Typhoon Kalmaegi (As of 18 Jul 2008)

MONGOLIA RUSSIAN FEDERATION Typhoon Kalmaegi (as of 18 Jul 2008) GMT +8 DPR Beijing KOREA SITUATION • Typhoon Kalmaegi struck REPUBLIC OF JAPAN Taiwan early Friday 18 June KOREA 2008, and is expected to hit the Yellow Tokyo east coast of China Sea • Three-level flood control emergency response to 20 July Typhoon Kalmaegi launched in CHINA China 180,000 evacuated • Storm is expected to cause - Xinhua heavy rains in coastal cities of China over the next two days Shanghai 180,000 evacuated LINKS Zhejiang (30,000 workers East 50,000 persons on shing vessels) Sheng • Latest updates for Typhoon - Xinhua 19 July China Kalmaegi - Jul 2008 • Related maps Sea Fujian Sheng 18 July Quanzhou Taipei Zhangzhou Disclaimers: Xiamen The boundaries and names shown and the designations used on all maps do not imply Taiwan official endorsement or acceptance by the United Nations. 17 July The data and information represented Philippine originates from public sources as indicated. ReliefWeb makes every effort to use the latest available data and to ensure that its products • 6 dead Sea are accurate, complete and timely, but no • 6 injured Basco Typhoon Kalmaegi Track warranties are made to this effect. Comments • 6 missing are welcome to [email protected]. Typhoon Kalmaegi Creation date: 18 July 2008 • T$86.93 million crop damage Predicted Track • T$20 million livestock damage Map sources: UNCS, SALB, GAUL, UNISYS 16 July 14 July - Reuters INTERNATIONAL BOUNDARY Narrative and statistical sources: Gov. of Philippines. NDCC update - Severe Region I 15 July Administrative Boundary weather final bulletin on Typhoon “Helen” South Reuters. Six dead, six missing in wake of Region II Affected Area (Gov. of Waiwan typhoon China Philippines, Xinhua) Xinhua News Agency. East China braces for 31,129 persons aected by weakening storm Kalmaegi, 360,000 oods in Region I and Region II evacuated. Sea National Capital Emergency Response to Typhoon Kalmaegi -Gov. of Philippines PHILIPPINES Populated Place launched. 0 100 Manila www.reliefweb.int Kilometres Office for the Coordination of Humanitarian Affairs United Nations.

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TUESDAY 16* Philippines 3,479* 1,167*
TUESDAY TYPHOON KALMAEGI 19 NOV 2019 PHILIPPINES 1230 HRS (UTC +7) FLASH UPDATE #2 Population Exposed (Estimated exposure by the PDC) Map source: Philippines Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) Initial Effects* *Estimations are based on data reported/confirmed by National Disaster 3,479* 1,167* 15* 16* Management Organisations of each AFFECTED DISPLACED FLOODED DAMAGED respective ASEAN Member State PERSONS PERSONS BARANGAYS HOUSES and other verified sources Philippines • Tropical Storm KALMAEGI (locally named RAMON in the Philippines), which strengthened into a Severe Tropical Storm on 18 November 2019, has now further developed into a Typhoon and currently moving slowly west-northwest towards Babuyan Islands, north of Luzon, Philippines as of 10:00 (UTC+7). • According to forecast by the Joint Typhoon Warning Center (JTWC), Typhoon KALMAEGI is moving at about 4 kph, and is expected to weaken over the next 24 hours. Based on the current forecast (the storm's center and path), the Typhoon is within 112 km from northern seaboard of the Philippines, and the center is expected to make landfall in the afternoon or evening today, 19 November 2019, with sustained winds of about 148 kph. • The Philippines Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) stated that moderate with frequent heavy rains will prevail over Batanes, northern portion of Cagayan (including the Babuyan Islands), Apayao and the northern portion of Ilocos Norte provinces. • The Philippines’ National Disaster Risk Reduction Management Council (NDRRMC) reported flood incidents, ranging from 0.5m to 1m of flood water, in 15 barangays/villages in Camarines Sur and Romblon provinces due to persistent heavy rains associated with the typhoon.
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Upper Ocean Response to Typhoon Kalmaegi and Sarika in the South China Sea from Multiple-Satellite Observations and Numerical Simulations
remote sensing Article Upper Ocean Response to Typhoon Kalmaegi and Sarika in the South China Sea from Multiple-Satellite Observations and Numerical Simulations Xinxin Yue 1, Biao Zhang 1,* ID , Guoqiang Liu 1,2, Xiaofeng Li 3 ID , Han Zhang 4 and Yijun He 1 ID 1 School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China; [email protected] (X.Y.); [email protected] (G.L.); [email protected] (Y.H.) 2 Bedford Institute of Oceanography, Fisheries and Oceans, Dartmouth, NS B2Y 4A2, Canada 3 GST at National Oceanic and Atmospheric Administration (NOAA)/NESDIS, College Park, MD 20740-3818, USA; [email protected] 4 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Hangzhou 310012, China; [email protected] * Correspondence: [email protected] Received: 12 December 2017; Accepted: 22 February 2018; Published: 24 February 2018 Abstract: We investigated ocean surface and subsurface physical responses to Typhoons Kalmaegi and Sarika in the South China Sea, utilizing synergistic multiple-satellite observations, in situ measurements, and numerical simulations. We found signiﬁcant typhoon-induced sea surface cooling using satellite sea surface temperature (SST) observations and numerical model simulations. This cooling was mainly caused by vertical mixing and upwelling. The maximum amplitudes were 6 ◦C and 4.2 ◦C for Typhoons Kalmaegi and Sarika, respectively. For Typhoon Sarika, Argo temperature proﬁle measurements showed that temperature response beneath the surface showed a three-layer vertical structure (decreasing-increasing-decreasing). Satellite salinity observations showed that the maximum increase of sea surface salinity (SSS) was 2.2 psu on the right side of Typhoon Sarika’s track, and the maximum decrease of SSS was 1.4 psu on the left.
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Origin and Maintenance of the Long-Lasting, Outer Mesoscale Convective System in Typhoon Fengshen (2008)
2838 MONTHLY WEATHER REVIEW VOLUME 142 Origin and Maintenance of the Long-Lasting, Outer Mesoscale Convective System in Typhoon Fengshen (2008) BUO-FU CHEN Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan RUSSELL L. ELSBERRY Department of Meteorology, Naval Postgraduate School, Monterey, California CHENG-SHANG LEE Department of Atmospheric Sciences, National Taiwan University, and Taiwan Typhoon and Flood Research Institute, National Applied Research Laboratories, Taipei, Taiwan (Manuscript received 27 January 2014, in final form 21 March 2014) ABSTRACT Outer mesoscale convective systems (OMCSs) are long-lasting, heavy rainfall events separate from the inner-core rainfall that have previously been shown to occur in 22% of western North Pacific tropical cyclones (TCs). Environmental conditions accompanying the development of 62 OMCSs are contrasted with the conditions in TCs that do not include an OMCS. The development, kinematic structure, and maintenance mechanisms of an OMCS that occurred to the southwest of Typhoon Fengshen (2008) are studied with Weather Research and Forecasting Model simulations. Quick Scatterometer (QuikSCAT) observations and the simulations indicate the low-level TC circulation was deflected around the Luzon terrain and caused an elongated, north–south moisture band to be displaced to the west such that the OMCS develops in the outer region of Fengshen rather than spiraling into the center. Strong northeasterly vertical wind shear contributed to frictional convergence in the boundary layer, and then the large moisture flux convergence in this moisture band led to the downstream development of the OMCS when the band interacted with the monsoon flow. As the OMCS developed in the region of low-level monsoon westerlies and midlevel northerlies associated with the outer circulation of Fengshen, the characteristic structure of a rear-fed inflow with a leading stratiform rain area in the cross-line direction (toward the south) was established.
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The Impact of Dropwindsonde on Typhoon Track Forecasts in DOTSTAR and T-PARC
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2008 Tropical Cyclone Review Summarises Last Year’S Global Tropical Cyclone Activity and the Impact of the More Significant Cyclones After Landfall
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<< LINGLING TRACKS OF TROPICAL CYCLONES IN 2019 SEP (), !"#$%&'( ) KROSA AUG @QY HAGIBIS *+ FRANCISCO OCT FAXAI AUG SEP DANAS JUL ? MITAG LEKIMA OCT => AUG TAPAH SEP NARI JUL BUALOI SEPAT OCT JUN SEPAT(1903) JUN HALONG NOV Z[ NEOGURI OCT ab ,- de BAILU FENGSHEN FUNG-WONG AUG NOV NOV PEIPAH SEP Hong Kong => TAPAH (1917) SEP NARI(190 6 ) MUN JUL JUL Z[ NEOGURI (1920) FRANCISCO (1908) :; OCT AUG WIPHA KAJIK() 1914 LEKIMA() 1909 AUG SEP AUG WUTIP *+ MUN(1904) WIPHA(1907) FEB FAXAI(1915) JUL JUL DANAS(190 5 ) de SEP :; JUL KROSA (1910) FUNG-WONG (1927) ./ KAJIKI AUG @QY @c NOV PODUL SEP HAGIBIS() 1919 << ,- AUG > KALMAEGI OCT PHANFONE NOV LINGLING() 1913 BAILU()19 11 \]^ ./ ab SEP AUG DEC FENGSHEN (1925) MATMO PODUL() 191 2 PEIPAH (1916) OCT _` AUG NOV ? SEP HALONG (1923) NAKRI (1924) @c MITAG(1918) NOV NOV _` KALMAEGI (1926) SEP NAKRI KAMMURI NOV NOV DEC \]^ MATMO (1922) OCT BUALOI (1921) KAMMURI (1928) OCT NOV > PHANFONE (1929) DEC WUTIP( 1902) FEB 二零一九年熱帶氣旋 TROPICAL CYCLONES IN 2019 2 二零二零年七月出版 Published July 2020 香港天文台編製香港九龍彌敦道134A Prepared by: Hong Kong Observatory 134A Nathan Road Kowloon, Hong Kong © 版權所有。未經香港天文台台長同意，不得翻印本刊物任何部分內容。 © Copyright reserved. No part of this publication may be reproduced without the permission of the Director of the Hong Kong Observatory. 本刊物的編製和發表，目的是促進資 This publication is prepared and disseminated in the interest of promoting 料交流。香港特別行政區政府(包括其 the exchange of information. The 僱員及代理人)對於本刊物所載資料 Government of the Hong Kong Special 的準確性、完整性或效用，概不作出 Administrative Region
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water Article Response of Coastal Water in the Taiwan Strait to Typhoon Nesat of 2017 Renhao Wu 1,2 , Qinghua Yang 1,3 , Di Tian 4, Bo Han 1,2, Shimei Wu 1,2 and Han Zhang 4,* 1 School of Atmospheric Sciences, and Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Zhuhai 519082, China; [email protected] (R.W.); [email protected] (Q.Y.); [email protected] (B.H.); [email protected] (S.W.) 2 Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China 3 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100039, China 4 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China; [email protected] * Correspondence: [email protected] Received: 29 September 2019; Accepted: 4 November 2019; Published: 7 November 2019 Abstract: The oceanic response of the Taiwan Strait (TWS) to Typhoon Nesat (2017) was investigated using a fully coupled atmosphere-ocean-wave model (COAWST) verified by observations. Ocean currents in the TWS changed drastically in response to significant wind variation during the typhoon. The response of ocean currents was characterised by a flow pattern generally consistent with the Ekman boundary layer theory, with north-eastward volume transport being significantly modified by the storm. Model results also reveal that the western TWS experienced the maximum generated storm surge, whereas the east side experienced only moderate storm surge.
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Application Note Such Disturbances
Weighing Performance during Typhoons Improving Balance Stability ScinoPharm Taiwan Ltd. Environmental disturbances cause issues with balance stability around the world. Peak typhoon season in particular creates significant weighing challenges for users of sensitive balances - measurement issues that standard balance filters simply cannot compensate for. Rather than accept this adverse effect on weighing results, METTLER TOLEDO set out to find a solution that could be utilized during Application Note such disturbances. The result is reliable weighing performance in extreme weather conditions. A typhoon is a mature tropical cyclone that develops in the northwestern part of the Pacific Ocean between 180° and 100°E, commonly referred to as the Northwest Pacific Basin. This region includes all the territory north of the equator and west of the International Date Line, including the South China Sea, and it is the most active basin on Earth, accounting for almost one-third of the world's annual tropical cyclones. While no official “typhoon season” exists, storm activity in the Northwest Pacific Basin tends to be highest from August to October, a period which nearly corresponds to Atlantic hurricane season. Along with high storm frequency, the basin also features the most intense tropical storms on record. Features like warm sea temperatures, atmospheric instability, high humidity, air rotation, and low ver- tical wind shear combine to create these potentially deadly storms. Aside from the obvious danger of typhoon landfall, manufacturers in Pacific regions such as coastal China, Hong Kong, Japan, Taiwan, Vietnam, South Korea, and The Philippines—and, to a lesser extent, Southeast Asian nations such as Malaysia, Thailand and Singapore—have reported poor balance stability and difficult weighing operation during periods of typhoon activity.
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Geostatistical Based Models for the Spatial Adjustment of Radar Rainfall Data in Typhoon Events at a High-Elevation River Watershed
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4138 JOURNAL OF CLIMATE VOLUME 26 Large Increasing Trend of Tropical Cyclone Rainfall in Taiwan and the Roles of Terrain CHIH-PEI CHANG Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan, and Department of Meteorology, Naval Postgraduate School, Monterey, California YI-TING YANG AND HUNG-CHI KUO Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan (Manuscript received 23 July 2012, in final form 7 November 2012) ABSTRACT Taiwan, which is in the middle of one of the most active of the western North Pacific Ocean’s tropical cyclone (TC) zones, experienced a dramatic increase in typhoon-related rainfall in the beginning of the twenty-first century. This record-breaking increase has led to suggestions that it is the manifestation of the effects of global warming. With rainfall significantly influenced by its steep terrain, Taiwan offers a natural laboratory to study the role that terrain effects may play in the climate change of TC rainfall. Here, it is shown that most of the recently observed large increases in typhoon-related rainfall are the result of slow-moving TCs and the location of their tracks relative to the meso-a-scale terrain. In addition, stronger interaction between the typhoon circulation and southwest monsoon wind surges after the typhoon center moves into the Taiwan Strait may cause a long-term trend of increasing typhoon rainfall intensity, which is not observed before the typhoon center exits Taiwan. The variation in the location of the track cannot be related to the effects of global warming on western North Pacific TC tracks reported in the literature.
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