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Nat. Hazards Earth Syst. Sci., 14, 2867–2882, 2014 www.nat-hazards-earth-syst-sci.net/14/2867/2014/ doi:10.5194/nhess-14-2867-2014 © Author(s) 2014. CC Attribution 3.0 License. A catalog of high-impact windstorms in Switzerland since 1859 P. Stucki1, S. Brönnimann1, O. Martius1,2, C. Welker1, M. Imhof3, N. von Wattenwyl1, and N. Philipp1 1Oeschger Centre for Climate Change Research and Institute of Geography, University of Bern, Bern, Switzerland 2Mobiliar Lab for Natural Risks, Bern, Switzerland 3Interkantonaler Rückversicherungsverband, Bern, Switzerland Correspondence to: P. Stucki ([email protected]) Received: 17 April 2014 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 28 May 2014 Revised: 12 September 2014 – Accepted: 23 September 2014 – Published: 4 November 2014 Abstract. In recent decades, extremely hazardous wind- The damage to buildings and forests from recent, extreme storms have caused enormous losses to buildings, infrastruc- windstorms, such as Vivian (February 1990) and Lothar (De- ture and forests in Switzerland. This has increased societal cember 1999), have been perceived as unprecedented and and scientific interest in the intensity and frequency of his- unanticipated (Bründl and Rickli, 2002; Holenstein, 1994; torical high-impact storms. However, high-resolution wind Schüepp et al., 1994; Brändli, 1996; WSL, 2001). data and damage statistics mostly span recent decades only. Public perception of a potentially increasing windstorm For this study, we collected quantitative (e.g., volumes of hazard (Schmith et al., 1998) motivated several studies on windfall timber, losses relating to buildings) and descriptive the intensity and occurrence frequency of high-impact storms (e.g., forestry or insurance reports) information on the impact (e.g., Pfister, 1999). -
Temporal and Spatial Characteristics of Typhoon Induced Precipitation Over Northern Japan 〇Sridhara NAYAK , Tetsuya TAKEMI
A06 Temporal and Spatial Characteristics of Typhoon Induced Precipitation over Northern Japan 〇Sridhara NAYAK , Tetsuya TAKEMI Introduction: various duration bins. Finally, we calculated the Typhoons are considered as one of the dangerous frequency in each bin. In the similar way, we weather phenomena in the earth that caused investigated the size of the precipitations. widespread flooding to the landfall regions. Over the year, plenty of typhoons have made landfall over Preliminary Results: Japan and some of them have devastated large areas Figure 1 shows the probability of the duration of and impacted millions of people by extreme extreme precipitations for the Typhoon Chanthu. It precipitations (Takemi et al. 2016; Takemi, 2019). In shows the duration of the precipitations exceeding August 2016, three typhoons [Typhoon Chanthu various percentiles of precipitation in the range (T1607), Mindulle (T1609), and Kompasu (T1611)] between 50% and 99.99%. Results indicate that the made landfall over Hokkaido region and one typhoon occurrence of extremely heavy precipitations (higher [Lionrock (T1610)] made landfall over Tohoku region. than 99th percentile) are short-lived and last up to 6 All these typhoons caused widespread damages over hours. The extreme precipitation with intensity below northern Japan with excessive precipitations. However, 90th percentile last at least 9 hours. We also find studies are limited to understand the temporal and long-lived precipitations which last 12 hours and more, spatial structure of precipitation, particularly the although they don’t occur so frequently. precipitation size and duration within individual typhoons. In this study, we analyzed the precipitations induced by these four typhoons to investigate their extreme precipitation spell duration and size. -
Typhoon Neoguri Disaster Risk Reduction Situation Report1 DRR Sitrep 2014‐001 ‐ Updated July 8, 2014, 10:00 CET
Typhoon Neoguri Disaster Risk Reduction Situation Report1 DRR sitrep 2014‐001 ‐ updated July 8, 2014, 10:00 CET Summary Report Ongoing typhoon situation The storm had lost strength early Tuesday July 8, going from the equivalent of a Category 5 hurricane to a Category 3 on the Saffir‐Simpson Hurricane Wind Scale, which means devastating damage is expected to occur, with major damage to well‐built framed homes, snapped or uprooted trees and power outages. It is approaching Okinawa, Japan, and is moving northwest towards South Korea and the Philippines, bringing strong winds, flooding rainfall and inundating storm surge. Typhoon Neoguri is a once‐in‐a‐decade storm and Japanese authorities have extended their highest storm alert to Okinawa's main island. The Global Assessment Report (GAR) 2013 ranked Japan as first among countries in the world for both annual and maximum potential losses due to cyclones. It is calculated that Japan loses on average up to $45.9 Billion due to cyclonic winds every year and that it can lose a probable maximum loss of $547 Billion.2 What are the most devastating cyclones to hit Okinawa in recent memory? There have been 12 damaging cyclones to hit Okinawa since 1945. Sustaining winds of 81.6 knots (151 kph), Typhoon “Winnie” caused damages of $5.8 million in August 1997. Typhoon "Bart", which hit Okinawa in October 1999 caused damages of $5.7 million. It sustained winds of 126 knots (233 kph). The most damaging cyclone to hit Japan was Super Typhoon Nida (reaching a peak intensity of 260 kph), which struck Japan in 2004 killing 287 affecting 329,556 people injuring 1,483, and causing damages amounting to $15 Billion. -
Cyclone Factsheet UPDATE
TROPICAL CYCLONES AND CLIMATE CHANGE: FACTSHEET CLIMATECOUNCIL.ORG.AU TROPICAL CYCLONES AND CLIMATE CHANGE: FACT SHEET KEY POINTS • Climate change is increasing the destructive power of tropical cyclones. o All weather events today, including tropical cyclones, are occurring in an atmosphere that is warmer, wetter, and more energetic than in the past. o It is likely that maximum windspeeds and the amount of rainfall associated with tropical cyclones is increasing. o Climate change may also be affecting many other aspects of tropical cyclone formation and behaviour, including the speed at which they intensify, the speed at which a system moves (known as translation speed), and how much strength is retained after reaching land – all factors that can render them more dangerous. o In addition, rising sea levels mean that the storm surges that accompany tropical cyclones are even more damaging. • While climate change may mean fewer tropical cyclones overall, those that do form can become more intense and costly. In other words, we are likely to see more of the really strong and destructive tropical cyclones. • A La Niña event brings an elevated tropical cyclone risk for Australia, as there are typically more tropical cyclones in the Australian region than during El Niño years. BACKGROUND Tropical cyclones, known as hurricanes in the North Atlantic and Northeast Pacific, typhoons in the Northwest Pacific, and simply as tropical cyclones in the South Pacific and Indian Oceans, are among the most destructive of extreme weather events. Many Pacific Island Countries, including Fiji, Vanuatu, Solomon Islands and Tonga, lie within the South Pacific cyclone basin. -
Efforts for Emergency Observation Mapping in Manila Observatory
Efforts for Emergency Observation Mapping in Manila Observatory: Development of a Typhoon Impact Estimation System (TIES) focusing on Economic Flood Loss of Urban Poor Communities in Metro Manila UN-SPIDER International Conference on Space-based Technologies for Disaster Risk Reduction – “Enhancing Disaster Preparedness for Effective Emergency Response” Session 4: Demonstrating Advances in Earth Observation to Build Back Better September 25, 2018 Ma. Flordeliza P. Del Castillo Manila Observatory EMERGENCY OBSERVATION MAPPING IN MANILA OBSERVATORY • Typhoon Reports • Sentinel Asia Data Analysis Node (2011-present) • Flood loss estimation for urban poor households in Metro Manila (2016-present) 1. Regional Climate Systems (RCS) – Hazard analysis (Rainfall and typhoon forecast) 2. Instrumentation and Efforts before typhoon arrives Technology Development – Automated Weather Stations 3. Geomatics for Environment and Development – Mapping and integration of Hazard, Exposure and Vulnerability layers Observing from space and also from the ground. Efforts during typhoon event Now, incorporating exposure and vulnerability variables Efforts after a typhoon event Data Analysis Node (Post- Disaster Event) Image Source: Secretariat of Sentinel Asia Japan Aerospace Exploration Agency, Sentinel Asia Annual Report 2016 MO Emergency Observation (EO) and Mapping Protocol (15 October 2018) Step 1: Step 2: Step 3: Establish the Apply for EMERGENCY Elevate status to LOCATION/COVERAGE of OBSERVATION to International Disaster EOR Sentinel Asia (SA) Charter (IDC) by ADRC Step 6: Step 5: Step 4: Upload maps in MO, SA MAP Download images & IDC websites PRODUCTION Emergency Observation Mapping Work • December 2011 – T.S. Washi “Sendong” • August 2012 – Southwest Monsoon Flood “Habagat” • ” Emergency Observation Mapping Work • December 2011 – T.S. Washi “Sendong” • August 2012 – Southwest Monsoon Flood “Habagat” • December 2012 – Bopha “Pablo” • August 2013 – Southwest Monsoon Flood and T.S. -
Monitoring Black Grouse Tetrao Tetrix in Isère, Northern French Alps: Cofactors, Population Trends and Potential Biases
Animal Biodiversity and Conservation 42.2 (2019) 227 Monitoring black grouse Tetrao tetrix in Isère, northern French Alps: cofactors, population trends and potential biases L. Dumont, E. Lauer, S. Zimmermann, P. Roche, P. Auliac, M. Sarasa Dumont, L., Lauer, E., Zimmermann, S., Roche, P., Auliac, P., Sarasa, M., 2019. Monitoring black grouse Tetrao tetrix in Isère, northern French Alps: cofactors, population trends and potential biases. Animal Biodiversity and Conservation, 42.2: 227–244, Doi: https://doi.org/10.32800/abc.2019.42.0227 Abstract Monitoring black grouse Tetrao tetrix in Isère, northern French Alps: cofactors, population trends and potential biases. Wildlife management benefits from studies that verify or improve the reliability of monitoring protocols. In this study in Isère, France, we tested for potential links between the abundance of black grouse (Tetrao tetrix) in lek–count surveys and cofactors (procedural, geographical and meteorological cofactors) between 1989 and 2016. We also examined the effect of omitting or considering the important cofactors on the long–term population trend that can be inferred from lek–count data. Model selections for data at hand highlighted that the abundance of black grouse was mainly linked to procedural cofactors, such as the number of observers, the time of first observation of a displaying male, the day, and the year of the count. Some additional factors relating to the surface of the census sector, temperature, northing, altitude and wind conditions also appeared depending on the spatial or temporal scale of the analysis. The inclusion of the important cofactors in models modulated the estimates of population trends. The results of the larger dataset highlighted a mean increase of +17 % (+5.3 %; +29 %) of the abundance of black grouse from 1997 to 2001, and a mean increase in population of +47 % (+16 %; +87 %) throughout the study period (1989–2016). -
OCHA PHL TY Sarika Haima 17Oct2016
Philippines: Typhoons Sarika (Karen) and Haima (Lawin) (17 October 2016) Typhoon Sarika Japan Typhoon Haima Typhoon category Typhoon Sarika (Karen) made landfall in (Saffir-Simpson Scale) Typhoon Haima (Lawin) has intensified 22 October 2016 Baler, Aurora province, at 2:30 a.m. on Category 1: 119-153 km/hr from a severe tropical storm. It was last 16 October. It slightly weakend while spotted 1,265 km east of the Visayas with China Category 3: 178-208 km/hr crossing Central Luzon but slightly maximum sustained winds of up to 150 intensified as it moves away from the Category 4: 209-251 km/hr km/h and gusts of up to 185 km/h. It is Philippines. As of 6am 17 October 2016, Taiwan moving west northwest at 22 km/h and is Typhoon Sarika is out of the Philippines Category 5: > 252 km/hr expected to enter PAR by the afternoon Area of Responsibility (PAR) and all PAGASA category of 17 October. The typhoon is projected Tropical Cyclone Warning Signals Hong Kong Typhoon Karen (SARIKA) to intensify into a category 5 as it moves Macao (TCWS) have been lifted. Tropical depression closer to northern Philippines. 21 October 2016 Lawin (HAIMA) Tropical storm EFFECTS Forecasted to make landfall Severe tropical storm PROFILE Regions I, II, III, IV-A, V and CAR in Northern Cagayan Typhoon within the 100 km radius of typhoon track affected areas 20 October 2016 P.A.R. 4 47 Actual typhoon track provinces cities/municipalities 75,000 Typhoon Haima people affected Forecasted track 17 October 2016 1.9 Million 406,000 19 October 2016 people households 70,800 LUZON people displaced 18 October 2016 Lawin (HAIMA) Forecasted to enter P.A.R. -
Pull up Banner Tropical Cycclone.Ai
Air released Eye air Warm air Cold rises Steady winds Eye Warm air A tropical Cyclone (also known as typhoons or hurricanes) is a violent rotating windstorm that develops over warm tropical waters warner than 26.5°C and located between 5° and 15°latitude. Tropical Cyclones affect nearly all Pacific Islands countries and are the most frequent hazard to affect Fiji with around 2 – 3 cyclones occurring every year. As a result of climate change, cyclone frequency has doubled in the last decade. The cyclone season in Fiji runs from November to April and some cyclones do occur outside the season. T ropical Cyclone Strong winds can devastating western Viti Levu continue for hours, days, and killing seven people. even causing widespread damage to buildings, Storm surges and waves infrastructure and created by low atmospheric vegetation and causing pressure and strong cyclonic loss of life. winds blowing over long distance. A storm surge is a Wind speed levels of a raised dome of seawater about tropical cyclone are; 60-80km wide and 2-5m higher Gale Force Winds : 63-87 km/h than normal sea level. As the Storm force winds : 88-117 km/h cyclone makes landfall, storm Hurricane force winds : 117 + km/h surge and waves inundate coastal areas. At the coast, Torrential rains can result in widespread flash flooding and storm surge and waves are the river flooding. Up to 600mm and more of high intensity rain can greatest threat to life and be produced in one day. These rains can also trigger property and also cause severe landslides in hilly areas, which may already be sodden due to coastal erosion. -
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) -
The Tropic Islesbreezes
Published by On Trac Publishing, P.O. Box 985, Bradenton, FL 34206 (941) 723-5003 Tropic Isles • 1503 28th Ave. West • Palmetto, Florida 34221 • (941) 721-8888 • Website: www.TropicIsles.net Home of the Month Meet Your New Neighbors By Cindy Shaw The Tropic Isles I’d like to introduce you to our new, part-time neighbors, PAUL September and MIRIAM GROSSI. They live in their new home at 128 Capri Dr. Paul is originally from New York City, NY, but both he and Miriam now reside part-time in Millersburg, Ohio. Paul is a retired hospital administrator in Ohio and Okla- homa where he worked for 35 years. Miriam is a retired RN of 17 years and has foster parented newborns for many years. Paul and Miriam also ran a B & B in Millersburg for 13 years. They have been coming down to this area for 14 years and have been vacationing on Anna Maria Island. While on vacation, they 2017 would often ride out to Emerson Point. They would also do an exchange system with their B & B allowing interested people to September’s “Home of the Month” belongs to Tommy and stay in their B & B in exchange for staying in other peoples’ homes. Charlene Barlow at 1312 29th Ave. W. Lots of work and loving When they became interested in putting down roots, they touches, both inside and out, went into the creation of this cute began looking at vacant lots in the area where they could build little “tropical cottage”. Congratulations! a house. They went to Jacobson Homes who sent them to Tropic Isles. -
The Diurnal Cycle of Clouds in Tropical Cyclones Over the Western North Pacific Basin
SOLA, 2020, Vol. 16, 109−114, doi:10.2151/sola.2020-019 109 The Diurnal Cycle of Clouds in Tropical Cyclones over the Western North Pacific Basin Kohei Fukuda1, Kazuaki Yasunaga1, Ryo Oyama2, 3, Akiyoshi Wada3, Atsushi Hamada1, and Hironori Fudeyasu4 1Department of Earth Science, Graduate School of Science and Engineering, University of Toyama, Toyama, Japan 2Forecast Division, Forecast Department, Japan Meteorological Agency (JMA), Tokyo, Japan 3Meteorological Research Institute (MRI), Tsukuba, Japan 4Yokohama National University, Yokohama, Japan for this is not understood. In addition, previous studies by Kossin Abstract (2002) and Dunion et al. (2014) focused exclusively on Atlantic storms or eastern Pacific storms. Our knowledge of the TC diurnal This study examined the diurnal cycles of brightness tempera- cycle over the western North Pacific (WNP) basin is limited, ture (TB) and upper-level horizontal winds associated with tropi- even though the WNP is the area where TCs are most frequently cal cyclones (TCs) over the western North Pacific basin, making generated (e.g., Peduzzi et al. 2012). Furthermore, relationships use of data retrieved from geostationary-satellite (Himawari-8) between cirrus cloud and dynamic fields have not been adequately observations that exhibited unprecedented temporal and spatial documented on the basis of observational data, while changes in resolutions. The results of a spectral analysis revealed that diurnal maximum wind velocity in TCs statistically depend on the local cycles prevail in TB variations over the outer regions of TCs (300− time (e.g., Yaroshevich and Ingel 2013). From a technical point of 500 km from the storm center). The dominance of the diurnal view, previous studies analyzed observations at a relatively lower cycle was also found in variations in the radial wind (Vr) in inten- time interval of three hours, and it is likely that the results were sive TCs, although there was no dominant cycle in tangential wind contaminated by higher-order harmonics due to aliasing. -
State of the Climate in 2016
STATE OF THE CLIMATE IN 2016 Special Supplement to the Bullei of the Aerica Meteorological Society Vol. 98, No. 8, August 2017 STATE OF THE CLIMATE IN 2016 Editors Jessica Blunden Derek S. Arndt Chapter Editors Howard J. Diamond Jeremy T. Mathis Ahira Sánchez-Lugo Robert J. H. Dunn Ademe Mekonnen Ted A. Scambos Nadine Gobron James A. Renwick Carl J. Schreck III Dale F. Hurst Jacqueline A. Richter-Menge Sharon Stammerjohn Gregory C. Johnson Kate M. Willett Technical Editor Mara Sprain AMERICAN METEOROLOGICAL SOCIETY COVER CREDITS: FRONT/BACK: Courtesy of Reuters/Mike Hutchings Malawian subsistence farmer Rozaria Hamiton plants sweet potatoes near the capital Lilongwe, Malawi, 1 February 2016. Late rains in Malawi threaten the staple maize crop and have pushed prices to record highs. About 14 million people face hunger in Southern Africa because of a drought that has been exacerbated by an El Niño weather pattern, according to the United Nations World Food Programme. A supplement to this report is available online (10.1175/2017BAMSStateoftheClimate.2) How to cite this document: Citing the complete report: Blunden, J., and D. S. Arndt, Eds., 2017: State of the Climate in 2016. Bull. Amer. Meteor. Soc., 98 (8), Si–S277, doi:10.1175/2017BAMSStateoftheClimate.1. Citing a chapter (example): Diamond, H. J., and C. J. Schreck III, Eds., 2017: The Tropics [in “State of the Climate in 2016”]. Bull. Amer. Meteor. Soc., 98 (8), S93–S128, doi:10.1175/2017BAMSStateoftheClimate.1. Citing a section (example): Bell, G., M. L’Heureux, and M. S. Halpert, 2017: ENSO and the tropical Paciic [in “State of the Climate in 2016”].