A Potential Risk Index Dataset for Landfalling Tropical Cyclones Over the Chinese Mainland (PRITC Dataset V1.0)

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A Potential Risk Index Dataset for Landfalling Tropical Cyclones Over the Chinese Mainland (PRITC Dataset V1.0) ADVANCES IN ATMOSPHERIC SCIENCES, VOL. 38, OCTOBER 2021, 1791–1802 • Data Description Article • A Potential Risk Index Dataset for Landfalling Tropical Cyclones over the Chinese Mainland (PRITC dataset V1.0) Peiyan CHEN1,2,3, Hui YU*1,2, Kevin K. W. CHEUNG4, Jiajie XIN1, and Yi LU1,2,3 1Shanghai Typhoon Institute, China Meteorological Administration, Shanghai 200030, China 2Key Laboratory of Numerical Modeling for Tropical Cyclone of China Meteorological Administration, Shanghai 20030, China 3The Joint Laboratory for Typhoon Forecasting Technique Applications between Shanghai Typhoon Institute and Wenzhou Meteorological Bureau, Wenzhou 325027, China 4Climate and Atmospheric Science, NSW Department of Planning Industry and Environment, Sydney 2000, Australia (Received 26 November 2020; revised 28 April 2021; accepted 6 May 2021) ABSTRACT A dataset entitled “A potential risk index dataset for landfalling tropical cyclones over the Chinese mainland” (PRITC dataset V1.0) is described in this paper, as are some basic statistical analyses. Estimating the severity of the impacts of tropical cyclones (TCs) that make landfall on the Chinese mainland based on observations from 1401 meteorological stations was proposed in a previous study, including an index combining TC-induced precipitation and wind (IPWT) and further information, such as the corresponding category level (CAT_IPWT), an index of TC-induced wind (IWT), and an index of TC-induced precipitation (IPT). The current version of the dataset includes TCs that made landfall from 1949–2018; the dataset will be extended each year. Long-term trend analyses demonstrate that the severity of the TC impacts on the Chinese mainland have increased, as embodied by the annual mean IPWT values, and increases in TC- induced precipitation are the main contributor to this increase. TC Winnie (1997) and TC Bilis (2006) were the two TCs with the highest IPWT and IPT values, respectively. The PRITC V1.0 dataset was developed based on the China Meteorological Administration’s tropical cyclone database and can serve as a bridge between TC hazards and their social and economic impacts. Key words: tropical cyclone, risk, dataset, China Citation: Chen, P. Y., H. Yu, K. Cheung, J. J. Xin, and Y. Lu, 2021: A potential risk index dataset for landfalling tropical cyclones over the Chinese mainland (PRITC dataset V1.0). Adv. Atmos. Sci., 38(10), 1791−1802, https://doi.org/10.1007/ s00376-021-0365-y. Dataset Profile Dataset title A potential risk index dataset for landfalling tropical cyclones over the Chinese mainland, Version 1.0 (PRITC dataset V1.0) Time range 1949–2018 Geographical scope The Chinese mainland Data format Text Data volume 68 KB Data service system http://tcdata.typhoon.org.cn/en/qzfxzs_sm.html Sources of funding National Key Research and Development Program of China (2017YFC1501604), National Natural Science Foundations of China (41875114), Shanghai Science & Technology Research Program (19dz1200101), National Basic Research Program of China (2015CB452806), and Basic Research Projects of the Shang- hai Typhoon Institute of the China Meteorological Administration (2020JB06). * Corresponding author: Hui YU Email: [email protected] © The Authors [2021]. This article is published with open access at link.springer.com 1792 PRITC DATASET V1.0 VOLUME 38 (Continued) Dataset composition The dataset has one file, which is called “PRITC_V1.0.txt”. It contains two parts: a headline and the data lines. Each data line has 10 columns, including the serial number, year, TC identifier, TC name, province and intensity grade at the first landfall of the TC, index of TC-induced wind (IWT), index of TC-induced pre- cipitation (IPT), combined index of TC-induced precipitation and wind (IPWT), and corresponding cat- egory level (CAT_IPWT). 1. Introduction risk caused by TC winds. The absence of precipitation in these indicators is one source of the differences that exist Tropical cyclones (TCs) are the most disastrous natural between the estimated and actual risks resulting from landfall- phenomena in the world, and China is among the most ing TCs, especially over complex terrain. To address this severely affected countries (Yu and Chen, 2019). In recent issue, Rezapour and Baldock, (2014) added a rainfall index years, extremely disastrous TCs have occurred frequently in to the hazard index to estimate and rank the severity levels China, possibly due to the warming climate. For example, of hurricanes making landfall in the continental United Super Typhoon Mangkhut (2018) made landfall in Guang- States based on precipitation data extracted from remotely dong Province in China, causing a total direct economic sensed imagery using an artificial neural network database. loss (DEL) of 14.23 billion Chinese Yuan in six provinces Zhang et al., (2010) added a total vapor index to the total dam- including Guangdong, Guangxi, Hainan, Hunan, Yunnan, age index for TCs making landfall in China. Both studies and Guizhou provinces. Super Typhoon Lekima (2019) and showed that the hazard indices, when rainfall factors were severe tropical storm Rumbia (2018) made landfall in East included, were highly correlated with DELs. China, causing severe flooding that spanned the eastern, north- Recently, Chen et al., (2009; 2013; 2019) developed ern, and northeastern regions of China (Zhou et al., 2021). three potential risk indices for TCs making landfall on the Recent research has also indicated that TCs in the Western Chinese mainland based on 30 years (1984–2013) of sur- North Pacific have shifted towards becoming fewer, slower, face observations obtained from the China Meteorological and stronger; a decreasing trend has been observed in trop- Administration (CMA). Among these three indices, one ical storm/typhoon (and above) counts, while statistically sig- index was based on wind, one was based on precipitation, nificant increasing trends have been observed in the intens- and one was based on both precipitation and wind. All three ity of TCs, the intensification rate from the tropical storm to indices were significantly correlated with damage, and the typhoon stage, and the proportion of TCs that undergo rapid index that was based on both precipitation and wind ranked intensification at least once during their lifetime (Knutson et best among the three. A potential risk index dataset for TCs al., 2010; Kishtawal et al., 2012; Ying et al., 2012; Holland that made landfall over the Chinese mainland from and Bruyere, 2014; Emanuel, 2017; Kossin, 2018; Zhao et 1949–2018, abbreviated as the PRITC dataset V1.0, was al., 2018a, b; Hall and Kossin, 2019; Kossin et al., 2020; Lee et al., 2020). There has also been a statistically signific- developed following the publishing of Chen et al., (2019) ant northwestward shift in the maximum intensity of TC and was released to the public through the internet in tracks over the Western North Pacific resulting in an August 2020. The dataset will be updated annually in the increase in TC intensity and a tendency for TCs to be more future. destructive when making landfall over East China (Park et For ease of use, detailed information about the dataset al., 2013, 2014; Mei and Xie, 2016; Li et al., 2017; Lee et is introduced in this paper. Section 2 describes the data al., 2020). These changes will cause China, especially East sources and the equations of the indices. Section 3 presents China and North China, to face higher TC hazards risks the dataset composition and the organizational structure of than ever. the data. Section 4 presents some general characteristics of The risks resulting from TCs are related to TC hazards the indices. The last section includes the conclusion and dis- and to the vulnerability and resilience of the hazard-bearing cussion. bodies. TC hazards are the drivers of risk or damage and gen- erally include severe winds, heavy precipitation, and storm 2. Data sources, expressions, and dataset surge. Reasonable and reliable indications of potential risk composition from the perspective of TC hazards are a key point in TC risk assessments. Several different expressions based on the 2.1. Best-track data intensity of TCs or on their extreme wind speeds exist and are most popularly used as indicators of the potential risk res- The 6-h track and intensity data of TCs that made land- ulting from TC hazards. Examples include the power dissipa- fall over the Chinese mainland were obtained from the tion index (Emanuel, 2005) and the hurricane intensity CMA TC best track dataset (Ying et al., 2014) and were index (Kantha 2006, 2013; Powell and Reinhold, 2007; downloaded from http://tcdata.typhoon.org.cn/en/zjljsjj_ Xiao et al., 2011; Peduzzi et al., 2012; Hong et al., 2016; sm.html. There were 583 TCs that made landfall on main- Choun and Kim, 2019; Fang et al., 2020; Liu et al., 2020b). land China from 1949 to 2018, with an annual mean of 8.3 Fundamentally, these indicators express the damage-based TCs. OCTOBER 2021 CHEN ET AL. 1793 2.2. Observed precipitation and wind data (Fig. 1) were selected following the methods of Lu et al. The TC-induced precipitation and wind data recorded (2017) and the Climatological Atlas of Tropical Cyclones at meteorological stations throughout the Chinese mainland over the Western North Pacific (1981–2010) published by were obtained from the CMA TC database (Ying et al., the Shanghai Typhoon Institute of CMA in 2017 2014). The temporal duration ranged from 1949 to 2018, cov- (STI/CMA, 2017). Among these stations, there were 449 ering a total of 70 years. The TC-induced precipitation data basic national weather stations, 102 reference national clima- consist of the daily precipitation, maximum 1-h precipita- tological stations, and 814 general national weather stations. tion, and the associated dates and times when stations recor- The years in which the stations were constructed ranged from 1914 to 1977 (Fig. 2); 4.8% of the stations were built ded total precipitation values ≥ 10 mm.
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