say why we get ocean currents?. Ocean currents and sea surface temperature . Review. For Next Class: . Study!! Bring a #2 pencil.. Extratropical Cyclones. Where are favored locations for extratropical cyclone formation in the contiguous U.S.?. Climatically Favored . Regions . A.V. Soloviev. 1. , C.W., B. Vanderplow. 1. , R. Lukas. 2. 1. Nova Southeastern University, Dania Beach, Florida, USA. 2. University of Hawaii, Honolulu, Hawaii, USA. 7 May 2020. EGU 2020 (online). Motivation.