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浙江沿海大风气候特征及影响系统分析
作者:曹宗元1  王坚侃1  何晴1  张骁1  傅娜1  陈冬冬2 
单位:1. 舟山市气象局, 浙江 舟山 316021;
2. 中国人民解放军 92012部队, 浙江 舟山 316000
关键词:浙江沿海大风 大风日数 风向 气候特征 影响系统 
分类号:P425.4+3
出版年·卷·期(页码):2023·40·第二期(89-97)
摘要:
选取浙北、浙中、浙南3个沿海代表站,对浙江沿海大风日数、大风频率、风向、影响系统的年际和月变化进行统计分析。结果表明:浙南沿海大风日数最多,平均每年有1/3的天数为大风日,浙北沿海次之,浙中沿海最少,大风日数呈现逐年下降的趋势,且近10 a的下降趋势减缓。浙江沿海大风日数具有一定的地域性特征。浙北沿海8级及以上、9级及以上、10级及以上的大风最多分别出现在4月、3—4月、4月和8月,最少均出现在6月;浙中沿海8级及以上大风日数冬多夏少,9级及以上大风日数呈现秋季—翌年初春多、春末—夏季少的特点,10级及以上大风集中爆发于9月台风季;浙南沿海8级及以上大风在12月最多,9级及以上和10级及以上大风最多出现在10月,最少在5月。浙江沿海季风特征显著,秋冬两季以偏北大风为主,且大风主导风向自北向南顺转(NNW、N、NE),浙中南沿海夏季风弱于冬季风。造成浙江沿海大风的主要天气系统有冷空气、台风、低压、高压后部和强对流等,冷空气偏北大风在11月—翌年3月最为常见,其次为夏季(7—10月)的台风大风,再次为春末夏初的低压大风。
This paper selects three representative stations along the coasts of the northern, the central, and the southern Zhejiang to statistically analyze the interannual and monthly changes of strong windy days, strong windy frequency, wind direction, and impact systems in the Zhejiang coastal area. The results are as follows: The number of strong windy days is the largest along the southern coast of Zhejiang, with 1/3 of the year are strong windy days on average, followed by the coastal area of northern Zhejiang, and the number of strong windy days is the least in the coastal area of central Zhejiang, meanwhile, the number of gale days shows a downward trend, which has slowed down in recent 10 years. The number of gale days along the coast of Zhejiang shows certain regional characteristics. The numbers of strong windy days of level 8, 9, 10 and above in the coastal area of northern Zhejiang peak in April, March-April, April and August, respectively, while the minimum numbers of which all occur in June. The number of strong windy days of level 8 and above along the coast of central Zhejiang is greater in winter and less in summer, while the number of strong windy days of level 9 and above is higher from autumn to early spring of the next year and lower from late spring to summer, and the number of strong windy days of level 10 and above is concentrated during the typhoon season in September. The number of strong wind days of level 8 and above along the coast of southern Zhejiang peaks in December, while the number of strong wind days of level 9, 10 and above are both reach to the highest in October, and to the lowest in May. The monsoon characteristics are significant in the coast of Zhejiang. In autumn and winter, the coast of Zhejiang is dominated by northerly winds, and the dominant wind directions turn clockwise from the north to the south, which are NNW, N, and NE, respectively, and the summer monsoon in the central and southern Zhejiang is weaker than the winter monsoon. The causes of strong winds along the coast of Zhejiang from atmospheric systems are cold air, typhoon, low pressure, high pressure at sea, and thunderstorm strong winds. Cold air northerly strong winds are most common from November to March of the following year, followed by typhoon strong winds in summer, mainly from July to October, and low-pressure strong winds in late spring and early summer.
参考文献:
[1] 陈秀宝, 温树伟, 张淑云. 浙江主要气象灾害概述[J]. 东海海洋, 1991, 9(1): 65-71. CHEN X B, WEN S W, ZHANG S Y. The meteorological calamity over Zhejiang[J]. Donghai Marine Science, 1991, 9(1): 65-71.
[2] BÄRRING L, VON STORCH H. Scandinavian storminess since about 1800[J]. Geophysical Research Letters, 2004, 31(20): L20202.
[3] 邱博, 张录军, 谭慧慧. 中国大风集中程度及气候趋势研究[J]. 气象科学, 2013, 33(5): 543-548. QIU B, ZHANG L J, TAN H H. Study on the gale concentration degree and climatic tendency in China[J]. Journal of the Meteorological Sciences, 2013, 33(5): 543-548.
[4] 曲巧娜, 盛春岩, 杨晓霞, 等. 黄、渤海沿海大风变化特征及影响系统[J]. 气象科学, 2018, 38(2): 212-220. QU Q N, SHENG C Y, YANG X X, et al. Variation characteristics of gale in the coastal Yellow Sea and the Bohai Sea and its weather system[J]. Journal of the Meteorological Sciences, 2018, 38(2): 212-220.
[5] 郑崇伟. 全球海域大风频率精细化统计分析[J]. 广东海洋大学学报, 2013, 33(6): 77-81. ZHENG C W. Statistics of gale frequency in global oceans[J]. Journal of Guangdong Ocean University, 2013, 33(6): 77-81.
[6] 吕爱民, 杨柳妮, 黄彬, 等. 中国近海大风的天气学分型[J]. 海洋气象学报, 2018, 38(1): 43-50. LYU A M, YANG L N, HUANG B, et al. Classification of synoptic patterns for China offshore gales[J]. Journal of Marine Meteorology, 2018, 38(1): 43-50.
[7] DING Y H, REN G Y, ZHAO Z C, et al. Detection, causes and projection of climate change over China: an overview of recent progress[J]. Advances in Atmospheric Sciences, 2007, 24(6): 954- 971.
[8] 王遵娅, 丁一汇, 何金海, 等. 近50年来中国气候变化特征的再分析[J]. 气象学报, 2004, 62(2): 228-236. WANG Z Y, DING Y H, HE J H, et al. An updating analysis of the climate change in China in recent 50 years[J]. Acta Meteorologica Sinica, 2004, 62(2): 228-236.
[9] 王小玲, 宋文玲. 近30a我国5 级以上风日数的时空变化特征[J]. 气候变化研究进展, 2008, 4(6): 347-351. WANG X L, SONG W L. Spatial and temporal variations in windy days over category 5 in China during 1975-2005[J]. Advances in Climate Change Research, 2008, 4(6): 347-351.
[10] 王畅, 刘倩, 龙强, 等. 唐山湾精细化海区大风特征初步分析[J]. 海洋预报, 2016, 33(1): 11-18. WANG C, LIU Q, LONG Q, et al. Preliminary analysis of strong wind over the fine sea area of Tangshan Bay[J]. Marine Forecasts, 2016, 33(1): 11-18.
[11] 郭俊建, 孙莎莎. 山东沿海精细化海区大风特征分析[J]. 海洋预报, 2014, 31(4): 41-46. GUO J J, SUN S S. Analysis of gale wind along Shandong coast [J]. Marine Forecasts, 2014, 31(4): 41-46.
[12] 李超, 魏建苏, 严文莲, 等. 江苏沿海大风特征及其变化分析[J]. 气象科学, 2013, 33(5): 584-589. LI C, WEI J S, YAN W L, et al. Synoptic and climatic survey of the gale in the coast of Jiangsu province[J]. Journal of the Meteorological Sciences, 2013, 33(5): 584-589.
[13] 夏丽花, 吴幸毓, 陈敏艳. 台湾海峡致灾大风气候特征分析[J]. 海峡科学, 2017(6): 3-8. XIA L H, WU X Y, CHEN M Y. Analysis on climate characteristics of disaster-causing Gale in the Taiwan Strait[J]. Straits Science, 2017(6): 3-8.
[14] 董加斌, 胡波. 浙江沿海大风的天气气候概况[J]. 台湾海峡, 2007, 26(4): 476-483. DONG J B, HU B. Synoptic and climatic survey of the gale in the coast of Zhejiang Province[J]. Journal of Oceanography in Taiwan Strait, 2007, 26(4): 476-483.
[15] 卢美, 朱业. 浙江沿海大风的天气气候特征[J]. 杭州师范大学学报(自然科学版), 2011, 10(5): 474-480. LU M, ZHU Y. Weather and climate characteristics of the coastal gale in Zhejiang[J]. Journal of Hangzhou Normal University (Natural Science Edition), 2011, 10(5): 474-480.
[16] 刘敏, 漆梁波. 嵊泗站大风的统计特征及其与平均风的关系[J]. 大气科学研究与应用, 2010(2): 83-92. LIU M, QI L B. Statistic characteristics of gale in Shengsi station and the relationship between gale and average wind force[J]. Atmospheric Science Research and Application, 2010(2): 83-92.
[17] 中国气象局. 地面气象观测规范[M]. 北京: 气象出版社, 2003: 21-27. China Meteorological Administration. Specification for surface meteorological observation[M]. Beijing: China Meteorological Press, 2003: 21-27.
[18] 曹兴, 万瑜, 陆辉, 等. 近30a新疆达坂城风区大风特征及其变化规律[J]. 干旱区研究, 2015, 32(1): 116-122. CAO X, WAN Y, LU H, et al. Gale and its change in Dabancheng, Xinjiang in recent 30 years[J]. Arid Zone Research, 2015, 32(1): 116-122.
[19] 赵宗慈, 罗勇, 江滢. 全球大风在减少吗?[J]. 气候变化研究进展, 2011, 7(2): 149-151. ZHAO Z C, LUO Y, JIANG Y. Is global strong wind declining? [J]. Advances in Climate Change Research, 2011, 7(2): 149-151.
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