Dynamical Downscaling of Typhoon Lionrock (2016) for Assessing the Resulting Hazards Under Global Warming

Total Page:16

File Type:pdf, Size:1020Kb

Dynamical Downscaling of Typhoon Lionrock (2016) for Assessing the Resulting Hazards Under Global Warming Nayak, S., and T. Takemi, 2019: Dynamical downscaling of Typhoon Lionrock (2016) for assessing the resulting hazards under global warming. J. Meteor. Soc. Japan, 97, 69-88. Special Edition on Tropical Cyclones in 2015–2016 https://doi.org/10.2151/jmsj.2019-003 Plain Language Summary: Recent studies have revealed that typhoons will be stronger and more powerful in a future warmer climate and be a threat to lives and properties. The present study attempted to perform dynamical downscaling simulations of Typhoon Lionrock (2016) at 1-km grid resolution by using the Weather Research and Forecasting (WRF) model to discuss the track and intensity of this typhoon and associated precipitation amount in the target region after landfall in present climate and under Pseudo Global Warming (PGW) conditions. (a) Precipitation distribution during landfall (b) Wind at 850-hPa during landfall (mm/h) (knots) (c) 24-hours accumulated precipitation (d) 2-days mean wind at 850-hPa (knots) (mm) Figure 1. (a) Precipitation distribution and (b) Wind (850-hPa) during landfall of Typhoon Lionorck in present climate and under PGW conditions. (c ) 24-hours (±12 hours of landfall) accumulated precipitation and (d) Two days (29-30 Aug) mean wind at 850-hPa in present and under PGW. The downscaled simulations with WRF model reproduced a significant improvement in the track and intensity of the typhoon with respect to the original reanalysis datasets. The typhoon is projected to be stronger and more powerful under future warm climate. It is expected to produce more precipitation over Hokkaido and the entire Tohoku region in warming climate. The study suggests that the typhoons under PGW condition may increase the risk of flooding, damages to infrastructures, and lives staying along the typhoon track. .
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • CFK Team Completes Fourth Visit for 2016 Observation of Emergency
    December 2016 “Rejoice always, pray without ceasing; in everything give thanks: for this is the will of God in Christ Jesus for you.” 1 Thessalonians 5:16–18 CFK Team Completes Fourth Visit for 2016 team of 17 people from the United States, Norway, A Australia, and New Zealand completed a 27-day visit to the DPRK with CFK on November 22nd. The purpose of this visit was wide-ranging, including flood relief confirming visits to the far northernmost cities of Musan and Yonsa; confirming visits to 18 CFK supported hospitals and rest homes; the completion of renovations at the Kaesong #2 Hepatitis Hospital Lab; the extension of a water distribution system at Kaesong #3 TB Hospital; presentation of advanced TB diagnostics training workshops at the National TB Reference Lab; running over 10,000 diagnostic lab tests at the newly renovated Pyongyang #2 Hepatitis Hospital Laboratory on blood samples from nearly 500 hepatitis patients; and starting Øyvind Dovland overlooking temporary shelters in the flood ravaged town of Musan 385 more patients on hepatitis B antiviral treatment. Musan. Beginning near the top of the high pass and winding Observation of Emergency Flood Activities down to Musan, there was clear evidence along the way of rom October 28–November 1, a small team including the devastation caused by the torrential rains that poured into Frepresentatives from CFK, the Mennonite Central these narrow mountain valleys. The road we traveled down Committee, and Evangelisk Orientmisjon, traveled the narrow hugs the mountains and largely parallels a small stream that mountain roads from Chongjin to the northeastern cities of had swelled enormously from the downpour in late August Musan and Yonsa; both cities were among the hardest hit areas into a raging torrent, sweeping away homes, trees, the road, during the late August flooding from Typhoon Lionrock.
    [Show full text]
  • Downloaded 10/01/21 02:24 PM UTC 4916 JOURNAL of the ATMOSPHERIC SCIENCES VOLUME 72
    DECEMBER 2015 T A N G E T A L . 4915 Horizontal Transition of Turbulent Cascade in the Near-Surface Layer of Tropical Cyclones JIE TANG Shanghai Typhoon Institute, China Meteorological Administration, Shanghai, and Key Laboratory of Mesoscale Severe Weather, Ministry of Education, and School of Atmospheric Sciences, Nanjing University, Nanjing, China DAVID BYRNE Environmental Physics Group, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich,€ Zurich, Switzerland JUN A. ZHANG National Oceanic and Atmospheric Administration/Atlantic Oceanographic and Meteorological Laboratory/Hurricane Research Division, Miami, Florida YUAN WANG Key Laboratory of Mesoscale Severe Weather, Ministry of Education, and School of Atmospheric Sciences, Nanjing University, Nanjing, China XIAO-TU LEI,DAN WU,PING-ZHI FANG, AND BING-KE ZHAO Shanghai Typhoon Institute, China Meteorological Administration, Shanghai, China (Manuscript received 15 December 2014, in final form 7 July 2015) ABSTRACT Tropical cyclones (TC) consist of a large range of interacting scales from hundreds of kilometers to a few meters. The energy transportation among these different scales—that is, from smaller to larger scales (up- scale) or vice versa (downscale)—may have profound impacts on TC energy dynamics as a result of the associated changes in available energy sources and sinks. From multilayer tower measurements in the low- level (,120 m) boundary layer of several landing TCs, the authors found there are two distinct regions where the energy flux changes from upscale to downscale as a function of distance to the storm center. The boundary between these two regions is approximately 1.5 times the radius of maximum wind. Two-dimensional tur- bulence (upscale cascade) occurs more typically at regions close to the inner-core region of TCs, while 3D turbulence (downscale cascade) mostly occurs at the outer-core region in the surface layer.
    [Show full text]
  • Tropical Cyclone Temperature Profiles and Cloud Macro-/Micro-Physical Properties Based on AIRS Data
    atmosphere Article Tropical Cyclone Temperature Profiles and Cloud Macro-/Micro-Physical Properties Based on AIRS Data 1,2, 1, 3 3, 1, 1 Qiong Liu y, Hailin Wang y, Xiaoqin Lu , Bingke Zhao *, Yonghang Chen *, Wenze Jiang and Haijiang Zhou 1 1 College of Environmental Science and Engineering, Donghua University, Shanghai 201620, China; [email protected] (Q.L.); [email protected] (H.W.); [email protected] (W.J.); [email protected] (H.Z.) 2 State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China 3 Shanghai Typhoon Institute, China Meteorological Administration, Shanghai 200030, China; [email protected] * Correspondence: [email protected] (B.Z.); [email protected] (Y.C.) The authors have the same contribution. y Received: 9 October 2020; Accepted: 29 October 2020; Published: 2 November 2020 Abstract: We used the observations from Atmospheric Infrared Sounder (AIRS) onboard Aqua over the northwest Pacific Ocean from 2006–2015 to study the relationships between (i) tropical cyclone (TC) temperature structure and intensity and (ii) cloud macro-/micro-physical properties and TC intensity. TC intensity had a positive correlation with warm-core strength (correlation coefficient of 0.8556). The warm-core strength increased gradually from 1 K for tropical depression (TD) to >15 K for super typhoon (Super TY). The vertical areas affected by the warm core expanded as TC intensity increased. The positive correlation between TC intensity and warm-core height was slightly weaker. The warm-core heights for TD, tropical storm (TS), and severe tropical storm (STS) were concentrated between 300 and 500 hPa, while those for typhoon (TY), severe typhoon (STY), and Super TY varied from 200 to 350 hPa.
    [Show full text]
  • Annual Report on the Climate System 2016
    Annual Report on the Climate System 2016 March 2017 Japan Meteorological Agency Preface The Japan Meteorological Agency is pleased to publish the Annual Report on the Climate System 2016. The report summarizes 2016 climatic characteristics and climate system conditions worldwide, with coverage of specific events including the effects of the summer 2014 – spring 2016 El Niño event and notable aspects of Japan’s climate in summer 2016. I am confident that the report will contribute to the understanding of recent climatic conditions and enhance awareness of various aspects of the climate system, including the causes of extreme climate events. Teruko Manabe Director, Climate Prediction Division Global Environment and Marine Department Japan Meteorological Agency Contents Preface 1. Explanatory notes ··························································································· 1 1.1 Outline of the Annual Report on the Climate System ······································· 1 1.2 Climate in Japan ···················································································· 1 1.3 Climate around the world ························································ ·············· 2 1.4 Atmospheric circulation ············· ···························································· 3 1.5 Oceanographic conditions ··········· ··············································· ·········· 5 1.6 Snow cover and sea ice ······································································· 5 2. Annual summaries of the 2016 climate system
    [Show full text]
  • Natural Catastrophes and Man-Made Disasters in 2016: a Year of Widespread Damages
    No 2 /2017 Natural catastrophes and 01 Executive summary 02 Catastrophes in 2016: man-made disasters in 2016: global overview a year of widespread damages 06 Regional overview 13 Floods in the US – an underinsured risk 18 Tables for reporting year 2016 40 Terms and selection criteria Executive summary There were a number of expansive In terms of devastation wreaked, there were a number of large-scale disasters across disaster events in 2016 … the world in 2016, including earthquakes in Japan, Ecuador, Tanzania, Italy and New Zealand. There were also a number of severe floods in the US and across Europe and Asia, and a record high number of weather events in the US. The strongest was Hurricane Matthew, which became the first Category 5 storm to form over the North Atlantic since 2007, and which caused the largest loss of life – more than 700 victims, mostly in Haiti – of a single event in the year. Another expansive, and expensive, disaster was the wildfire that spread through Alberta and Saskatchewan in Canada from May to July. … leading to the highest level of overall In total, in sigma criteria terms, there were 327 disaster events in 2016, of which losses since 2012. 191 were natural catastrophes and 136 were man-made. Globally, approximately 11 000 people lost their lives or went missing in disasters. At USD 175 billion, total economic losses1 from disasters in 2016 were the highest since 2012, and a significant increase from USD 94 billion in 2015. As in the previous four years, Asia was hardest hit. The earthquake that hit Japan’s Kyushu Island inflicted the heaviest economic losses, estimated to be between USD 25 billion and USD 30 billion.
    [Show full text]
  • Member Report (2016)
    MEMBER REPORT (2016) ESCAP/WMO Typhoon Committee 11th Integrated Workshop China MERANTI (1614) October 24-28, 2016 Cebu, Philippines Contents I. Review of Tropical Cyclones Which Have Affected/Impacted Members since the Previous Session 1.1 Meteorological and hydrological assessment ....................................................................................... 1 1.2 Socio-economic assessment ................................................................................................................ 13 1.3 Regional cooperation assessment ....................................................................................................... 15 II. SUMMARY OF KEY RESULT AREAS Typhoon forecast, prediction and research 2.1 Typhoon forecasting technique .......................................................................................................... 20 2.2 Typhoon numerical modeling and data assimilation .......................................................................... 21 2.3 Typhoon research ................................................................................................................................ 23 2.4 Journal of tropical cyclone research and review ................................................................................. 25 Typhoon observation, satellite application and data broadcasting 2.5 Ocean observing system and observation experiments ..................................................................... 26 2.6 GF-4 satellite applied in typhoon monitoring ....................................................................................
    [Show full text]
  • Parameters of Lightning Activity in the Tropical Cyclones at the Stage of Maximum Development in August 2016
    E3S Web of Conferences 127, 01006 (2019) https://doi.org/10.1051/e3sconf /2019127010 06 Solar-Terrestrial Relations and Physics of Earthquake Precursors Parameters of lightning activity in the tropical cyclones at the stage of maximum development in August 2016 Svetlana Shabaganova1*, Lena Tarabukina2, and Vladimir Kozlov2 1Polytechnic Institute (branch) M.K. Ammosov North-Eastern Federal University, Mirny, Russia 2Institute of Cosmophysical Research and Aeronomy, Siberian Branch of the Russian Academy of Sciences, Yakutsk, Russia Abstract. This article discusses the parameters of thunderstorm activity in the structure of tropical cyclones that had an impact on the Russian Far East in August 2016. The study shows in detail the change in the cloud mass and describes its structure during the lifetime of the most powerful tropical cyclone Lionrock (2016). It is shown that the density distribution of lightning discharges in the range of tropical cyclones (up to 1000 km), reaching the typhoon stage, is characterized by two local maxima. The distribution density of lightning discharges in the range of tropical cyclones that have reached a strong tropical storm is characterized by one maximum. The lifetime of thunderstorm cells that stand out is 40-50 minutes in average. Before the typhoon stage, the area of thunderstorm cells increased, and then, the number of cells as well as the intensity of discharges in the cell increased, but their lifetime and area decreased. 1 Introduction The economy of any state significantly depends on weather conditions. Extreme sectors, such as floods and hurricanes, have a significant impact on various sectors of the economy. One of the reasons for the occurrence of such dangerous phenomena is tropical cyclones, which are almost always accompanied by powerful thunderstorms.
    [Show full text]
  • Does Deforestation Trigger Severe Flood Damage at Hoeryeong City in North Korea?
    Article Does Deforestation Trigger Severe Flood Damage at Hoeryeong City in North Korea? Joongbin Lim 1 , Kyoung-Min Kim 1 and Kyoo-Seock Lee 2,* 1 Inter-Korean Forest Research Team, Division of Global Forestry, Department of Forest Policy and Economics, National Institute of Forest Science, 57 Hoegi-ro, Dongdaemun-gu, Seoul 02455, Korea 2 Department of Landscape Architecture, Graduate School, Sungkyunkwan University, Suwon 16419, Korea * Correspondence: [email protected]; Tel.: +82-31-290-7845 Received: 4 August 2019; Accepted: 9 September 2019; Published: 11 September 2019 Abstract: North Korea has suffered flood damage every year since 1995. It is assumed that this damage is linked to deforestation. Therefore, the purpose of this study was to investigate the effects of deforestation on the occurrence of floods in North Korea using spatial statistical techniques. The research was conducted at Hoeryeong City, which experienced disastrous flooding in 2016. A land-use change map was produced using two Landsat data sets from 1977 and 2016. The flood- damaged areas map, landform map, and the distance from the nearest stream map were also used in the spatial statistical analysis. In the deforestation zone, area of soil loss over 200 tons/yr increased by 14 km2 (16.6%), while that under 50 tons/yr decreased by 25 km2 (29.3%). In addition, the land-use change, runoff coefficient, and peak time runoff increased from 0.31 to 0.46, 56.3 mm/hr to 60.8 mm/hr, and 128.2 m3/sec to 206.6 m3/sec, respectively. Also, spatial statistical analysis results showed that land-use change was concluded to strongly affect the occurrence of floods.
    [Show full text]
  • 60 10,000 Ha 23 112 Km
    DEMOCRATIC PEOPLE’S REPUBLIC OF KOREA: Flooding - Humanitarian Snapshot (as of 05 September 2016) Overview Typhoon Lionrock, as well as a low pressure system, has triggered heavy rains over northwestern DPRK, causing the Tumen River to overflow and buildings to collapse. Early findings from the Government indicate that North Hamgyong Province has been most severely CHINA Onsong affected by extensive flooding, in particular Musan, Onsong, Kyongwon, Kyonghung, Yonsan Kyongwon RUSSIAN counties as well as Hoeryong City. FEDERATION Tumen Flooding is known to have killed 60 people and displaced over 44,000 people - 5 per cent of the Kyonghung 1 Hoeryong population of affected areas , as well as destroying more than 4,400 houses. Communication City with and access to affected areas remains a challenge, however, immediate needs have been Rason City identified as emergency shelter, food, medication, water and sanitary items. 1. Total population for affected areas is taken from the 2011 Census. Musan Puryong Chongjin City North Hamgyong Number of buldings destroyed / damaged Number of people displaced Yonsan Number of affected Households Yonsan 950 2,700 Yonsan 17,000 Kyongsong More than 5,000 Musan 1,800 600 Musan 13,000 Ryanggang Hoeryong City 1,200 520 Hoeryong City 8,000 1,000 - 5,000 Orang Kyongwon 4 / 370 Onsong 2,400 Less than 1,000 Onsong 260 / 0 4,400 Kyongwon 780 Hwasong Other affected counties buildings destroyed Undok 80 / 40 Undok 750 Kilju 4,300 44,000 Hwasong Other counties 110 / 90 Other counties 1,100 buildings damaged people displaced Hwadae Kim Chaek City Response South Hamgyong The Government of DPRK, through the State Committee for Emergency and Disaster Management (SCEDM) is coordinating the humanitarian response to the Typhoon and floods, Pyongyang activating its early warning and evacuation system.
    [Show full text]
  • Flood Relief for North Korea -- Sending Winter Sweaters to Children!
    Flood Relief for North Korea -- Sending winter sweaters to children! Angelika Selle September 29, 2016 Local children outside Hoeryong City, UNICEF DPRK, 2016 FLOOD RELIEF FOR NORTH KOREA Help us to send winter clothes to North Korean children! After hearing of Typhoon Lionrock in North Korea, subsequent flooding, and the displacement of between 70,000 to 100,000 people, WFWP USA contacted WFWP in South Korea to see of their plans to support those affected. Their response: WFWP Korea is a member of the Korean Council for Reconciliation and Cooperation (KCRC), and will be working with them during this crisis. During the recent KCRC emergency meeting it was decided to collect monetary donations to buy winter clothes for children in North Korea at this time. Our WFWP representative adds that it is already quite cold in Korea, and many children and families are suffering and in great need. In order to support this initiative, WFWP USA will be collecting contributions through our 1% Love Share Program Fund, to be sent to our WFWP counterparts in Korea. This ongoing fund currently supports women, children, and disaster hit areas around the world. If you would like to support the livelihood of children in North Korea as the winter season approaches, please donate here now. DONATE NOW! Background More than 70,000 people displaced by severe flooding in North Korea nearly a month ago are urgently in need of supplies and shelter before winter sets in. Typhoon Lionrock created floods that submerged, severely damaged or destroyed 30,000 homes and displaced 70,000 people.
    [Show full text]