欧美精品在线观看,色欲狠狠躁天天躁无码中文字幕,成熟妇人A片免费看网站

東海黑潮溫度鋒的三維結(jié)構(gòu)特征分析

單位：浙江海洋大學(xué) 海洋科學(xué)與技術(shù)學(xué)院, 浙江舟山 316022

分類號(hào)：P731.27

出版年·卷·期（頁碼）：2022·39·第一期（67-79）

摘要：

結(jié)合衛(wèi)星遙感海表溫度、三維再分析溫度資料和數(shù)值模擬結(jié)果，研究了東海黑潮溫度鋒從海表到底層的三維結(jié)構(gòu)特征。結(jié)果表明：東海黑潮海表溫度鋒在冬季和春季較強(qiáng)，秋季次之，夏季消失。多年平均的東海黑潮海表溫度鋒區(qū)范圍主要在70~700 m水深區(qū)域，溫度鋒的中心線與黑潮的流軸大致平行，在濟(jì)州島以南的黑潮中段區(qū)域有北上的分支。受臺(tái)灣暖流、黑潮及其分支的共同影響，在200 m以淺區(qū)域，東海黑潮溫度鋒在冬季和春季從海表到海底常年存在，夏季和秋季主要出現(xiàn)在水深50 m以下水層。東海黑潮和底層陸架水形成顯著的溫度鋒，位置在順著黑潮流向的左側(cè)及下方深度為100~700 m的陸架區(qū)域，該區(qū)域的溫度鋒強(qiáng)度比同一位置的海表溫度鋒的強(qiáng)度大。受黑潮的路徑、流幅寬度、深度和速度大小的影響，東海黑潮溫度鋒在陸架區(qū)域的影響深度兼具區(qū)域性差異和季節(jié)性差異，一般比黑潮流速0.2 m/s的到達(dá)深度深200 m左右，甚至可以影響到水深1 000 m左右。

Based on satellite remote sensing sea surface temperature data, three-dimensional reanalysis temperature data and numerical simulation results, the three-dimensional structure characteristics of Kuroshio thermal front in the East China Sea are studied in this paper. The Kuroshio thermal front at the sea surface in winter and spring are stronger than that in autumn and disappears in summer. The annual mean SST front zones mainly located in the area of water depth of 70~700 m. The core line of the thermal front is roughly parallel to the current axis of the Kuroshio with a northward branch in the middle region of the Kuroshio to the south of Jeju Island. The Kuroshio thermal front in the East China Sea is affected by the Taiwan Warm Current, the Kuroshio and its branches. It always exists from the surface to the bottom in winter and spring where the water is shallower than 200 m, while it mainly appears below 50 m in summer and autumn. The Kuroshio and the shelf water in the East China Sea can also form significant thermal front, which is located at the bottom-left side of the Kuroshio on the shelf area with a depth of 100~700 m. The intensity of the thermal front in this area is larger than that of the sea surface thermal front at the same location. Affected by the path, current amplitude, depth and velocity of the Kuroshio, the impact depth of Kuroshio thermal front in the East China Sea reveals both regional and seasonal differences. The front is generally 200 m deeper than the arrival depth of the Kuroshio's velocity of 0.2 m/s, and can even reach the depth of about 1 000 m.

參考文獻(xiàn)：

[1] 劉寶銀. 利用諾阿衛(wèi)星紅外信息對(duì)東海黑潮表層溫度鋒的解譯[J]. 山東海洋學(xué)院學(xué)報(bào), 1982, 12(3):11-20. Liu B Y. The interpretation on the surface temperature fronts of Kuroshio in the East China Sea using NOAA IR data[J]. Journal of Shandong College of Oceanology, 1982, 12(3):11-20.
[2] 林傳蘭. 東海黑潮鋒的海洋學(xué)特征及其與漁場的關(guān)系[J]. 海洋學(xué)研究, 1986(2):12-20. Lin C L. Oceanographic characteristics of the Kuroshio Front in the East China Sea and the relationship with fisheries[J]. Donghai Marine Science, 1986, 4(2):8-16.
[3] 劉敬武. 東海黑潮區(qū)海洋鋒的區(qū)域氣候?qū)W效應(yīng)[D]. 青島:中國海洋大學(xué), 2010. Liu J W. The regional climate effect of SST front in the vicinity of the Kuroshio in East China Sea[D]. Qingdao:Ocean University of China, 2010.
[4] 張然, 徐海明, 張百超. 東中國海黑潮海洋鋒的季節(jié)變化特征及其成因[J]. 氣象科學(xué), 2016, 36(2):203-211. Zhang R, Xu H M, Zhang B C. Seasonal variation of the SST front in the East China Sea and its causes[J]. Journal of the Meteorological Sciences, 2016, 36(2):203-211.
[5] 湯毓祥. 初論東海黑潮鋒的區(qū)域性差異[J]. 黃渤海海洋, 1992, 10(3):1-9. Tang Y X. On regional difference of the Kuroshio front in the East China Sea[J]. Journal of Oceanography of Huanghai & Bohai Seas, 1992, 10(3):1-9.
[6] 郭炳火, 萬邦君, 湯毓祥. 東海海洋鋒的波動(dòng)及演變特征[J]. 黃渤海海洋, 1995, 13(2):1-10. Guo B H, Wan B J, Tang Y X. Wavelike features and evolution of the Oceanic Fronts in the East China Sea[J]. Journal of Oceanography of Huanghai & Bohai Seas, 1995, 13(2):1-10.
[7] 賈英來, 劉秦玉, 劉偉, 等. 臺(tái)灣以東黑潮流量的年際變化特征[J]. 海洋與湖沼, 2004, 35(6):507-512. Jia Y L, Liu Q Y, Liu W, et al. The interannual variation of the Kuroshio transport East of Taiwan[J]. Oceanologia et Limnologia Sinica, 2004, 35(6):507-512.
[8] 劉傳玉. 中國東部近海溫度鋒面的分布特征和變化規(guī)律[D]. 青島:中國科學(xué)院研究生院(海洋研究所), 2009. Liu C Y. Distribution and variations of the thermal fronts in the eastern China Seas[D]. Qingdao:Graduate School of the Chinese Academy of Sciences (Institute of Oceanology), 2009.
[9] 湯毓祥, 鄭義芳. 關(guān)于黃、東海海洋鋒的研究[J]. 海洋通報(bào), 1990, 9(5):89-96. Tang Y X, Zheng Y F. Research on fronts in East China Sea[J]. Marine Science Bulletin, 1990, 9(5):89-96.
[10] Shibata A. Meander of the Kuroshio along the edge of the continental shelf in the East China Sea[J]. Umi to Sora, 1983, 58(4):113-120.
[11] Sugimoto T, Kimura S, Miyaji K. Meander of the Kuroshio front and current variability in the East China Sea[J]. Journal of the Oceanographical Society of Japan, 1988, 44(3):125-135.
[12] Qiu B, Toda T, Imasato N. On Kuroshio front fluctuations in the East China Sea using satellite and in situ observational data[J]. Journal of Geophysical Research:Oceans, 1990, 95(C10):18191- 18204.
[13] 任詩鶴, 王輝, 劉娜. 中國近海海洋鋒和鋒面預(yù)報(bào)研究進(jìn)展[J]. 地球科學(xué)進(jìn)展, 2015, 30(5):552-563. Ren S H, Wang H, Liu N. Review of ocean front in Chinese marginal seas and frontal forecasting[J]. Advances in Earth Science, 2015, 30(5):552-563.
[14] 鄭全安, 袁業(yè)立. 切變波動(dòng)力學(xué)研究Ⅰ. 尺度分析與頻散關(guān)系[J]. 海洋學(xué)報(bào), 1988, 10(6):659-665. Zheng Q A, Yuan Y L. Study on shear wave dynamics Ⅰ. Scale analysis and dispersion relationship[J]. Acta Oceanologica Sinica, 1988, 10(6):659-665.
[15] 李立, 蘇紀(jì)蘭, 許建平. 南海的黑潮分離流環(huán)[J]. 熱帶海洋學(xué)報(bào), 1997, 16(2):42-57. Li L, Su J L, Xu J P. Detached Kuroshio rings in the South China Sea[J]. Tropic Oceanology, 1997, 16(2):42-57.
[16] 郭炳火, 葛人峰. 東海黑潮鋒面渦旋在陸架水與黑潮水交換中的作用[J]. 海洋學(xué)報(bào), 1997, 19(6):1-11. Guo B H, Ge R F. The role of the East China Sea Kuroshio front vortex in the exchange between shelf water and Kuroshio water[J]. Acta Oceanologica Sinica, 1997, 19(6):1-11.
[17] 袁耀初, 蘇紀(jì)蘭. 1995年以來我國對(duì)黑潮及琉球海流的研究[J]. 科學(xué)通報(bào), 2000, 45(22):2353-2356. Yuan Y C, Su J L. Research on Kuroshio and Ryukyu Current in my country since 1995[J]. Chinese Science Bulletin, 2000, 45(22):2353-2356.
[18] 陳春濤, 劉佳佳. 東海北部黑潮鋒面渦的快速生成和消散[J]. 遙感信息, 2010(3):103-107, 128. Chen C T, Liu J J. The generation and evanescence of frontal eddy in the East China Sea[J]. Remote Sensing Information, 2010(3):103-107, 128.
[19] 賈永君. 東海黑潮鋒面不穩(wěn)定過程遙感與數(shù)值模擬研究[D]. 青島:中國科學(xué)院研究生院(海洋研究所), 2010. Jia Y J. Remote sensing and numerical simulation of the Kuroshio frontal instability process in the East China Sea[D]. Qingdao:Graduate School of the Chinese Academy of Sciences (Institute of Oceanology), 2010.
[20] 李威, 王琦, 馬繼瑞, 等. 臺(tái)灣以東黑潮鋒的中尺度過程研究[J]. 海洋通報(bào), 2011, 30(5):518-528. Li W, Wang Q, Ma J R, et al. Study on the meso-scale process of the Kuroshio front to the east of Taiwan[J]. Marine Science Bulletin, 2011, 30(5):518-528.
[21] Donlon C J, Martin M, Stark J, et al. The operational sea surface temperature and sea ice analysis (OSTIA) system[J]. Remote Sensing of Environment, 2012, 116:140-158.
[22] Locarnini R A, Mishonov A V, Antonov J I, et al. World ocean atlas 2013, volume 1:temperature[R]. NOAA Atlas NESDIS 73. Silver Spring:NOAA, 2013:40.
[23] 黨振中, 周立佳, 劉建斌, 等. 基于WOA13數(shù)據(jù)的東海黑潮主軸溫度鋒特征分析[J]. 海洋技術(shù)學(xué)報(bào), 2016, 35(4):26-30. Dang Z Z, Zhou L J, Liu J B, et al. Analysis on the characteristics of the Kuroshio temperature front in the East China Sea based on WOA13 data[J]. Journal of Ocean Technology, 2016, 35(4):26-30.
[24] 劉鵬, 張永剛, 劉建斌. 基于WOA13數(shù)據(jù)的赤道大西洋海區(qū)溫度鋒的時(shí)空分布特征分析[J]. 海洋預(yù)報(bào), 2017, 34(5):47-57. Liu P, Zhang Y G, Liu J B. Temporal and spatial distribution characteristics of temperature front in the equatorial Atlantic based on WOA13 data[J]. Marine Forecasts, 2017, 34(5):47-57.
[25] 于洪華, 苗育田. 東海黑潮鋒的特征分析. 黑潮調(diào)查研究論文選(三)[M]. 北京:海洋出版社, 1991. Yu H H, Miao Y T. Characteristic analysis of the Kuroshio front in the East China Sea. Selected papers on the Kuroshio survey (3)[M]. Beijing:Ocean Press, 1991.
[26] James C, Wimbush M, Ichikawa H. Kuroshio meanders in the East China Sea[J]. Journal of Physical Oceanography, 1999, 29(2):259-272.
[27] Liu Choteng and Pai Suchuan. As Kuroshio turns:(Ⅱ) the oceanic front North of Taiwan[J]. 1987, 18:49-61.
[28] 羅義勇, 吳德星, 林霄沛. 地形對(duì)東海黑潮鋒面彎曲影響研究[J]. 青島海洋大學(xué)學(xué)報(bào), 2001, 31(3):305-312. Luo Y Y, Wu D X, Lin X P. Effects of topography on Kuroshio frontal meanders in the East China Sea[J]. Journal of Ocean University of Qingdao, 2001, 31(3):305-312.
[29] 蘇紀(jì)蘭. 中國近海的環(huán)流動(dòng)力機(jī)制研究[J]. 海洋學(xué)報(bào), 2001, 23(4):1-16. Su J L. A review of circulation dynamics of the coastal oceans near China[J]. Acta Oceanologica Sinica, 2001, 23(4):1-16.

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】