A Statistical Analysis of Tropical Cyclone-Induced Low-Level Winds near Taiwan Island

被引:1
|
作者
Xue, Lin [1 ]
Li, Ying [2 ]
Yao, Sen [1 ]
机构
[1] Yunnan Univ Finance & Econ, Sch Finance, Kunming 650221, Peoples R China
[2] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing 100081, Peoples R China
基金
中国国家自然科学基金;
关键词
tropical cyclone; low-level wind field; Taiwan Island; wind structure; WESTERN NORTH PACIFIC; ROLL VORTICES; VERTICAL SHEAR; SURFACE WINDS; PART I; INTENSITY; SENSITIVITY; TRACK; CLIMATOLOGY; VARIABILITY;
D O I
10.3390/atmos14040715
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Using ERA5 reanalysis data and the tropical cyclone (TC) best track datasets from the China Meteorological Administration and Joint Typhoon Warning Center (from 1979 to 2021), TC-induced low-level winds near Taiwan Island are statistically analyzed. This study mainly concerns TC activity, low-level wind fields around Taiwan Island under TCs, and the detailed characteristics of TC wind structure. Results show that on average, 8.3 TCs enter the study region near Taiwan Island every year mainly from May to November, with more frequent and stronger TCs on the eastern and southern sides of Taiwan Island. For TC centers located at different positions around Taiwan Island, positive and negative vertical vorticity belts alternate between Taiwan Island and the TC center. Moreover, stronger and more frequent TC-induced winds mainly occur on the eastern side of Taiwan Island and the north of Taiwan Strait. TCs to the east of Taiwan Island have stronger maximum sustained wind than those on the western side of the island. Radii of the maximum wind (RMW) for TCs around Taiwan Island range from 5 to 90 nautical mile (nm, 9.3 to 116.7 km) with a mean value of 24.7 nm (44.4 km). Moreover, the RMWs of TCs are the largest (smallest) when the TC centers are located to the southwest (east) of the island. In addition, the outer sizes of TC winds vary from 52 to 360 nm (17.2 to 666.7 km) in the study region, with 187.4 nm (347.1 km) on average, and smaller values for TCs on the western side of the island. The average radii of severe winds, including R-34, R-50, and R-64, are largest in the northeast quadrant and smallest in the southwest quadrant of the TC. The higher the specific wind speed is, the smaller the TC radius and the more symmetric its wind circle. These statistical results may provide references for TC gale forecasting and wind-resistant design for offshore engineering to mitigate TC-induced wind hazards.
引用
收藏
页数:17
相关论文
共 50 条
  • [11] Stronger Tropical Cyclone-Induced Ocean Cooling in Near-Coastal Regions Compared to the Open Ocean
    Da, Nguyen Dac
    Foltz, Gregory R.
    Balaguru, Karthik
    Fernald, Eleda
    JOURNAL OF CLIMATE, 2023, 36 (18) : 6447 - 6463
  • [12] Midsummer gap winds and low-level circulation over the eastern tropical Pacific
    Romero-Centeno, Rosario
    Zavala-Hidalgo, Jorge
    Raga, G. B.
    JOURNAL OF CLIMATE, 2007, 20 (15) : 3768 - 3784
  • [13] Statistical downscaling of North Atlantic tropical cyclone frequency and the amplified role of the Caribbean low-level jet in a warmer climate
    Jones, Jhordanne J.
    Stephenson, Tannecia S.
    Taylor, Michael A.
    Campbell, Jayaka D.
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2016, 121 (08) : 3741 - 3758
  • [14] Using surface adjusted goes low-level cloud-drift winds to imrove the estimation of tropical cyclone outer wind radii
    Dunion, JP
    Houston, S
    Velden, C
    Powell, M
    Black, P
    24TH CONFERENCE ON HURRICANES AND TROPICAL METEOROLOGY/10TH CONFERENCE ON INTERACTION OF THE SEA AND ATMOSPHERE, 2000, : 488 - 489
  • [15] Influence of Low-Level, High-Entropy Air in the Eye on Tropical Cyclone Intensity: A Trajectory Analysis
    Zhou, Xingyang
    Wu, Liguang
    Liu, Qingyuan
    Zheng, Yan
    JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 2020, 98 (06) : 1231 - 1243
  • [16] Reanalysis representation of low-level winds in the Antarctic near-coastal region
    Caton Harrison, Thomas
    Biri, Stavroula
    Bracegirdle, Thomas J.
    King, John C.
    Kent, Elizabeth C.
    Vignon, Etienne
    Turner, John
    WEATHER AND CLIMATE DYNAMICS, 2022, 3 (04): : 1415 - 1437
  • [17] Mountain Waves, Downslope Winds, and Low-Level Blocking Forced by a Midlatitude Cyclone Encountering an Isolated Ridge
    Menchaca, Maximo Q.
    Durran, Dale R.
    JOURNAL OF THE ATMOSPHERIC SCIENCES, 2017, 74 (02) : 617 - 639
  • [18] Composite Analysis-Based Machine Learning for Prediction of Tropical Cyclone-Induced Sea Surface Height Anomaly
    Cui, Hongxing
    Tang, Danling
    Liu, Huizeng
    Sui, Yi
    Gu, Xiaowei
    IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING, 2023, 16 : 2644 - 2653
  • [19] Low-Level Westerly Winds, Topography, and Tropical Cyclogenesis of Arlene (2005): Observations and Model Simulations
    Yoo, Jinwoong
    Rohli, Robert V.
    Collins, Jennifer M.
    PROFESSIONAL GEOGRAPHER, 2017, 69 (03): : 348 - 361
  • [20] Quadrant-Dependent Evolution of Low-Level Tangential Wind of a Tropical Cyclone in the Shear Flow
    Gu, Jian-Feng
    Tan, Zhe-Min
    Qiu, Xin
    JOURNAL OF THE ATMOSPHERIC SCIENCES, 2016, 73 (03) : 1159 - 1177