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Summary of 2014 NW Pacific Typhoon Season and Verification of Authors’ Seasonal Forecasts
Summary of 2014 NW Pacific Typhoon Season and Verification of Authors’ Seasonal Forecasts Issued: 27th January 2015 by Dr Adam Lea and Professor Mark Saunders Dept. of Space and Climate Physics, UCL (University College London), UK. Summary The 2014 NW Pacific typhoon season was characterised by activity slightly below the long-term (1965-2013) norm. The TSR forecasts over-predicted activity but mostly to within the forecast error. The Tropical Storm Risk (TSR) consortium presents a validation of their seasonal forecasts for the NW Pacific basin ACE index, numbers of intense typhoons, numbers of typhoons and numbers of tropical storms in 2014. These forecasts were issued on the 6th May, 3rd July and the 5th August 2014. The 2014 NW Pacific typhoon season ran from 1st January to 31st December. Features of the 2014 NW Pacific Season • Featured 23 tropical storms, 12 typhoons, 8 intense typhoons and a total ACE index of 273. These numbers were respectively 12%, 25%, 0% and 7% below their corresponding long-term norms. Seven out of the last eight years have now had a NW Pacific ACE index below the 1965-2013 climate norm value of 295. • The peak months of August and September were unusually quiet, with only one typhoon forming within the basin (Genevieve formed in the NE Pacific and crossed into the NW Pacific basin as a hurricane). Since 1965 no NW Pacific typhoon season has seen less than two typhoons develop within the NW Pacific basin during August and September. This lack of activity in 2014 was in part caused by an unusually strong and persistent suppressing phase of the Madden-Julian Oscillation. -
Improved Global Tropical Cyclone Forecasts from NOAA: Lessons Learned and Path Forward
Improved global tropical cyclone forecasts from NOAA: Lessons learned and path forward Dr. Vijay Tallapragada Chief, Global Climate and Weather Modeling Branch & HFIP Development Manager Typhoon Seminar, JMA, Tokyo, Japan. NOAA National Weather Service/NCEP/EMC, USA January 6, 2016 Typhoon Seminar JMA, January 6, 2016 1/90 Rapid Progress in Hurricane Forecast Improvements Key to Success: Community Engagement & Accelerated Research to Operations Effective and accelerated path for transitioning advanced research into operations Typhoon Seminar JMA, January 6, 2016 2/90 Significant improvements in Atlantic Track & Intensity Forecasts HWRF in 2012 HWRF in 2012 HWRF in 2015 HWRF HWRF in 2015 in 2014 Improvements of the order of 10-15% each year since 2012 What it takes to improve the models and reduce forecast errors??? • Resolution •• ResolutionPhysics •• DataResolution Assimilation Targeted research and development in all areas of hurricane modeling Typhoon Seminar JMA, January 6, 2016 3/90 Lives Saved Only 36 casualties compared to >10000 deaths due to a similar storm in 1999 Advanced modelling and forecast products given to India Meteorological Department in real-time through the life of Tropical Cyclone Phailin Typhoon Seminar JMA, January 6, 2016 4/90 2014 DOC Gold Medal - HWRF Team A reflection on Collaborative Efforts between NWS and OAR and international collaborations for accomplishing rapid advancements in hurricane forecast improvements NWS: Vijay Tallapragada; Qingfu Liu; William Lapenta; Richard Pasch; James Franklin; Simon Tao-Long -
Chun-Chieh Wu (吳俊傑) Department of Atmospheric Sciences, National Taiwan University No. 1, Sec. 4, Roosevelt Rd., Taipei 1
Chun-Chieh Wu (吳俊傑) Department of Atmospheric Sciences, National Taiwan University No. 1, Sec. 4, Roosevelt Rd., Taipei 106, Taiwan Telephone & Facsimile: (886) 2-2363-2303 Email: [email protected], WWW: http://typhoon.as.ntu.edu.tw Date of Birth: 30 July, 1964 Education: Graduate: Massachusetts Institute of Technology, Ph.D., Department of Earth Atmospheric, and Planetary Sciences, May 1993 Thesis under the supervision of Professor Kerry A. Emanuel on "Understanding hurricane movement using potential vorticity: A numerical model and an observational study." Undergraduate: National Taiwan University, B.S., Department of Atmospheric Sciences, June 1986 Recent Positions: Professor and Chairman Department of Atmospheric Sciences, National Taiwan University August 2008 to present Director NTU Typhoon Research Center January 2009 to present Adjunct Research Scientist Lamont-Doherty Earth Observatory, Columbia University July 2004 - present Professor Department of Atmospheric Sciences, National Taiwan University August 2000 to 2008 Visiting Fellow Geophysical Fluid Dynamics Laboratory, Princeton University January – July, 2004 (on sabbatical leave from NTU) Associate Professor Department of Atmospheric Sciences, National Taiwan University August 1994 to July 2000 Visiting Research Scientist Geophysical Fluid Dynamics Laboratory, Princeton University August 1993 – November 1994; July to September 1995 1 Awards: Gold Bookmarker Prize Wu Ta-You Popular Science Book Prize in Translation Wu Ta-You Foundation, 2008 Outstanding Teaching Award, National Taiwan University, 2008 Outstanding Research Award, National Science Council, 2007 Research Achievement Award, National Taiwan Univ., 2004 University Teaching Award, National Taiwan University, 2003, 2006, 2007 Academia Sinica Research Award for Junior Researchers, 2001 Memberships: Member of the American Meteorological Society. Member of the American Geophysical Union. -
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. -
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. -
A Climatology Model for Forecasting Typhoon Rainfall in Taiwan
Natural Hazards (2006) 37:87–105 Ó Springer 2006 DOI 10.1007/s11069-005-4658-8 A Climatology Model for Forecasting Typhoon Rainfall in Taiwan CHENG-SHANG LEE1,2,w, LI-RUNG HUANG2, HORNG-SYI SHEN2 and SHI-TING WANG3 1Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan, ROC; 2Meteorology Division, National S&T Center for Disaster Reduction, Taipei, Taiwan, ROC; 3Central Weather Bureau, Taiwan, ROC Abstract. The continuous torrential rain associated with a typhoon often caused flood, landslide or debris flow, leading to serious damages to Taiwan. Thus, a usable scheme to forecast rainfall amount during a typhoon period is highly desired. An analysis using hourly rainfall amounts taken at 371 stations during 1989–2001 showed that the topographical lifting of typhoon circulation played an important role in producing heavier rainfall. A climatology model for typhoon rainfall, which considered the topographical lifting and the variations of rain rate with radius was then developed. The model could provide hourly rainfall at any station or any river basin for a given typhoon center. The cumulative rainfall along the forecasted typhoon track was also available. The results showed that the R2 value between the model estimated and the observed cumulative rainfall during the typhoon period for the Dan- Shui (DSH) and Kao-Ping (KPS) River Basins reached 0.70 and 0.81, respectively. The R2 values decreased slightly to 0.69 and 0.73 if individual stations were considered. However, the values decreased significantly to 0.40 and 0.51 for 3-hourly rainfalls, indicating the strong influence of the transient features in producing the heavier rainfall. -
Concentric Eyewall Formation in Typhoon Sinlaku (2008). Part I: Assimilation of T-PARC Data Based on the Ensemble Kalman Filter (Enkf)
506 MONTHLY WEATHER REVIEW VOLUME 140 Concentric Eyewall Formation in Typhoon Sinlaku (2008). Part I: Assimilation of T-PARC Data Based on the Ensemble Kalman Filter (EnKF) CHUN-CHIEH WU,YI-HSUAN HUANG, AND GUO-YUAN LIEN Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan (Manuscript received 4 March 2011, in final form 11 November 2011) ABSTRACT Typhoon Sinlaku (2008) is a case in point under The Observing System Research and Predictability Ex- periment (THORPEX) Pacific Asian Regional Campaign (T-PARC) with the most abundant flight obser- vations taken and with great potential to address major scientific issues in T-PARC such as structure change, targeted observations, and extratropical transition. A new method for vortex initialization based on ensemble Kalman filter (EnKF) data assimilation and the Weather Research and Forecasting (WRF) model is adopted in this study. By continuously assimilating storm positions (with an update cycle every 30 min), the mean surface wind structure, and all available measurement data, this study constructs a unique high-spatial/ temporal-resolution and model/observation-consistent dataset for Sinlaku during a 4-day period. Simulations of Sinlaku starting at different initial times are further investigated to assess the impact of the data. It is striking that some of the simulations are able to capture Sinlaku’s secondary eyewall formation, while others starting the simulation earlier with less data assimilated are not. This dataset provides a unique opportunity to study the dynamical processes of concentric eyewall formation in Sinlaku. In Part I of this work, results from the data assimilation and simulations are presented, including concentric eyewall evolution and the precursors to its formation, while detailed dynamical analyses are conducted in follow-up research. -
Economic Analysis of Disaster Management Investment Effectiveness in Korea
sustainability Article Economic Analysis of Disaster Management Investment Effectiveness in Korea Bo-Young Heo 1 and Won-Ho Heo 2,* 1 National Disaster Management Research Institute, Ulsan 44538, Korea; [email protected] 2 School of Civil and Environmental Engineering, Yonsei University, 50 Yonsei-ro Seodaemun-gu, Seoul 03722, Korea * Correspondence: [email protected]; Tel.: +82-52-928-8112 Received: 12 March 2019; Accepted: 21 May 2019; Published: 28 May 2019 Abstract: Governments have been investing in extensive operations to minimize economic losses and casualties from natural disasters such as floods and storms. A suitable verification process is required to guarantee maximum effectiveness and efficiency of investments while ensuring sustained funding. Active investment can be expected by verifying the effectiveness of disaster prevention spending. However, the results of the budget invested in disaster-safety-related projects are not immediate but evident only over a period of time. Additionally, their effects should be verified in terms of the state or society overall, not from an individualistic perspective because of the nature of public projects. In this study, an economic analysis of the short- and long-term effects of investment in a disaster-safety-related project was performed and the effects of damage reduction before and after project implementation were analyzed to evaluate the short-term effects and a cost–benefit analysis was conducted to assess the long-term effects. The results show that disaster prevention projects reduce damages over both the short and long term. Therefore, investing in preventive projects to cope with disasters effectively is important to maximize the return on investment. -
The Effect of Typhoon on POC Flux
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Biogeosciences Discuss., 7, 3521–3550, 2010 Biogeosciences www.biogeosciences-discuss.net/7/3521/2010/ Discussions BGD doi:10.5194/bgd-7-3521-2010 7, 3521–3550, 2010 © Author(s) 2010. CC Attribution 3.0 License. The effect of typhoon This discussion paper is/has been under review for the journal Biogeosciences (BG). on POC flux Please refer to the corresponding final paper in BG if available. C.-C. Hung et al. The effect of typhoon on particulate Title Page Abstract Introduction organic carbon flux in the southern East Conclusions References China Sea Tables Figures C.-C. Hung1, G.-C. Gong1, W.-C. Chou1, C.-C. Chung1,2, M.-A. Lee3, Y. Chang3, J I H.-Y. Chen4, S.-J. Huang4, Y. Yang5, W.-R. Yang5, W.-C. Chung1, S.-L. Li1, and 6 E. Laws J I 1Institute of Marine Environmental Chemistry and Ecology, National Taiwan Ocean University Back Close Keelung, 20224, Taiwan 2Center for Marine Bioscience and Biotechnology, National Taiwan Ocean University Keelung, Full Screen / Esc 20224, Taiwan 3 Department of Environmental Biology and Fisheries Science, National Taiwan Ocean Printer-friendly Version University, 20224, Taiwan 4Department of Marine Environmental Informatics, National Taiwan Ocean University, Interactive Discussion Keelung, 20224, Taiwan 5Taiwan Ocean Research Institute, National Applied Research Laboratories, Taipei, Taiwan 3521 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | BGD 6 Department of Environmental Sciences, School of the Coast and Environment, Louisiana 7, 3521–3550, 2010 State University, Baton Rouge, LA 70803, USA Received: 16 April 2010 – Accepted: 7 May 2010 – Published: 19 May 2010 The effect of typhoon on POC flux Correspondence to: C.-C. -
Philippines: 106 Dead* China
Creation date: 20 Feb 2015 Philippines, China: Typhoon RAMMASUN, Flood and landslide Philippines, China Country Philippines: Northern and central parts of the country Philippines: 106 dead* and China: Southern part District China: 62 dead* Duration 15 Jul 2014- Typhoon Rammasun that landed on the eastern part of Philippines: 5 missing* Philippines on 15 Jul, moved across Luzon Island and made Outline final landfall in southern China. Rammasun was the most powerful typhoon that hit southern China in 40 years. 106 China: 21 missing* people in Philippines, and 62 in China were killed. *Philippines: Reported on 16 Sep 2014 *China: Reported on 27 Jul 2014 Photo 1 A man gathering bamboos that drifted to the bridge due to the Typhoon Rammasun, in Batangas in the southwest of Manila (17 Jul 2014) Source http://www.afpbb.com/articles/-/3020815 Copyright © 1956 Infrastructure Development Institute – Japan. All Rights Reserved. The reproduction or republication of this material is strictly prohibited without the prior written permission of IDI. 一般社団法人 国際建設技術協会 Infrastructure Development Institute – Japan Photo 2 Residents heading to an evacuation shelter in the strong wind and heavy rain caused by the typhoon in Manila (16 Jul 2014) Source http://www.afpbb.com/articles/-/3020815?pid=14054270 Photo 3 A resident climbs on a bridge destroyed during the onslaught of Typhoon Rammasun, (locally named Glenda) in Batangas city south of Manila, July 17, 2014. Source http://www.reuters.com/article/2014/07/17/us-philippines-typhoon-idUSKBN0FM01320140717 Photo 4 A person taking photos of storm-swept sea in Hainan province (18 Jul 2014) Source http://www.afpbb.com/articles/-/3021050?pid=14066126 Copyright © 1956 Infrastructure Development Institute – Japan. -
On the Extreme Rainfall of Typhoon Morakot (2009)
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116, D05104, doi:10.1029/2010JD015092, 2011 On the extreme rainfall of Typhoon Morakot (2009) Fang‐Ching Chien1 and Hung‐Chi Kuo2 Received 21 September 2010; revised 17 December 2010; accepted 4 January 2011; published 4 March 2011. [1] Typhoon Morakot (2009), a devastating tropical cyclone (TC) that made landfall in Taiwan from 7 to 9 August 2009, produced the highest recorded rainfall in southern Taiwan in the past 50 years. This study examines the factors that contributed to the heavy rainfall. It is found that the amount of rainfall in Taiwan was nearly proportional to the reciprocal of TC translation speed rather than the TC intensity. Morakot’s landfall on Taiwan occurred concurrently with the cyclonic phase of the intraseasonal oscillation, which enhanced the background southwesterly monsoonal flow. The extreme rainfall was caused by the very slow movement of Morakot both in the landfall and in the postlandfall periods and the continuous formation of mesoscale convection with the moisture supply from the southwesterly flow. A composite study of 19 TCs with similar track to Morakot shows that the uniquely slow translation speed of Morakot was closely related to the northwestward‐extending Pacific subtropical high (PSH) and the broad low‐pressure systems (associated with Typhoon Etau and Typhoon Goni) surrounding Morakot. Specifically, it was caused by the weakening steering flow at high levels that primarily resulted from the weakening PSH, an approaching short‐wave trough, and the northwestward‐tilting Etau. After TC landfall, the circulation of Goni merged with the southwesterly flow, resulting in a moisture conveyer belt that transported moisture‐laden air toward the east‐northeast.