首頁(yè)期刊介紹通知公告編 委 會(huì)投稿須知電子期刊廣告合作聯(lián)系我們在線留言
 
1971—2020年南海生成熱帶氣旋的活動(dòng)規(guī)律與大風(fēng)分布特征
作者:楊亞新 
單位:江蘇航運(yùn)職業(yè)技術(shù)學(xué)院 航海技術(shù)學(xué)院, 江蘇 南通 226010
關(guān)鍵詞:南海 熱帶氣旋 活動(dòng)規(guī)律 大風(fēng)分布特征 
分類號(hào):P444
出版年·卷·期(頁(yè)碼):2024·41·第一期(104-111)
摘要:
利用東京臺(tái)風(fēng)中心提供的1971—2020年的西北太平洋熱帶氣旋資料,對(duì)南海生成熱帶氣旋的發(fā)生頻數(shù)、發(fā)生源地、強(qiáng)度和持續(xù)時(shí)間、移動(dòng)路徑以及大風(fēng)分布特征進(jìn)行統(tǒng)計(jì)分析。結(jié)果表明:南海熱帶氣旋主要生成于5—12月,其中6—9月為盛行期,約有70%的熱帶氣旋生成;熱帶氣旋生成位置季節(jié)變化明顯,6—9月多生成于南海北部17°N附近,11月—次年4月多生成于14°N以南的南海南部,5月和10月為季節(jié)轉(zhuǎn)換期,生成位置大幅北進(jìn)或南撤;熱帶氣旋中心最低氣壓為940~1 004 hPa,平均值為985.4 hPa,近中心最大風(fēng)速為35~85 kt,平均值為48.3 kt,平均持續(xù)天數(shù)為6.2 d;熱帶氣旋移動(dòng)路徑以西移和西北移路徑居多,各月都有發(fā)生,其次為東北移路徑,主要發(fā)生在5—6月;近90%的南海熱帶氣旋10級(jí)以上大風(fēng)以中心呈對(duì)稱分布,大風(fēng)圈平均半徑為53.2 n mile,在7級(jí)以上大風(fēng)中以中心呈對(duì)稱分布的略多于不對(duì)稱分布的,7級(jí)大風(fēng)圈的平均半徑為142.3 n mile。
Based on the data of tropical cyclones in the Northwestern Pacific from 1971 to 2020 provided by the Tokyo typhoon center, the occurrence frequency, origin location, intensity and duration, moving path and gale distribution characteristics of tropical cyclones generated in the South China Sea are statistically analyzed. The following main conclusions are obtained: tropical cyclones in the South China Sea mainly occur during May and December, in which June to September is the prevailing period, and the occurrence frequency in these four months accounts for about 70% of annual number. The seasonal variation of the cyclone origins is large. From June to September, cyclones originate near 17°N in the northern South China Sea on average. From November to April of the next year, cyclones originate in the southern South China Sea (south of 14°N). May and October are the seasonal transition periods, and the origin locations of cyclones shift northward or southward significantly; The minimum pressure of the cyclone center is 940~1 004 hPa with an average of 985.4 hPa, the maximum wind speed near the cyclone center is 35~85 kt with an average of 48.3 kt, and the average duration is 6.2 d; Most of the cyclones move westward and northwestward during June and December, followed by northeastward during May and June. Strong winds above force 10 associated with nearly 90% of the South China Sea tropical cyclones are symmetrically distributed with respect to the center, and the average radius of the strong wind circle is 53.2 n miles. The symmetrically distributed strong winds above force 7 are slight more than the asymmetrically distributed strong winds above force 7, and the average radius of the strong wind circle is 142.3 n miles.
參考文獻(xiàn):
[1] 梁梅, 鐘校堯, 徐建軍, 等. 1960—2017年南海熱帶氣旋強(qiáng)度突變特征[J]. 廣東海洋大學(xué)學(xué)報(bào), 2020, 40(3): 83-91. LIANG M, ZHONG X Y, XU J J, et al. Sudden changes in tropical cyclone intensity in South China Sea from 1960 to 2017[J]. Journal of Guangdong Ocean University, 2020, 40(3): 83-91.
[2] 孔寧謙, 陳潤(rùn)珍, 蔡敏. 改進(jìn)的持續(xù)法作盛夏南海熱帶氣旋強(qiáng)度和路徑預(yù)報(bào)方法[J]. 海洋預(yù)報(bào), 2006, 23(2): 52-55. KONG N Q, CHEN R Z, CAI M. The advanced climatic persistence method of forecasting tropical-cyclone track and intensity in South China Sea during midsummer[J]. Marine Forecasts, 2006, 23(2): 52-55.
[3] 李宇, 孔寧謙, 陳潤(rùn)珍. 用模糊聚類分型方法作盛夏南海熱帶氣旋路徑預(yù)報(bào)[J]. 海洋預(yù)報(bào), 2008, 25(3): 81-85. LI Y, KONG N Q, CHEN R Z. Difference of QBO structure between east Asia monsoon region and south Asia monsoon region [J]. Marine Forecasts, 2008, 25(3): 81-85.
[4] 李春暉, 劉春霞, 程正泉. 近50年南海熱帶氣旋時(shí)空分布特征及其海洋影響因子[J]. 熱帶氣象學(xué)報(bào), 2007, 23(4): 341-347. LI C H, LIU C X, CHENG Z Q. The characteristics of temporal and spatial distribution of tropical cyclone frequencies over the South China Sea and its affecting oceanic factors in the past 50yrs [J]. Journal of Tropical Meteorology, 2007, 23(4): 341-347.
[5] 江文, 王東海, 張春燕, 等. 近70年不同路徑的南海熱帶氣旋的統(tǒng)計(jì)特征[J]. 熱帶氣象學(xué)報(bào), 2022, 38(3): 433-443. JIANG W, WANG D H, ZHANG C Y, et al. Statistical characteristics of tropical cyclones in the South China Sea with different tracks in the past 70 years[J]. Journal of Tropical Meteorology, 2022, 38(3): 433-443.
[6] 秦南南, 鐘瑋, 趙嘉琦. 1949-2017年南海地區(qū)熱帶氣旋統(tǒng)計(jì)特征研究[J]. 氣象研究與應(yīng)用, 2019, 40(3): 1-4. QIN N N, ZHONG W, ZHAO J Q. Statistical characteristics of tropical cyclones in the South China Sea from 1949 to 2017[J]. Journal of Meteorological Research and Application, 2019, 40(3):1-4.
[7] 廖菲, 李文婷, 張子然, 等. 1949-2017年南海海域熱帶氣旋強(qiáng)度和路徑快速變化統(tǒng)計(jì)特征[J]. 海洋學(xué)報(bào), 2019, 41(9): 126-135. LIAO F, LI W T, ZHANG Z R, et al. Analysis of rapid changes of tropical cyclones over the South China Sea for 1949-2017[J]. Haiyang Xuebao, 2019, 41(9): 126-135.
[8] 曹力戈, 王喜冬, 李威, 等. 路經(jīng)南海熱帶氣旋迅速加強(qiáng)的年代際變化[J]. 海洋學(xué)報(bào), 2021, 43(5): 50-62. CAO L G, WANG X D, LI W, et al. Multidecadal variability of rapid intensification of tropical cyclones passing through the South China Sea[J]. Haiyang Xuebao, 2021, 43(5): 50-62.
[9] 黃小燕, 管兆勇, 何潔琳, 等. 南海ITCZ異常變化及其對(duì)非移入性南海熱帶氣旋(TC)活動(dòng)的可能影響[J]. 大氣科學(xué), 2017, 41(1):1-14. HUANG X Y, GUAN Z Y, HE J L, et al. Variations of ITCZ in the South China Sea and their possible influences on the South China Sea-generated tropical cyclone (SCS-G TC) activities[J]. Chinese Journal of Atmospheric Sciences, 2017, 41(1): 1-14.
[10] 胡皓, 端義宏. 南海熱帶氣旋迅速加強(qiáng)環(huán)境場(chǎng)因子的影響分析[J]. 熱帶氣象學(xué)報(bào), 2016, 32(3): 299-310. HU H, DUAN Y H. Analysis of environmental variables of rapidly intensifying tropical cyclones in the South China Sea[J]. Journal of Tropical Meteorology, 2016, 32(3): 299-310.
[11] Japan Meteorological Agency. RSMC best track data (text) (1951-2023)[EB/OL]. [2022-03-20]. https://www.jma.go.jp/jma/jma-eng/jma-center/rsmc-hp-pub-eg/trackarchives.html.
[12] 郝賽, 毛江玉. 西北太平洋與南海熱帶氣旋活動(dòng)季節(jié)變化的差異及可能原因[J]. 氣候與環(huán)境研究, 2015, 20(4): 380-392. HAO S, MAO J Y. Differences of the seasonal variations of tropical cyclone activities over the South China Sea and the western north Pacific and the possible causes[J]. Climatic and Environmental Research, 2015, 20(4): 380-392.
[13] 楊亞新. 西北太平洋熱帶氣旋中大風(fēng)和波浪分布特征[J]. 上海海事大學(xué)學(xué)報(bào), 2015, 36(4): 74-78. YANG Y X. Distribution characteristics of wind and wave in tropical cyclone of western North Pacific[J]. Journal of Shanghai Maritime University, 2015, 36(4): 74-78.
服務(wù)與反饋:
文章下載】【發(fā)表評(píng)論】【查看評(píng)論】【加入收藏
 
 海洋預(yù)報(bào)編輯部 地址:北京海淀大慧寺路8號(hào) 電話:010-62105776
投稿網(wǎng)址:http://familyfy.cn
郵箱:bjb@nmefc.cn
本系統(tǒng)由北京博淵星辰網(wǎng)絡(luò)科技有限公司設(shè)計(jì)開發(fā) 技術(shù)支持電話:010-63361626
塔城市| 苍山县| 独山县| 南丹县| 黄大仙区| 高州市| 南陵县| 南开区| 历史| 奉节县| 三门峡市| 香港 | 五家渠市| 安顺市| 讷河市| 绥芬河市| 鹤庆县| 阿城市| 修文县| 翁牛特旗| 平江县| 武山县| 闸北区| 沙洋县| 玉林市| 简阳市| 双柏县| 兴海县| 宁河县| 阜新市| 乌审旗| 乌拉特后旗| 墨竹工卡县| 新密市| 忻城县| 沈阳市| 富蕴县| 饶平县| 恩平市| 普宁市| 凤城市|