福建沿海海水表層溫度實(shí)測(cè)數(shù)據(jù)個(gè)例分析

作者：朱本璐  陳金瑞  鄭祥靖  李星

單位：福建省海洋預(yù)報(bào)臺(tái), 福建 福州 350003

關(guān)鍵詞：海水表層溫度 日變化 周期分析

分類號(hào)：P731.11

出版年·卷·期（頁碼）：2019·36·第一期（69-75）

摘要：

采用福建沿海4個(gè)站點(diǎn)（包括浮標(biāo)）2016年的實(shí)測(cè)水文氣象數(shù)據(jù)，初步分析了不同天氣系統(tǒng)影響情況下海表溫度的變化特征。研究結(jié)果表明：福建沿海月均海溫日變化和氣溫日變化有一定關(guān)系，二者都有明顯的日變化周期，海溫的日變化的峰值略滯后于氣溫日變化的峰值；無明顯天氣系統(tǒng)影響時(shí)，海溫和氣溫的變化趨勢(shì)比較一致，有冷空氣或臺(tái)風(fēng)系統(tǒng)影響時(shí)海溫和氣溫的變化趨勢(shì)不再一致；冷空氣系統(tǒng)影響時(shí)氣溫下降的時(shí)間從北到南依次滯后，而海溫的下降從北到南延遲不明顯；7月上升流的作用使得古雷浮標(biāo)附近海表溫度降低，并且周期發(fā)生明顯改變。

This study preliminarily analyzes observed hydro-meteorological data of four sites (including buoys) along Fujian coastal waters in 2016 to reveal the variation characteristics of sea surface temperature (SST) under the influence of different weather systems. The results show evident diurnal cycle of both monthly-averaged SST and air temperature, in which the peak of SST lags that of air temperature. The variation trends of SST and air temperature exhibits distinct consistence without influence of significant weather system. However, the consistence vanishes with influence of cold air or typhoon. Air temperature starts to decrease from the north to the south under the influence of cold air system, whereas the decrease of SST doesn't show evident lag between the north and south. The SST near Gulei buoy decreases attributed to the upwelling in July with significant variation of its cycle.

參考文獻(xiàn)：

[1] 容志明, 宗林植. 西沙群島海區(qū)表層海水溫度的譜分析[J]. 南海研究與開發(fā), 1991, (2):1-5. [2] 余克服. 雷瓊海區(qū)近40年海溫變化趨勢(shì)[J]. 熱帶地理, 2000, 20(2):111-115. [3] 郭偉其, 沙偉, 沈紅梅, 等. 東海沿岸海水表層溫度的變化特征及變化趨勢(shì)[J]. 海洋學(xué)報(bào), 2005, 27(5):1-8. [4] 湯超蓮, 鄭兆勇, 游大偉, 等. 珠江口近30a的SST變化特征分析[J]. 臺(tái)灣海峽, 2006, 25(1):96-101. [5] 莊樺. 沿岸海域海溫研究進(jìn)展[J]. 中國水運(yùn), 2014, 14(2):194-195. [6] 夏華永, 古萬才. 廣西沿海海洋站觀測(cè)海水溫度的統(tǒng)計(jì)分析[J]. 海洋通報(bào), 2000, 19(4):15-21. [7] 趙冬至. 中國典型海域赤潮災(zāi)害發(fā)生規(guī)律[M]. 北京:海洋出版社, 2010:326-330. [8] Hu J Y, Kawamura H, Hong H S, et al. A review of research on the upwelling in the Taiwan Strait[J]. Bulletin of Marine Science, 2003, 73(3):605-628. [9] Hu J Y, Kawamura H, Li C Y, et al. Review on current and seawater volume transport through the Taiwan Strait[J]. Journal of Oceanography, 2010, 66(5):591-610. [10] Jiang Y W, Chai F, Wan Z W, et al. Characteristics and mechanisms of the upwelling in the southern Taiwan Strait:a three-dimensional numerical model study[J]. Journal of Oceanography, 2011, 67(6):699-708. [11] 苗馨, 胡建宇. 用沿岸上升流指數(shù)分析中國東南沿岸風(fēng)生上升流的特征[J]. 海洋通報(bào), 2011, 30(3):258-265. [12] 李燕, 張建華, 劉欽政, 等. 單站海溫短期預(yù)報(bào)自動(dòng)化[J]. 海洋預(yù)報(bào), 2007, 24(4):33-41. [13] Burg J P. Maximum entropy spectral analysis[C]//Presented at 37th annual international SEG meeting. Oklahoma City, USA:Society of Exploration Geophysics, 1967. [14] 鄭兆勇, 周雄, 江四義, 等. 近50年華南沿海SST熱事件變化的時(shí)空特征[J]. 熱帶海洋學(xué)報(bào), 2010, 29(4):14-19.

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