| 基于非對稱臺風(fēng)風(fēng)場的風(fēng)暴潮模擬研究 |
| 作者:邱超1 劉暢2 王淑英1 陳永平3 |
單位:1. 浙江省水文管理中心, 浙江 杭州 310027; 2. 浙江省水利河口研究院(浙江省海洋規(guī)劃設(shè)計研究院), 浙江 杭州 310020; 3. 河海大學(xué)港口海岸與近海工程學(xué)院, 江蘇 南京 210098 |
| 關(guān)鍵詞:最大風(fēng)速半徑 非對稱風(fēng)場 風(fēng)暴潮 數(shù)值模擬 |
| 分類號:P731.23 |
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| 出版年·卷·期(頁碼):2025·42·第四期(1-10) |
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摘要:
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| 在對2001—2021年西北太平洋熱帶氣旋最大風(fēng)速半徑特征分析的基礎(chǔ)上,基于最優(yōu)風(fēng)速半徑Lin&Fang公式,提出了與方位角相關(guān)的四象限非對稱最大風(fēng)速半徑計算公式。選取影響浙江沿海的4場歷史臺風(fēng)(臺風(fēng)“菲特”、“馬勒卡”、“摩羯”、“利奇馬”)進(jìn)行研究,通過與原始公式計算結(jié)果進(jìn)行對比發(fā)現(xiàn),四象限非對稱最大風(fēng)速半徑計算公式可以更加準(zhǔn)確地模擬臺風(fēng)風(fēng)速的變化過程,基于該公式得到的風(fēng)暴潮模擬結(jié)果更準(zhǔn)確地反映了臺風(fēng)期間浙江沿海地區(qū)的最大風(fēng)暴增水過程。 |
| Based on the analysis of maximum wind speed radius of tropical cyclones in the Northwest Pacific from 2001 to 2021, a four-quadrant asymmetric maximum wind speed radius calculation formula relying on azimuth angle is proposed based on the optimal wind speed radius formula of Lin&Fang. Four historical typhoons( "Fitow", "Malakas", "Yagi", "Lekima") affecting the Zhejiang coast are selected to validate the proposed formula in comparison with the original Lin&Fang formula. The results show that the proposed formula simulates the typhoon wind speed change more accurately. The storm surge calculation using the proposed formula products more accurate maximum storm surge along the Zhejiang coast. |
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參考文獻(xiàn):
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[1] WALSH K J E, CAMARGO S J, KNUTSON T R, et al. Tropical cyclones and climate change[J]. Tropical Cyclone Research and Review, 2019, 8(4):240-250. [2] CUI W, CARACOGLIA L. Exploring hurricane wind speed along US Atlantic coast in warming climate and effects on predictions of structural damage and intervention costs[J]. Engineering Structures, 2016, 122:209-225. [3] PAN Y, CHEN Y P, LI J X, et al. Improvement of wind field hindcasts for tropical cyclones[J]. Water Science and Engineering,2016, 9(1):58-66. [4] YAN D C, ZHANG T Y. Research progress on tropical cyclone parametric wind field models and their application[J]. Regional Studies in Marine Science, 2022, 51:102207. [5] JELESNIANSKI C P. Numerical computations of storm surges without bottom stress[J]. Monthly Weather Review, 1966, 94(6):379-394. [6] HOLLAND G J. An analytic model of the wind and pressure profiles in hurricanes[J]. Monthly Weather Review, 1980, 108(8):1212-1218. [7] HU B H, YANG X Q, TAN Y K, et al. A new method for calculating the wind speed distribution of a moving tropical cyclone[J]. Advances in Atmospheric Sciences, 2010, 27(1):69-79. [8] 吳彥,趙紅軍,葉榮輝,等.非對稱風(fēng)場對臺風(fēng)浪模擬效果的比較研究[J]. 海洋預(yù)報, 2020, 37(1):55-61.WU Y, ZHAO H J, YE R H, et al. A comparative study of the effects of asymmetric wind field on typhoon wave simulation[J]. Marine Forecasts, 2020, 37(1):55-61. [9] 傅賜福,于福江,劉秋興,等.四象限非對稱風(fēng)場對風(fēng)暴潮的改進(jìn)研究[J]. 海洋通報, 2013, 32(6):626-632.FU C F, YU F J, LIU Q X, et al. An improved study on the storm surge with four-quadrant asymmetric wind model[J]. Marine Science Bulletin, 2013, 32(6):626-632. [10] 陳孔沫.一種計算臺風(fēng)風(fēng)場的方法[J]. 熱帶海洋, 1994, 13(2):41-48.CHEN K M. A computation method for typhoon wind field[J]. Tropic Oceanology, 1994, 13(2):41-48. [11] ZHONG X, WEI K, SHANG D M. An improved azimuthdependent Holland model for typhoons along the Zhejiang coast prior to landfall based on WRF–ARW simulations[J]. Natural Hazards, 2023, 117(3):2325-2346. [12] 房偉,陳國平,趙紅軍,等.最大風(fēng)速半徑對臺風(fēng)浪計算效果的比較研究[J]. 水道港口, 2017, 38(6):574-580.FANG W, CHEN G P, ZHAO H J, et al. The influence of radius of maximum wind on typhoon waves[J]. Journal of Waterway and Harbor, 2017, 38(6):574-580. [13] WU Y, DOU S T, FAN Y S, et al. Research on the influential characteristics of asymmetric wind fields on typhoon waves[J]. Frontiers in Marine Science, 2023, 10:1113494. [14] ZHAO S K, LIU Z W, WEI X R, et al. Intercomparison of empirical formulations of maximum wind radius in parametric tropical storm modeling over Zhoushan Archipelago[J]. Sustainability, 2021, 13(21):11673. [15] 羅佳敏,姜云鵬,龐亮,等.基于參數(shù)化風(fēng)場的浙江沿海風(fēng)暴潮數(shù)值模擬[J]. 海洋學(xué)報, 2022, 44(10):20-34.LUO J M, JIANG Y P, PANG L, et al. Numerical simulation of storm surge in the coast of Zhejiang based on para-metric wind field model[J]. Haiyang Xuebao, 2022, 44(10):20-34. [16] 劉士誠,陳永平,譚亞,等.珠江河網(wǎng)1822號臺風(fēng)“山竹”期間風(fēng)暴增水模擬及特性分析[J]. 海洋預(yù)報, 2021, 38(2):12-20.LIU S C, CHEN Y P, TAN Y, et al. Storm surge simulation and characteristic analysis during typhoon“Mangkhut” 2018 in the Pearl River Estuary[J]. Marine Forecasts, 2021, 38(2):12-20. [17] 羅鋒,汪憶,楊潔,等.相似路徑臺風(fēng)風(fēng)暴潮過程對比[J]. 河海大學(xué)學(xué)報(自然科學(xué)版), 2023, 51(6):130-140.LUO F, WANG Y, YANG J, et al. Comparative study on storm surge processes caused by typhoons with similar tracks[J]. Journal of Hohai University(Natural Sciences), 2023, 51(6):130-140. [18] 張露,傅賜福,董劍希,等.臺風(fēng)“妮妲”風(fēng)暴潮與近岸浪的數(shù)值模擬與預(yù)報[J]. 海洋預(yù)報, 2018, 35(2):27-35.ZHANG L, FU C F, DONG J X, et al. Numerical simulation and forecasting on storm surge and offshore wave of typhoon“Nida”[J]. Marine Forecasts, 2018, 35(2):27-35. |
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