Application of WRF 3DVAR to Operational Typhoon Prediction in Taiwan: Impact of Outer Loop and Partial Cycling Approaches
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Typhoon Hagupit (Ruby), Dec
Typhoon Hagupit (Ruby), Dec. 9, 2014 CDIR No. 6 BLUF – Implications to PACOM No DOD requirements anticipated PACOM Joint Liaison Group re-deploying from Philippines within next 72 hours (PACOM J35) Typhoon Hagupit – Stats & Facts Summary: (The following times in this report are Phil. local time unless otherwise specified) Current Status: Typhoon Hagupit has weakened into a tropical depression as it heads west into the West Philippine Sea towards Vietnam. All public storm warning signals have been lifted. Storm expected to head out of the Philippine Area of Responsibility (PAR) Thursday (11 DEC) early AM. Est. rainfall is 5 – 15 mm per hour (Moderate – heavy) within the 200 km of the storm. (NDRRMC, Bulletin No. 23) Local officials reported nearly 13,000 houses were destroyed and more than 22,300 were partially damaged in Eastern Samar province, where Hagupit first hit as a CAT 3 typhoon on 6 DEC. (Reuters) Deputy Presidential Spokesperson Key Concerns & Trends Abigail Valte said so far, Dolores appears worst hit. (GPH) Domestic air and sea travel has resumed, markets reopened • GPH and the international humanitarian community are and state workers returned to their offices. Some shopping capable of meeting virtually all disaster response requirements. Major malls were open but schools remained closed. actions and activities include: The privately run National Grid Corp said nearly two million Assessments are ongoing to determine the full extent of the homes across central Philippines and southern Luzon remain typhoon’s impact; reports so far indicate the scale and severity without power. (Reuters) Twenty provinces in six regions of the impact of Hagupit was not as great as initially feared. -
Wang, M., M. Xue, and K. Zhao (2016), September 2008
PUBLICATIONS Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE The impact of T-TREC-retrieved wind and radial 10.1002/2015JD024001 velocity data assimilation using EnKF Key Points: and effects of assimilation window • T-TREC-retrieved wind and radial velocity data are assimilated using an on the analysis and prediction ensemble Kalman filter • The relative impacts of two data sets of Typhoon Jangmi (2008) on analysis and prediction changes with assimilation windows Mingjun Wang1,2, Ming Xue1,2,3, and Kun Zhao1 • The combination of retrieved wind and radial velocity produces better 1Key Laboratory for Mesoscale Severe Weather/MOE and School of Atmospheric Science, Nanjing University, Nanjing, analyses and forecasts China, 2Center for Analysis and Prediction of Storms, Norman, Oklahoma, USA, 3School of Meteorology, University of Oklahoma, Norman, Oklahoma, USA Correspondence to: M. Xue, Abstract This study examines the relative impact of assimilating T-TREC-retrieved winds (VTREC)versusradial [email protected] velocity (Vr) on the analysis and forecast of Typhoon Jangmi (2008) using an ensemble Kalman filter (EnKF). The VTREC and Vr data at 30 min intervals are assimilated into the ARPS model at 3 km grid spacing over four different Citation: assimilation windows that cover, respectively, 0000–0200, 0200–0400, 0400–0600, and 0000–0600 UTC, 28 Wang, M., M. Xue, and K. Zhao (2016), September 2008. The assimilation of VTREC data produces better analyses of the typhoon structure and intensity The impact of T-TREC-retrieved wind and radial velocity data assimilation than the assimilation of Vr data during the earlier assimilation windows, but during the later assimilation using EnKF and effects of assimilation windows when the coverage of Vr data on the typhoon from four Doppler radars is much improved, the window on the analysis and prediction assimilation of V outperforms V data. -
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. -
The Influence of Assimilating Dropsonde Data on Typhoon Track
908 MONTHLY WEATHER REVIEW VOLUME 139 The Influence of Assimilating Dropsonde Data on Typhoon Track and Midlatitude Forecasts MARTIN WEISSMANN,* FLORIAN HARNISCH,* CHUN-CHIEH WU,1 PO-HSIUNG LIN,1 YOICHIRO OHTA,# KOJI YAMASHITA,# YEON-HEE KIM,@ EUN-HEE JEON,@ TETSUO NAKAZAWA,& AND SIM ABERSON** * Deutsches Zentrum fu¨r Luft- und Raumfahrt, Institut fu¨r Physik der Atmospha¨re, Oberpfaffenhofen, Germany 1 Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan # Japan Meteorological Agency, Tokyo, Japan @ National Institute of Meteorological Research, Korea Meteorological Agency, Seoul, South Korea & Meteorological Research Institute, Tsukuba, Japan ** NOAA/AOML/Hurricane Research Division, Miami, Florida (Manuscript received 9 February 2010, in final form 21 April 2010) ABSTRACT A unique dataset of targeted dropsonde observations was collected during The Observing System Re- search and Predictability Experiment (THORPEX) Pacific Asian Regional Campaign (T-PARC) in the autumn of 2008. The campaign was supplemented by an enhancement of the operational Dropsonde Ob- servations for Typhoon Surveillance near the Taiwan Region (DOTSTAR) program. For the first time, up to four different aircraft were available for typhoon observations and over 1500 additional soundings were collected. This study investigates the influence of assimilating additional observations during the two major typhoon events of T-PARC on the typhoon track forecast by the global models of the European Centre for Medium- Range Weather Forecasts (ECMWF), the Japan Meteorological Agency (JMA), the National Centers for Environmental Prediction (NCEP), and the limited-area Weather Research and Forecasting (WRF) model. Additionally, the influence of T-PARC observations on ECMWF midlatitude forecasts is investigated. All models show an improving tendency of typhoon track forecasts, but the degree of improvement varied from about 20% to 40% in NCEP and WRF to a comparably low influence in ECMWF and JMA. -
Science Discussion Started: 22 October 2018 C Author(S) 2018
Discussions Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2018-127 Earth System Manuscript under review for journal Earth Syst. Sci. Data Science Discussion started: 22 October 2018 c Author(s) 2018. CC BY 4.0 License. Open Access Open Data 1 Field Investigations of Coastal Sea Surface Temperature Drop 2 after Typhoon Passages 3 Dong-Jiing Doong [1]* Jen-Ping Peng [2] Alexander V. Babanin [3] 4 [1] Department of Hydraulic and Ocean Engineering, National Cheng Kung University, Tainan, 5 Taiwan 6 [2] Leibniz Institute for Baltic Sea Research Warnemuende (IOW), Rostock, Germany 7 [3] Department of Infrastructure Engineering, Melbourne School of Engineering, University of 8 Melbourne, Australia 9 ---- 10 *Corresponding author: 11 Dong-Jiing Doong 12 Email: [email protected] 13 Tel: +886 6 2757575 ext 63253 14 Add: 1, University Rd., Tainan 70101, Taiwan 15 Department of Hydraulic and Ocean Engineering, National Cheng Kung University 16 -1 Discussions Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2018-127 Earth System Manuscript under review for journal Earth Syst. Sci. Data Science Discussion started: 22 October 2018 c Author(s) 2018. CC BY 4.0 License. Open Access Open Data 1 Abstract 2 Sea surface temperature (SST) variability affects marine ecosystems, fisheries, ocean primary 3 productivity, and human activities and is the primary influence on typhoon intensity. SST drops 4 of a few degrees in the open ocean after typhoon passages have been widely documented; 5 however, few studies have focused on coastal SST variability. The purpose of this study is to 6 determine typhoon-induced SST drops in the near-coastal area (within 1 km of the coast) and 7 understand the possible mechanism. -
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. -
A Vortex Relocation Scheme for Tropical Cyclone Initialization in Advanced Research WRF
3298 MONTHLY WEATHER REVIEW VOLUME 138 A Vortex Relocation Scheme for Tropical Cyclone Initialization in Advanced Research WRF LING-FENG HSIAO Central Weather Bureau, and Taiwan Typhoon and Flood Research Institute, Taipei, Taiwan CHI-SANN LIOU Naval Research Laboratory, Monterey, California TIEN-CHIANG YEH Central Weather Bureau, Taipei, Taiwan YONG-RUN GUO National Center for Atmospheric Research, Boulder, Colorado DER-SONG CHEN,KANG-NING HUANG,CHUEN-TEYR TERNG, AND JEN-HER CHEN Central Weather Bureau, Taipei, Taiwan (Manuscript received 6 November 2009, in final form 23 February 2010) ABSTRACT This paper introduces a relocation scheme for tropical cyclone (TC) initialization in the Advanced Research Weather Research and Forecasting (ARW-WRF) model and demonstrates its application to 70 forecasts of Ty- phoons Sinlaku (2008), Jangmi (2008), and Linfa (2009) for which Taiwan’s Central Weather Bureau (CWB) issued typhoon warnings. An efficient and dynamically consistent TC vortex relocation scheme for the WRF terrain- following mass coordinate has been developed to improve the first guess of the TC analysis, and hence improves the tropical cyclone initialization. The vortex relocation scheme separates the first-guess atmospheric flow into a TC circulation and environmental flow, relocates the TC circulation to its observed location, and adds the relocated TC circulation back to the environmental flow to obtain the updated first guess with a correct TC position. Analysis of these typhoon cases indicates that the relocation procedure moves the typhoon circulation to the observed typhoon position without generating discontinuities or sharp gradients in the first guess. Numerical experiments with and without the vortex relocation procedure for Typhoons Sinlaku, Jangmi, and Linfa forecasts show that about 67% of the first-guess fields need a vortex relocation to correct typhoon position errors while eliminates the topographical effect. -
Report on UN ESCAP / WMO Typhoon Committee Members Disaster Management System
Report on UN ESCAP / WMO Typhoon Committee Members Disaster Management System UNITED NATIONS Economic and Social Commission for Asia and the Pacific January 2009 Disaster Management ˆ ` 2009.1.29 4:39 PM ˘ ` 1 ¿ ‚fiˆ •´ lp125 1200DPI 133LPI Report on UN ESCAP/WMO Typhoon Committee Members Disaster Management System By National Institute for Disaster Prevention (NIDP) January 2009, 154 pages Author : Dr. Waonho Yi Dr. Tae Sung Cheong Mr. Kyeonghyeok Jin Ms. Genevieve C. Miller Disaster Management ˆ ` 2009.1.29 4:39 PM ˘ ` 2 ¿ ‚fiˆ •´ lp125 1200DPI 133LPI WMO/TD-No. 1476 World Meteorological Organization, 2009 ISBN 978-89-90564-89-4 93530 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspon- dence and requests to publish, reproduce or translate this publication in part or in whole should be addressed to: Chairperson, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0) 22 730 84 03 P.O. Box No. 2300 Fax: +41 (0) 22 730 80 40 CH-1211 Geneva 2, Switzerland E-mail: [email protected] NOTE The designations employed in WMO publications and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of WMO concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
Phase Concept for Mudflow Based on the Influence of Viscosity
Soils and Foundations 2013;53(1):77–90 The Japanese Geotechnical Society Soils and Foundations www.sciencedirect.com journal homepage: www.elsevier.com/locate/sandf Phase concept for mudflow based on the influence of viscosity Shannon Hsien-Heng Leen, Budijanto Widjaja1 National Taiwan University of Science and Technology, Department of Construction Engineering, No. 43 Keelung Road, Section 4, Taipei 106, Taiwan Received 22 November 2011; received in revised form 4 July 2012; accepted 1 September 2012 Available online 26 January 2013 Abstract The phase concept implies that the state of soil changes from plastic to viscous liquid as a function of water content. This principle could be used to interpret the behavior of mudflows, the most dangerous mass movements today. When Typhoon Jangmi hit northern Taiwan in 2008, a mudflow occurred in the Maokong area as a result of the high-intensity rainfall. This case was studied using three simulations, each with a different water content. Based on the mudflow classifications, the primary criteria used in this study were flow velocity and solid concentration by volume, while the major rheology parameters directly obtained from our new laboratory device, the flow box test, were yield stress and viscosity. The results show that the mass movement confirmed the aforementioned criteria for mudflow when the water content reaches or exceeds the liquid limit. The flow box test can determine the viscosity for both plastic and viscous liquid states, which is advantageous. Viscosity is important for explaining the general characteristics of mudflow movement because it controls flow velocity. Therefore, the present study successfully elucidates the changes in mudflow from its initiation to its transportation and deposition via a numerical simulation using laboratory rheology parameters. -
Sheared Deep Vortical Convection in Pre‐Depression Hagupit During TCS08 Michael M
GEOPHYSICAL RESEARCH LETTERS, VOL. 37, L06802, doi:10.1029/2009GL042313, 2010 Click Here for Full Article Sheared deep vortical convection in pre‐depression Hagupit during TCS08 Michael M. Bell1,2 and Michael T. Montgomery1,3 Received 28 December 2009; accepted 4 February 2010; published 17 March 2010. [1] Airborne Doppler radar observations from the recent (2008) that occurred during the TCS08 experiment, and Tropical Cyclone Structure 2008 field campaign in the suggested that the pre‐Nuri disturbance was of the easterly western North Pacific reveal the presence of deep, buoyant wave type with the preferred location for storm genesis near and vortical convective features within a vertically‐sheared, the center of the cat’s eye recirculation region that was readily westward‐moving pre‐depression disturbance that later apparent in the frame of reference moving with the wave developed into Typhoon Hagupit. On two consecutive disturbance. This work suggests that this new cyclogenesis days, the observations document tilted, vertically coherent model is applicable in easterly flow regimes and can prove precipitation, vorticity, and updraft structures in response to useful for tropical weather forecasting in the WPAC. It the complex shearing flows impinging on and occurring reaffirms also that easterly waves or other westward propa- within the disturbance near 18 north latitude. The observations gating disturbances are often important ingredients in the and analyses herein suggest that the low‐level circulation of formation process of typhoons [Chang, 1970; Reed and the pre‐depression disturbance was enhanced by the coupling Recker, 1971; Ritchie and Holland, 1999]. Although the of the low‐level vorticity and convergence in these deep Nuri study offers compelling support for the large‐scale convective structures on the meso‐gamma scale, consistent ingredients of this new tropical cyclogenesis model [Dunkerton with recent idealized studies using cloud‐representing et al., 2009], it leaves open important unanswered questions numerical weather prediction models. -
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. -
The Impact of Dropwindsonde Observations on Typhoon Track Forecasts in DOTSTAR and T-PARC
1728 MONTHLY WEATHER REVIEW VOLUME 139 The Impact of Dropwindsonde Observations on Typhoon Track Forecasts in DOTSTAR and T-PARC KUN-HSUAN CHOU Department of Atmospheric Sciences, Chinese Culture University, Taipei, Taiwan CHUN-CHIEH WU AND PO-HSIUNG LIN Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan SIM D. ABERSON Hurricane Research Division, NOAA/AOML, Miami, Florida MARTIN WEISSMANN AND FLORIAN HARNISCH Deutsches Zentrum fu¨r Luft- und Raumfahrt (DLR), Institut fu¨r Physik der Atmospha¨re, Oberpfaffenhofen, Germany TETSUO NAKAZAWA Meteorological Research Institute, JMA, Tsukuba, Japan (Manuscript received 3 August 2010, in final form 1 November 2010) ABSTRACT The typhoon surveillance program Dropwindsonde Observations for Typhoon Surveillance near the Taiwan Region (DOTSTAR) has been conducted since 2003 to obtain dropwindsonde observations around tropical cyclones near Taiwan. In addition, an international field project The Observing System Research and Predictability Experiment (THORPEX) Pacific Asian Regional Campaign (T-PARC) in which dropwindsonde observations were obtained by both surveillance and reconnaissance flights was conducted in summer 2008 in the same region. In this study, the impact of the dropwindsonde data on track forecasts is investigated for DOTSTAR (2003–09) and T-PARC (2008) experi- ments. Two operational global models from NCEP and ECMWF are used to evaluate the impact of dropwindsonde data. In addition, the impact on the two-model mean is assessed. The impact of dropwindsonde data on track forecasts is different in the NCEP and ECMWF model systems. Using the NCEP system, the assimilation of dropwindsonde data leads to improvements in 1- to 5-day track forecasts in about 60% of the cases.