Nonus Tropical Cyclone and Earthquake CAT Loss Estimates
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Member Report
MEMBER REPORT ESCAP/WMO Typhoon Committee 10 th Integrated Workshop REPUBLIC OF KOREA 26-29 October 2015 Kuala Lumpur, Malaysia CONTENTS I. Overview of tropical cyclones which have affected/impacted Member’s area since the last Typhoon Committee Session (as of 10 October) II. Summary of progress in Key Result Areas (1) Starting the Tropical Depression Forecast Service (2) Typhoon Post-analysis procedure in KMA (3) Capacity Building on the Typhoon Analysis and Forecast (4) Co-Hosting the 8 th China-Korea Joint Workshop on Tropical Cyclones (5) Theweb-based portal to provide the products of seasonal typhoon activity outlook for the TC Members (POP5) (6) Implementation of Typhoon Analysis and Prediction System (TAPS)inthe Thai Meteorological Department and Lao PDR Department of Meteorology and Hydrology (POP4) (7) Development and application of multi-model ensemble technique for improving tropical cyclone track and intensity forecast (8) Improvement in TC analysis using automated ADT and SDT operationally by COMS data and GPM microwave data in NMSC/KMA (9) Typhoon monitoring using ocean drifting buoys around the Korea (10) Case study of typhoon CHAN-HOM using Yong-In Test-bed dual-polarization radar in Korea (11) Achievementsaccording toExtreme Flood Forecasting System (AOP2) (12) Technical Report on Assessment System of Flood Control Measures (ASFCM) (13) Progress on Extreme Flood Management Guideline (AOP6) (14) Flood Information Mobile Application (15) The 4 th Meeting and Workshop of TC WGH and WGH Homepage (16) 2015 Northern Mindanao Project in Philippines by NDMI and PAGASA (17) Upgrade of the functions in Typhoon Committee Disaster Information System (TCDIS) (18) The 9 th WGDRR Annual Workshop (19) 2015 Feasibility Studies to disseminate Disaster Prevention Technology in Vietnam and Lao PDR I. -
SCIENCE CHINA Earth Sciences
SCIENCE CHINA Earth Sciences SPECIAL TOPIC: Weather characteristics and climate anomalies of the TC track, heavy rainfall and tornadoes in 2018 https://doi.org/10.1007/s11430-019-9391-1 •RESEARCH PAPER• Climatology of tropical cyclone tornadoes in China from 2006 to 2018 Lanqiang BAI1,2,3, Zhiyong MENG2*, Kenta SUEKI4, Guixing CHEN1,3 & Ruilin ZHOU2 1 School of Atmospheric Sciences, and Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Guangzhou 510275, China; 2 Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871, China; 3 Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China; 4 RIKEN Center for Computational Science, Kobe 650-0047, Japan Received March 12, 2019; revised June 14, 2019; accepted July 11, 2019; published online September 12, 2019 Abstract We surveyed the occurrence of tropical cyclone (TC) tornadoes in China from 2006 to 2018. There were 64 cataloged TC tornadoes, with an average of five per year. About one-third of the landfalling TCs in China were tornadic. Consistent with previous studies, TC tornadoes preferentially formed in the afternoon shortly before and within about 36 h after landfall of the TCs. These tornadoes mainly occurred in coastal areas with relatively flat terrains. The maximum number of TC tornadoes occurred in Jiangsu and Guangdong provinces. Most of the TC tornadoes were spawned within 500 km of the TC center. Two notable characteristics were found: (1) TC tornadoes in China mainly occurred in the northeast quadrant (Earth-relative co- ordinates) rather than the right-front quadrant (TC motion-relative coordinates) of the parent TC circulation; and (2) most tornadoes were produced by TCs with a relatively weak intensity (tropical depressions/storms), in contrast with the United States where most tornadoes are associated with stronger TCs. -
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. -
Chapter 7. Building a Safe and Comfortable Society
Section 1 Realizing a Universal Society Building a Safe and Comfortable Chapter 7 Society Section 1 Realizing a Universal Society 1 Realizing Accessibility through a Universal Design Concept The “Act on Promotion of Smooth Transportation, etc. of Elderly Persons, Disabled Persons, etc.” embodies the universal design concept of “freedom and convenience for anywhere and anyone”, making it mandatory to comply with “Accessibility Standards” when newly establishing various facilities (passenger facilities, various vehicles, roads, off- street parking facilities, city parks, buildings, etc.), mandatory best effort for existing facilities as well as defining a development target for the end of FY2020 under the “Basic Policy on Accessibility” to promote accessibility. Also, in accordance with the local accessibility plan created by municipalities, focused and integrated promotion of accessibility is carried out in priority development district; to increase “caring for accessibility”, by deepening the national public’s understanding and seek cooperation for the promotion of accessibility, “accessibility workshops” are hosted in which you learn to assist as well as virtually experience being elderly, disabled, etc.; these efforts serve to accelerate II accessibility measures (sustained development in stages). Chapter 7 (1) Accessibility of Public Transportation In accordance with the “Act on Figure II-7-1-1 Current Accessibility of Public Transportation Promotion of Smooth Transportation, etc. (as of March 31, 2014) of Elderly Persons, Disabled -
Table of Contents
Table of Contents 1. Atmospheric data assimilation schemes, analysis and initialization, data impact studies, observing system experiments Author Paper Title Country Pages L. Duc, T. Koruda, K. Saito and Data assimilation experiments of Myanmar cyclone Japan 01-03 T. Fujita Nargis based on NHM-LETKF Radar reflectivity assimilation in JMA’s operational Y. Ikuta Japan 01-05 meso-analysis system Simplified basic state update in the JMA global 4D- T. Ishibashi Japan 01-07 Var A new inner model with a higher horizontal T. Kadowaki and K. Yoshimoto resolution (TL319) in JMA’s Global 4D-Var data Japan 01-09 assimilation system Assimilation experiments involving surface-sensitive M. Kazumori microwave radiances in JMA’s global data Japan 01-11 assimilation system Initial assessment of FY-3A microwave temperature M. Kazumori and H. Murata sounder radiance data in JMA’s global data Japan 01-13 assimilation system T. Kuroda, T. Fujita, H. Seko Construction of Mesoscale LETKF Data Assimilation Japan 01-15 and K. Saito Experiment System N. Saint-Ramond, A. Forecast sensitivity to observations at Météo-France Doerenbecher, F. Rabier, Application to GPS radio-occultation data France 01-17 V. Guidard, N. Fourrié GPS TPW Assimilation with the JMA Nonhydrostatic K. Saito, Y. Shoji, S. Origuchi, 4DVAR and Cloud Resolving Ensemble Forecast for Japan 01-19 L. Duc and H. Seko the 2008 August Tokyo Metropolitan Area Local Heavy Rainfalls H. Seko, S. Kogure and T. Observation System Simulation Experiments of Japan 01-21 Tsuda Quasi-Zenith Satellite H. Seko, K. Saito, O. Suzuki and Impacts of the low-level convergence data on the A. -
4. the TROPICS—HJ Diamond and CJ Schreck, Eds
4. THE TROPICS—H. J. Diamond and C. J. Schreck, Eds. Pacific, South Indian, and Australian basins were a. Overview—H. J. Diamond and C. J. Schreck all particularly quiet, each having about half their The Tropics in 2017 were dominated by neutral median ACE. El Niño–Southern Oscillation (ENSO) condi- Three tropical cyclones (TCs) reached the Saffir– tions during most of the year, with the onset of Simpson scale category 5 intensity level—two in the La Niña conditions occurring during boreal autumn. North Atlantic and one in the western North Pacific Although the year began ENSO-neutral, it initially basins. This number was less than half of the eight featured cooler-than-average sea surface tempera- category 5 storms recorded in 2015 (Diamond and tures (SSTs) in the central and east-central equatorial Schreck 2016), and was one fewer than the four re- Pacific, along with lingering La Niña impacts in the corded in 2016 (Diamond and Schreck 2017). atmospheric circulation. These conditions followed The editors of this chapter would like to insert two the abrupt end of a weak and short-lived La Niña personal notes recognizing the passing of two giants during 2016, which lasted from the July–September in the field of tropical meteorology. season until late December. Charles J. Neumann passed away on 14 November Equatorial Pacific SST anomalies warmed con- 2017, at the age of 92. Upon graduation from MIT siderably during the first several months of 2017 in 1946, Charlie volunteered as a weather officer in and by late boreal spring and early summer, the the Navy’s first airborne typhoon reconnaissance anomalies were just shy of reaching El Niño thresh- unit in the Pacific. -
Tracking the Origin and Dispersion of Contaminated Sediments Transported by Rivers Draining the Fukushima Radioactive Contaminant Plume
Sediment Dynamics from the Summit to the Sea 237 (Proceedings of a symposium held in New Orleans, Louisiana, USA, 11–14 December 2014) (IAHS Publ. 367, 2014). Tracking the origin and dispersion of contaminated sediments transported by rivers draining the Fukushima radioactive contaminant plume HUGO LEPAGE1, OLIVIER EVRARD1, YUICHI ONDA2, CAROLINE CHARTIN1, IRENE LEFEVRE1, AYRAULT SOPHIE1 & PHILIPPE BONTE1 1 Laboratoire des Sciences du Climat et de l’Environnement (CEA, CNRS,UVSQ), F-91198 Gif-sur-Yvette France [email protected] 2 Center for Research in Isotopes and Environmental Dynamics (CRIED), Tsukuba University, Tsukuba, Japan Abstract This study was conducted in several catchments draining the main Fukushima Dai-ichi Power Plant contaminant plume in Fukushima prefecture, Japan. We collected soils and sediment drape deposits (n = 128) and investigated the variation in 137Cs enrichment during five sampling campaigns, conducted every six months, which typically occurred after intense erosive events such as typhoons and snowmelt. We show that upstream contaminated soils are eroded during summer typhoons (June–October) before being exported during the spring snowmelt (March–April). However, this seasonal cycle of sediment dispersion is further complicated by the occurrence of dam releases that may discharge large amounts of contaminants to the coastal plains during the coming years. Key words erosion; sediment; soil; Fukushima; radio-caesium; enrichment factor INTRODUCTION The Tohoku earthquake and the subsequent tsunami that occurred on 11 March 2011 impacted the Fukushima Dai-Ichi Nuclear Power Plant (FDNPP) and led to a significant atmospheric release of 137 radionuclides such as Cs (T1/2 = 30 years). About 80% of the release was transported out and over the Pacific Ocean, with the rest primarily deposited on the soils of Fukushima Prefecture as a result of wet atmospheric fallout. -
6 2. Annual Summaries of the Climate System in 2009 2.1 Climate In
2. Annual summaries of the climate system in above normal in Okinawa/Amami because hot and 2009 sunny weather was dominant under the subtropical high in July and August. 2.1 Climate in Japan (d) Autumn (September – November 2009, Fig. 2.1.1 Average surface temperature, precipitation 2.1.4d) amounts and sunshine durations Seasonal mean temperatures were near normal in The annual anomaly of the average surface northern and Eastern Japan, although temperatures temperature over Japan (averaged over 17 observatories swung widely. In Okinawa/Amami, seasonal mean confirmed as being relatively unaffected by temperatures were significantly above normal due to urbanization) in 2009 was 0.56°C above normal (based the hot weather in the first half of autumn. Monthly on the 1971 – 2000 average), and was the seventh precipitation amounts were significantly below normal highest since 1898. On a longer time scale, average nationwide in September due to dominant anticyclones. surface temperatures have been rising at a rate of about In contrast, in November, they were significantly 1.13°C per century since 1898 (Fig. 2.1.1). above normal in Western Japan under the influence of the frequent passage of cyclones and fronts around 2.1.2 Seasonal features Japan. In October, Typhoon Melor (0918) made (a) Winter (December 2008 – February 2009, Fig. landfall on mainland Japan, bringing heavy rainfall and 2.1.4a) strong winds. Since the winter monsoon was much weaker than (e) December 2009 usual, seasonal mean temperatures were above normal In the first half of December, temperatures were nationwide. In particular, they were significantly high above normal nationwide, and heavy precipitation was in Northern Japan, Eastern Japan and Okinawa/Amami. -
Global Catastrophe Review – 2015
GC BRIEFING An Update from GC Analytics© March 2016 GLOBAL CATASTROPHE REVIEW – 2015 The year 2015 was a quiet one in terms of global significant insured losses, which totaled around USD 30.5 billion. Insured losses were below the 10-year and 5-year moving averages of around USD 49.7 billion and USD 62.6 billion, respectively (see Figures 1 and 2). Last year marked the lowest total insured catastrophe losses since 2009 and well below the USD 126 billion seen in 2011. 1 The most impactful event of 2015 was the Port of Tianjin, China explosions in August, rendering estimated insured losses between USD 1.6 and USD 3.3 billion, according to the Guy Carpenter report following the event, with a December estimate from Swiss Re of at least USD 2 billion. The series of winter storms and record cold of the eastern United States resulted in an estimated USD 2.1 billion of insured losses, whereas in Europe, storms Desmond, Eva and Frank in December 2015 are expected to render losses exceeding USD 1.6 billion. Other impactful events were the damaging wildfires in the western United States, severe flood events in the Southern Plains and Carolinas and Typhoon Goni affecting Japan, the Philippines and the Korea Peninsula, all with estimated insured losses exceeding USD 1 billion. The year 2015 marked one of the strongest El Niño periods on record, characterized by warm waters in the east Pacific tropics. This was associated with record-setting tropical cyclone activity in the North Pacific basin, but relative quiet in the North Atlantic. -
NASA Sees Typhoon Noru Raging Near the Minami Tori Shima Atoll 24 July 2017
NASA sees Typhoon Noru raging near the Minami Tori Shima Atoll 24 July 2017 north latitude and 154.9 degrees east longitude. That's about 128 nautical miles north of Minami Tori Shima. It was moving to the east-southeast at 13.8 mph (12 knots/22.2 kph). Noru is located to the southwest of Tropical Storm Koru, which is a much smaller and weaker storm. Noru is moving in a cyclonic loop and is forecast to turn back toward the west by July 26. The Joint Typhoon Warning Center's forecast calls for the storm to approach the island of Iwo To, Japan around July 29. Provided by NASA's Goddard Space Flight Center On July 24 at 0342 UTC (July 23 at 11:42 p.m. EDT) NASA-NOAA's Suomi NPP satellite captured a visible image of Typhoon Noru in the Northwestern Pacific Ocean. Credit: NASA/NOAA NASA-NOAA's Suomi NPP satellite captured an image of Typhoon Noru raging near the unpopulated atoll of Minami Tori Shima in the Northwestern Pacific Ocean. Minami-Tori-shima or Marcus Island is an isolated Japanese coral atoll about 1,150 miles (1,850 kilometers) southeast of Tokyo. On July 24 at 0342 UTC (July 23 at 11:42 p.m. EDT), the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument aboard NASA-NOAA's Suomi NPP satellite provided a visible-light image of Typhoon Noru. The VIIRS image showed a cloud-covered eye surrounded by a thick band of powerful thunderstorms and a thick band wrapping into the center from the southeastern quadrant. -
NASA Satellite Sees Typhoon Noru in Infrared Light 31 July 2017
NASA satellite sees Typhoon Noru in infrared light 31 July 2017 To Island, Japan. Maximum sustained winds were near 143.8 mph (125 knots/231 kph). Noru was moving to the west at 6.9 mph (6 knots/11.1 kph). The Joint Typhoon Warning Center forecasts Noru to move slowly to the northwest over the next several days and move toward Kyushu, Japan. Noru is expected to near Kyushu around August 5. Kyushu is the third biggest island of Japan and located farthest southwest of Japan's four main islands. Provided by NASA's Goddard Space Flight Center NASA-NOAA's Suomi NPP satellite captured this infrared image of Typhoon Noru on July 30, 2017, at 11:50 a.m. EDT (1550 UTC) in the Northwestern Pacific Ocean. Credit: University of Wisconsin- Madison/CIMSS/William Straka III NASA-NOAA's Suomi NPP satellite captured an infrared image of Typhoon Noru that showed the structure and cloud top temperatures of the powerful thunderstorms circling its eye. On July 27, 2017 at 12:24 a.m. EDT (0424 UTC) the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument aboard NASA-NOAA's Suomi NPP satellite provided an infrared image of Typhoon Noru. The VIIRS image revealed very cold cloud top temperatures as cold as 190 Kelvin (minus 83.1 degrees Celsius/minus 117.7 degrees Fahrenheit) in thunderstorms circling the eye. Thunderstorms with cloud tops that high in the troposphere have been shown to generate heavy rain. At 11 a.m. EDT (1500 UTC) on July 30, the center of Typhoon Noru was located near 23.0 degrees north latitude and 139.3 degrees east longitude. -
Appendix 8: Damages Caused by Natural Disasters
Building Disaster and Climate Resilient Cities in ASEAN Draft Finnal Report APPENDIX 8: DAMAGES CAUSED BY NATURAL DISASTERS A8.1 Flood & Typhoon Table A8.1.1 Record of Flood & Typhoon (Cambodia) Place Date Damage Cambodia Flood Aug 1999 The flash floods, triggered by torrential rains during the first week of August, caused significant damage in the provinces of Sihanoukville, Koh Kong and Kam Pot. As of 10 August, four people were killed, some 8,000 people were left homeless, and 200 meters of railroads were washed away. More than 12,000 hectares of rice paddies were flooded in Kam Pot province alone. Floods Nov 1999 Continued torrential rains during October and early November caused flash floods and affected five southern provinces: Takeo, Kandal, Kampong Speu, Phnom Penh Municipality and Pursat. The report indicates that the floods affected 21,334 families and around 9,900 ha of rice field. IFRC's situation report dated 9 November stated that 3,561 houses are damaged/destroyed. So far, there has been no report of casualties. Flood Aug 2000 The second floods has caused serious damages on provinces in the North, the East and the South, especially in Takeo Province. Three provinces along Mekong River (Stung Treng, Kratie and Kompong Cham) and Municipality of Phnom Penh have declared the state of emergency. 121,000 families have been affected, more than 170 people were killed, and some $10 million in rice crops has been destroyed. Immediate needs include food, shelter, and the repair or replacement of homes, household items, and sanitation facilities as water levels in the Delta continue to fall.