Improved Global Tropical Cyclone Forecasts from NOAA: Lessons Learned and Path Forward
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Characteristics of Tropical Cyclonic Storm Phailin As Derived from Satellite and Atmospherics Observations 1R
IJECT VOL . 5, ISSU E SPL - 2, JAN - MAR C H 2014 ISSN : 2230-7109 (Online) | ISSN : 2230-9543 (Print) Characteristics of Tropical Cyclonic Storm Phailin as Derived From Satellite and Atmospherics Observations 1R. Bhattacharya, 2R. Guha, 3J. Pandit, 4A. B. Bhattacharya 1,2Dept. of Environmental Science, University of Kalyani, Kalyani, West Bengal, India 3,4Dept. of Physics, University of Kalyani, Kalyani, West Bengal, India 3Dept. of Physics, JIS School of Polytechnic, Kalyani, West Bengal, India Abstract But on the very next day, Phailin became equivalent to a A summary map concerning the formation of depression and category 4 hurricane on the SSHWS before it underwent an eye cyclonic storms over the North Indian Ocean in the year 2013 wall replacement cycle and formed a new eye wall early on October is first presented pointing out their names, durations and peak 11. This new eye wall further consolidated and allowed the system intensities. The cyclone Phailin originating from North Indian to intensify and become equivalent to a category 5 hurricane on Ocean rapidly developed an eye when it was converted to a very the SSHWS later that day [1-4]. The paper summarizes some severe cyclonic storm on October 10, 2013. Maximum sustained interesting characteristics of the cyclone Phailin and finds its winds are estimated at 195 km/h, gusting to 295 km/h while association with the VLF atmospherics at 27 kHz. minimum central pressure is estimated at 936 hPa with Dvorak intensity of the storm as T6.0. The system subsequently intensified II. Seasons Summary Map and became equivalent to a category 5 hurricane. -
Observation of Near-Inertial Oscillations Induced by Energy Transformation During Typhoons
energies Article Observation of Near-Inertial Oscillations Induced by Energy Transformation during Typhoons Huaqian Hou 1,2, Fei Yu 1,*, Feng Nan 1, Bing Yang 1, Shoude Guan 1 and Yuanzhi Zhang 3,* 1 Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; [email protected] (H.H.); [email protected] (F.N.); [email protected] (B.Y.); [email protected] (S.G.) 2 University of Chinese Academy of Sciences, Beijing 100049, China 3 Nanjing University of Information Science and Technology, Nanjing 210044, China * Correspondence: [email protected] (F.Y.); [email protected] (Y.Z.); Tel.: +86-186-5328-0417 (F.Y.) Received: 19 October 2018; Accepted: 25 December 2018; Published: 29 December 2018 Abstract: Three typhoon events were selected to examine the impact of energy transformation on near-inertial oscillations (NIOs) using observations from a subsurface mooring, which was deployed at 125◦ E and 18◦ N on 26 September 2014 and recovered on 11 January 2016. Almost 16 months of continuous observations were undertaken, and three energetic NIO events were recorded, all generated by passing typhoons. The peak frequencies of these NIOs, 0.91 times of the local inertial frequency f, were all lower than the local inertial frequency f. The estimated vertical −1 group velocities (Cgz) of the three NIO events were 11.9, 7.4, and 23.0 m d , and were relatively small compared with observations from other oceans (i.e., 100 m d−1). The directions of the horizontal near-inertial currents changed four or five times between the depths of 40 and 800 m in all three NIO events, implying that typhoons in the northwest Pacific usually generate high-mode NIOs. -
Characteristics of Satellite-Based Ocean Turbulent Heat Flux Around the Korean Peninsula and Relationship with Changes in Typhoon Intensity
remote sensing Article Characteristics of Satellite-Based Ocean Turbulent Heat Flux around the Korean Peninsula and Relationship with Changes in Typhoon Intensity Jaemin Kim and Yun Gon Lee * Atmospheric Sciences, Department of Astronomy, Space Science, and Geology, Chungnam National University, Daejeon 34134, Korea; [email protected] * Correspondence: [email protected]; Tel.: +82-042-821-7107 Abstract: Ocean-atmosphere energy exchange is an important factor in the maintenance of oceanic and atmospheric circulation and the regulation of meteorological and climate systems. Oceanic sensible and latent heat fluxes around the Korean Peninsula were determined using satellite-based air-sea variables (wind speed, sea surface temperature, and atmospheric specific humidity and temperature) and the coupled ocean-atmosphere response experiment (COARE) 3.5 bulk algorithm for six years between 2014 and 2019. Seasonal characteristics of the marine heat flux and its short- term fluctuations during summer typhoons were also investigated. Air-sea variables were produced through empirical relationships and verified with observational data from marine buoys around the Korean Peninsula. Satellite-derived wind speed, sea surface temperature, atmospheric specific humidity, and air temperature were strongly correlated with buoy data, with R2 values of 0.80, 0.97, 0.90, and 0.91, respectively. Satellite-based sensible and latent heat fluxes around the peninsula were also validated against fluxes calculated from marine buoy data, and displayed low values in summer and higher values in autumn and winter as the difference between air-sea temperature and specific humidity increased. Through analyses of spatio-temporal fluctuations in the oceanic turbulent heat Citation: Kim, J.; Lee, Y.G. -
Typhoon Haiyan
Emergency appeal Philippines: Typhoon Haiyan Emergency appeal n° MDRPH014 GLIDE n° TC-2013-000139-PHL 12 November 2013 This emergency appeal is launched on a preliminary basis for CHF 72,323,259 (about USD 78,600,372 or EUR 58,649,153) seeking cash, kind or services to cover the immediate needs of the people affected and support the Philippine Red Cross in delivering humanitarian assistance to 100,000 families (500,000 people) within 18 months. This includes CHF 761,688 to support its role in shelter cluster coordination. The IFRC is also soliciting support from National Societies in the deployment of emergency response units (ERUs) at an estimated value of CHF 3.5 million. The operation will be completed by the end of June 2015 and a final report will be made available by 30 September 2015, three months after the end Red Cross staff and volunteers were deployed as soon as safety conditions allowed, of the operation. to assess conditions and ensure that those affected by Typhoon Haiyan receive much-needed aid. Photo: Philippine Red Cross CHF 475,495 was allocated from the International Federation of Red Cross and Red Crescent Societies (IFRC) Disaster Relief Emergency Fund (DREF) on 8 November 2013 to support the National Society in undertaking delivering immediate assistance to affected people and undertaking needs assessments. Un-earmarked funds to replenish DREF are encouraged. Summary Typhoon Haiyan (locally known as Yolanda) made landfall on 8 November 2013 with maximum sustained winds of 235 kph and gusts of up to 275 kph. The typhoon and subsequent storm surges have resulted in extensive damage to infrastructure, making access a challenge. -
Typhoon Maysak Situation Report No
FSM: Typhoon Maysak Situation Report No. 5 (as of 17 April 2015) This report is produced by the Office of Environment and Emergency Management in collaboration with FSM National and Yap and Chuuk State authorities, UNDAC, USAID and humanitarian partners. It covers the period from 15 to 17 April 2015. The date for the issuing of the next report is Tuesday 21 April. Highlights The Caroline Voyager is docked in Yap since April 22, 2015 and re-provisioning. It is scheduled to depart for Ulithi, Fais, and Fareulap on April 25, 2015 to continue its delivery of relief items. Vice President Alik Alik is making his official visit to the State of Yap on April 25, 2015 for a week, scheduled to visit the islands of Ulithi and Fais during his stay. USAID conducted an Airlift of Emergency Relief Supplies to Yap and Chuuk on April 22, 2015. Tanks being loaded on Voyager for Outlying effected islands, April 23, 2015 Food Assistance Over 90% of Emergency water Home repair Infrastructure c. 30,000 source and water and repair and Affected crops for 6 Individuals destroyed treatment reconstruction rehabilitation months supplies Situation Overview Typhoon Maysak made landfall at Chuuk lagoon on Sunday 29th March and Ulithi Atoll, Yap on 1st April while neighboring islands within the two states also experienced strong destructive winds causing damages. Governor Johnson Elimo of Chuuk and Governor Tony Ganngiyan of Yap had on 30th March and 1st April respectively declared state of emergency for their states. President Manny Mori consequently had declared a State of Emergency for both states and reaffirms the FSM Emergency Task Force to coordinate all response efforts which includes mobilization of national government resources and international assistance. -
Forecasting of Storm Surge and Wave Along Taiwan Coast Y
Forecasting of Storm Surge and Wave along Taiwan Coast Y. Peter Sheng1, *, Vladimir A. Paramygin2, Chuen-Teyr Terng 3, and Chi-Hao Chu 3 1Advanced Aqua Dynamics, Inc., Gainesville, Florida, U.S.A. 2 University of Florida, Gainesville, Florida, U.S.A. 3 Central Weather Bureau, Taipei, Taiwan, R.O.C. *Corresponding Author: [email protected] Abstract This paper describes the application of a coupled surge-wave modeling system CH3D-SWAN for simulating storm surge and wave along Taiwan coast. The modeling system has been used for simulating storm surge and wave in the U.S., Arabian Gulf, and Taiwan. This paper presents the hindcasting of Typhoon Soudelor in 2015 and the forecasting of the typhoon season in 2016 with Typhoon Meiji as an example. Performance of the forecasting system is assessed and future forecasting effort is discussed. Key words: Storm Surge, Wave, Numerical Simulation, Forecasting, Taiwan 1. Introduction typhoons of Taiwan. In the following section, we first give a brief description of the CH3D-SWAN modeling In Taiwan, typhoons are an annual threat. Typhoons not only bring torrential rain, but often cause storm surge, wave, and coastal inundation that system with all the associated modules of the impact areas near the coast and amplifies the flooding forecasting system and model domains. Model from rainfall. The impact of tropical cyclones on the hindcasting of storm surge and wave during Typhoon coastal regions in Taiwan depend on the Soudelor in 2015 is then described, followed by a characteristics of tropical cyclones and coastal regions. description of the forecasting performance of the 2016 For example, along the southwest coast of Taiwan typhoon season using Typhoon Meji as an example. -
The Impact of Tropical Cyclone Hayan in the Philippines: Contribution of Spatial Planning to Enhance Adaptation in the City of Tacloban
UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS Faculdade de Ciências Faculdade de Ciências Sociais e Humanas Faculdade de Letras Faculdade de Ciências e Tecnologia Instituto de Ciências Sociais Instituto Superior de Agronomia Instituto Superior Técnico The impact of tropical cyclone Hayan in the Philippines: Contribution of spatial planning to enhance adaptation in the city of Tacloban Doutoramento em Alterações Climáticas e Políticas de Desenvolvimento Sustentável Especialidade em Ciências do Ambiente Carlos Tito Santos Tese orientada por: Professor Doutor Filipe Duarte Santos Professor Doutor João Ferrão Documento especialmente elaborado para a obtenção do grau de Doutor 2018 UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS Faculdade de Ciências Faculdade de Ciências Sociais e Humanas Faculdade de Letras Faculdade de Ciências e Tecnologia Instituto de Ciências Sociais Instituto Superior de Agronomia Instituto Superior Técnico The impact of tropical cyclone Haiyan in the Philippines: Contribution of spatial planning to enhance adaptation in the city of Tacloban Doutoramento em Alterações Climáticas e Políticas de Desenvolvimento Sustentável Especialidade em Ciências do Ambiente Carlos Tito Santos Júri: Presidente: Doutor Rui Manuel dos Santos Malhó; Professor Catedrático Faculdade de Ciências da Universidade de Lisboa Vogais: Doutor Carlos Daniel Borges Coelho; Professor Auxiliar Departamento de Engenharia Civil da Universidade de Aveiro Doutor Vítor Manuel Marques Campos; Investigador Auxiliar Laboratório Nacional de Engenharia Civil(LNEC) -
Structural Characteristics of T-PARC Typhoon Sinlaku During Its Extratropical Transition
MAY 2014 Q U I N T I N G E T A L . 1945 Structural Characteristics of T-PARC Typhoon Sinlaku during Its Extratropical Transition JULIAN F. QUINTING Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany MICHAEL M. BELL* AND PATRICK A. HARR Department of Meteorology, Naval Postgraduate School, Monterey, California 1 SARAH C. JONES Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany (Manuscript received 28 September 2013, in final form 27 December 2013) ABSTRACT The structure and the environment of Typhoon Sinlaku (2008) were investigated during its life cycle in The Observing System Research and Predictability Experiment (THORPEX) Pacific Asian Regional Campaign (T-PARC). On 20 September 2008, during the transformation stage of Sinlaku’s extratropical transition (ET), research aircraft equipped with dual-Doppler radar and dropsondes documented the structure of the con- vection surrounding Sinlaku and low-level frontogenetical processes. The observational data obtained were assimilated with the recently developed Spline Analysis at Mesoscale Utilizing Radar and Aircraft In- strumentation (SAMURAI) software tool. The resulting analysis provides detailed insight into the ET system and allows specific features of the system to be identified, including deep convection, a stratiform pre- cipitation region, warm- and cold-frontal structures, and a dry intrusion. The analysis offers valuable information about the interaction of the features identified within the transitioning tropical cyclone. The existence of dry midlatitude air above warm-moist tropical air led to strong potential instability. Quasigeo- strophic diagnostics suggest that forced ascent during warm frontogenesis triggered the deep convective development in this potentially unstable environment. -
Dependence of Probabilistic Quantitative Precipitation Forecast Performance on Typhoon Characteristics and Forecast Track Error in Taiwan
APRIL 2020 T E N G E T A L . 585 Dependence of Probabilistic Quantitative Precipitation Forecast Performance on Typhoon Characteristics and Forecast Track Error in Taiwan HSU-FENG TENG AND JAMES M. DONE National Center for Atmospheric Research, Boulder, Colorado CHENG-SHANG LEE Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan YING-HWA KUO National Center for Atmospheric Research, and University Corporation for Atmospheric Research, Boulder, Colorado (Manuscript received 15 August 2019, in final form 7 January 2020) ABSTRACT This study investigates the probabilistic quantitative precipitation forecast (PQPF) performance of ty- phoons that affected Taiwan during 2011–16. In this period, a total of 19 typhoons with a land warning issued by the Central Weather Bureau (CWB) are analyzed. The PQPF is calculated using the ensemble precipi- tation forecast data from the Taiwan Cooperative Precipitation Ensemble Forecast Experiment (TAPEX), and the verification data, verification thresholds, and typhoon characteristics are obtained from the CWB. The overall PQPF performance of TAPEX has an acceptable reliability and discrimination ability, and the higher probability error is distributed at the mountainous area of Taiwan. The PQPF performance is significantly influenced by typhoon characteristics (e.g., typhoon tracks, sizes, and forward speeds). The PQPFs for westward-moving, large, or slow typhoons have higher reliability and discrimination ability, and lower- probability error than those for northward-moving, small, or fast typhoons, except for similar reliability between fast and slow typhoons. Because northward-moving or small typhoons have larger forecast track error, and their PQPF performance is sensitive to the accuracy of the forecast track, a higher probability error occurs than that for westward-moving or large typhoons. -
September 2013 Global Catastrophe Recap 2 2
September 2013 Global Catastrophe Recap Table of Contents Executive0B Summary 3 United2B States 4 Remainder of North America (Canada, Mexico, Caribbean, Bermuda) 4 South4B America 5 Europe 6 6BAfrica 6 Asia 6 Oceania8B (Australia, New Zealand and the South Pacific Islands) 8 8BAAppendix 9 Contact Information 16 Impact Forecasting | September 2013 Global Catastrophe Recap 2 2 Executive0B Summary . Tropical cyclone landfalls in Mexico and Asia cause more than USD10 billion in economic losses . Major flooding damages 20,000 homes in Colorado as economic losses top USD2.0 billion . Two powerful earthquakes (M7.7 & M6.8) kill at least 825 people in Pakistan Hurricanes Manuel and Ingrid made separate landfalls within 24 hours on opposite sides of Mexico, bringing tremendous rainfall and gusty winds that caused extensive damage across more than two-thirds of the country. At least 192 people were killed or listed as missing. Manuel made separate landfalls in the states of Colima and Sinaloa while slowly tracking along the Mexico’s Pacific coastline, and Ingrid made landfall in the state of Tamaulipas. The government estimated total economic losses from both storms at MXN75 billion (USD5.7 billion), with the Mexican Association of Insurance Institutions estimating insured losses minimally at MXN12 billion (USD915 million). Super Typhoon Usagi made landfall in China after first skirting the Philippines and Taiwan. At least 47 people were killed. Usagi’s landfall in China marked one of the strongest typhoons to come ashore in Guangdong Province in nearly 40 years. Property damage was widespread in five Chinese provinces as Usagi damaged at least 101,200 homes. -
North Pacific, on August 31
Marine Weather Review MARINE WEATHER REVIEW – NORTH PACIFIC AREA May to August 2002 George Bancroft Meteorologist Marine Prediction Center Introduction near 18N 139E at 1200 UTC May 18. Typhoon Chataan: Chataan appeared Maximum sustained winds increased on MPC’s oceanic chart area just Low-pressure systems often tracked from 65 kt to 120 kt in the 24-hour south of Japan at 0600 UTC July 10 from southwest to northeast during period ending at 0000 UTC May 19, with maximum sustained winds of 65 the period, while high pressure when th center reached 17.7N 140.5E. kt with gusts to 80 kt. Six hours later, prevailed off the west coast of the The system was briefly a super- the Tenaga Dua (9MSM) near 34N U.S. Occasionally the high pressure typhoon (maximum sustained winds 140E reported south winds of 65 kt. extended into the Bering Sea and Gulf of 130 kt or higher) from 0600 to By 1800 UTC July 10, Chataan of Alaska, forcing cyclonic systems 1800 UTC May 19. At 1800 UTC weakened to a tropical storm near coming off Japan or eastern Russia to May 19 Hagibis attained a maximum 35.7N 140.9E. The CSX Defender turn more north or northwest or even strength of 140-kt (sustained winds), (KGJB) at that time encountered stall. Several non-tropical lows with gusts to 170 kt near 20.7N southwest winds of 55 kt and 17- developed storm-force winds, mainly 143.2E before beginning to weaken. meter seas (56 feet). The system in May and June. -
Simulating Storm Surge and Inundation Along the Taiwan Coast During Typhoons Fanapi in 2010 and Soulik in 2013
Terr. Atmos. Ocean. Sci., Vol. 27, No. 6, 965-979, December 2016 doi: 10.3319/TAO.2016.06.13.01(Oc) Simulating Storm Surge and Inundation Along the Taiwan Coast During Typhoons Fanapi in 2010 and Soulik in 2013 Y. Peter Sheng1, *, Vladimir A. Paramygin1, Chuen-Teyr Terng 2, and Chi-Hao Chu 2 1 University of Florida, Gainesville, Florida, U.S.A. 2 Central Weather Bureau, Taipei City, Taiwan, R.O.C. Received 10 January 2016, revised 9 June 2016, accepted 13 June 2016 ABSTRACT Taiwan is subjected to significant storm surges, waves, and coastal inundation during frequent tropical cyclones. Along the west coast, with gentler bathymetric slopes, storm surges often cause significant coastal inundation. Along the east coast with steep bathymetric slopes, waves can contribute significantly to the storm surge in the form of wave setup. To examine the importance of waves in storm surges and quantify the significance of coastal inundation, this paper presents numerical simulations of storm surge and coastal inundation during two major typhoons, Fanapi in 2010 and Soulik in 2013, which impacted the southwest and northeast coasts of Taiwan, respectively. The simulations were conducted with an integrated surge-wave modeling system using a large coastal model domain wrapped around the island of Taiwan, with a grid resolution of 50 - 300 m. During Fanapi, the simulated storm surge and coastal inundation near Kaohsiung are not as accurate as those obtained using a smaller coastal domain with finer resolution (40 - 150 m). During Soulik, the model simulations show that wave setup contributed significantly (up to 20%) to the peak storm surge along the northeast coast of Taiwan.