Haiyan and Haima typhoons: Characteristics During Formation, Maturation and Dissipation

Tropical cyclones that have wind intensity equal or higher than 119 km/h, when formed in the western sector of the tropical Pacific Ocean, are called typhoons. These systems are responsible for great devastation over continental areas. Two cases that reached the Philippines and attracted the inter...

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Main Authors: Bruna Andrelina Silva, Rayan Reis Miranda Leite, Michelle Simões Reboita
Format: Article
Language:English
Published: Universidade Federal do Rio de Janeiro 2018-12-01
Series:Anuário do Instituto de Geociências
Subjects:
Online Access:http://www.anuario.igeo.ufrj.br/2018_03/2018_3_37_53.pdf
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author Bruna Andrelina Silva
Rayan Reis Miranda Leite
Michelle Simões Reboita
author_facet Bruna Andrelina Silva
Rayan Reis Miranda Leite
Michelle Simões Reboita
author_sort Bruna Andrelina Silva
collection DOAJ
description Tropical cyclones that have wind intensity equal or higher than 119 km/h, when formed in the western sector of the tropical Pacific Ocean, are called typhoons. These systems are responsible for great devastation over continental areas. Two cases that reached the Philippines and attracted the international attention were the typhoons Haiyan and Haima. Haiyan was the strongest typhoon recorded since 1979 in the western Pacific and remained active from 3 to 11 November 2013. Haima was the second typhoon that reached winds with an intensity exceeding 220 km/h since 1979. The purpose of the present study is to describe the evolution of the lifecycle of Haiyan and Haima typhoons (lagrangian analysis), to show similarities and differences between them, and to evaluate the impact of these systems on atmospheric variables close to the Philippines (eulerian analysis). The atmospheric variables used in the study were obtained from the Global Forecast System Analysis and the Tropical Rainfall Measuring Mission. The cyclogenesis region of the Haiyan and Haima typhoons showed positive sea surface temperature anomalies of 0.7 °C and 1.1 ° C, respectively. Along the trajectory, the typhoons produced a cold trail on the ocean. Near the Philippines, the Haiyan caused winds with an intensity of 232 km/h and the Haima of 226 km/h. Regarding the lifecycle of these systems, the maturation phase shows more intense cyclonic relative vorticity and the highest zonal departure of air temperature in the core of the typhoons in relation to the neighborhood
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spelling doaj.art-d2518e62e7e9465caad4346650d89dca2023-01-02T19:40:51ZengUniversidade Federal do Rio de JaneiroAnuário do Instituto de Geociências0101-97591982-39082018-12-014133753http://dx.doi.org/10.11137/2018_3_37_53Haiyan and Haima typhoons: Characteristics During Formation, Maturation and DissipationBruna Andrelina Silva0Rayan Reis Miranda Leite1Michelle Simões Reboita2Universidade de Federal de ItajubáUniversidade de Federal de ItajubáUniversidade de Federal de ItajubáUniversidade de Federal de ItajubáTropical cyclones that have wind intensity equal or higher than 119 km/h, when formed in the western sector of the tropical Pacific Ocean, are called typhoons. These systems are responsible for great devastation over continental areas. Two cases that reached the Philippines and attracted the international attention were the typhoons Haiyan and Haima. Haiyan was the strongest typhoon recorded since 1979 in the western Pacific and remained active from 3 to 11 November 2013. Haima was the second typhoon that reached winds with an intensity exceeding 220 km/h since 1979. The purpose of the present study is to describe the evolution of the lifecycle of Haiyan and Haima typhoons (lagrangian analysis), to show similarities and differences between them, and to evaluate the impact of these systems on atmospheric variables close to the Philippines (eulerian analysis). The atmospheric variables used in the study were obtained from the Global Forecast System Analysis and the Tropical Rainfall Measuring Mission. The cyclogenesis region of the Haiyan and Haima typhoons showed positive sea surface temperature anomalies of 0.7 °C and 1.1 ° C, respectively. Along the trajectory, the typhoons produced a cold trail on the ocean. Near the Philippines, the Haiyan caused winds with an intensity of 232 km/h and the Haima of 226 km/h. Regarding the lifecycle of these systems, the maturation phase shows more intense cyclonic relative vorticity and the highest zonal departure of air temperature in the core of the typhoons in relation to the neighborhoodhttp://www.anuario.igeo.ufrj.br/2018_03/2018_3_37_53.pdfTropical cycloneWestern Pacific OceanHaiyanHaima
spellingShingle Bruna Andrelina Silva
Rayan Reis Miranda Leite
Michelle Simões Reboita
Haiyan and Haima typhoons: Characteristics During Formation, Maturation and Dissipation
Anuário do Instituto de Geociências
Tropical cyclone
Western Pacific Ocean
Haiyan
Haima
title Haiyan and Haima typhoons: Characteristics During Formation, Maturation and Dissipation
title_full Haiyan and Haima typhoons: Characteristics During Formation, Maturation and Dissipation
title_fullStr Haiyan and Haima typhoons: Characteristics During Formation, Maturation and Dissipation
title_full_unstemmed Haiyan and Haima typhoons: Characteristics During Formation, Maturation and Dissipation
title_short Haiyan and Haima typhoons: Characteristics During Formation, Maturation and Dissipation
title_sort haiyan and haima typhoons characteristics during formation maturation and dissipation
topic Tropical cyclone
Western Pacific Ocean
Haiyan
Haima
url http://www.anuario.igeo.ufrj.br/2018_03/2018_3_37_53.pdf
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