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
 
東中國(guó)海海溫在增暖停滯期的變化特征及成因分析
作者:張琪1  龍景超2 
單位:1. 國(guó)家海洋局天津海洋環(huán)境監(jiān)測(cè)中心站, 天津市海洋環(huán)境監(jiān)測(cè)預(yù)報(bào)中心, 天津 300457;
2. 廣東海洋大學(xué) 海洋與氣象學(xué)院/南海海洋氣象研究院, 廣東 湛江 524088
關(guān)鍵詞:中國(guó)近海 海表溫度 增暖停滯期 凈熱通量 黑潮 
分類號(hào):P731.11
出版年·卷·期(頁(yè)碼):2021·38·第一期(78-82)
摘要:
通過(guò)HadSST3原始觀測(cè)數(shù)據(jù)和HadISST1重組數(shù)據(jù),分析了東中國(guó)海海溫在增暖停滯期(1998—2014年)的變化特征。研究表明:兩組數(shù)據(jù)的海溫變化特征和程度相似。在增暖停滯期,渤海、黃海和東海海溫線性趨勢(shì)主要表現(xiàn)為負(fù),降溫最多的集中在長(zhǎng)江口附近,約-1℃。渤海、黃海及東海部分區(qū)域的凈熱通量對(duì)海溫降低起正作用,而在東海黑潮區(qū)海洋的凈熱通量對(duì)海溫降低起負(fù)作用,黑潮入侵的減弱可能是東海海表溫度下降的主要原因。在增暖停滯期,海溫變化趨勢(shì)具有較顯著的區(qū)域性季節(jié)特征。春季海溫幾乎呈現(xiàn)全海盆的下降趨勢(shì),尤以長(zhǎng)江口附近下降最多,可達(dá)-1.4℃;夏季海溫下降趨勢(shì)較春季減弱,下降最多的地區(qū)主要集中在渤海;秋季渤海海溫下降較明顯;冬季海溫變化主要在長(zhǎng)江口沿岸,渤黃海海溫的變化并不明顯。
In this study, the trends of SST over the eastern China seas in the warming hiatus period (1998-2014) are analyzed using the un-interpolated dataset HadSST3 and the reconstructed dataset HadISST1. The results show that the SST in the Bohai Sea, Yellow Sea and East China Sea mainly reveals a decreasing trend during the warming hiatus period with the maximum value of about -1℃ near the Yangtze River estuary. The net heat flux plays a positive role in the decrease of SST in the Bohai Sea, Yellow Sea and part of the East China Sea. However, it plays a negative role in the Kuroshio area of the East China Sea, where the weakening of Kuroshio intrusion may be the main reason for the decrease of SST. The trend of SST variation reveals significant regional and seasonal characteristics during the warming hiatus period. In spring, the SST shows a decreasing trend over almost the whole eastern China seas, especially for the area near Yangtze River estuary where the SST decreases by about -1.4℃. The decreasing trend of SST in summer is weaker than that in spring, and the most decreasing area is mainly in the Bohai Sea. In autumn, the SST in the Bohai Sea decreases significantly. In winter, the SST variation is mainly along the Yangtze River Estuary, while it is not significant in the Bohai Sea and Yellow Sea.
參考文獻(xiàn):
[1] Tang X H, Wang F, Chen Y L, et al. Warming trend in northern East China Sea in recent four decades[J]. Chinese Journal of Oceanology and Limnology, 2009, 27(2):185-191.
[2] 馮琳, 林霄沛. 1945~2006年?yáng)|中國(guó)海海表溫度的長(zhǎng)期變化趨勢(shì)[J]. 中國(guó)海洋大學(xué)學(xué)報(bào), 2009, 39(1):13-18.
[3] Wu L X, Cai W J, Zhang L P, et al. Enhanced warming over the global subtropical western boundary currents[J]. Nature Climate Change, 2012, 2(3):161-166, doi:10.1038/nclimate1353.
[4] 張琪. 中國(guó)近海海表溫度的年代際變化及其對(duì)全球變暖的響應(yīng)[D]. 青島:中國(guó)海洋大學(xué), 2014.
[5] Cai R S, Tan H J, Kontoyiannis H. Robust surface warming in offshore China seas and its relationship to the east Asian monsoon wind field and ocean forcing on interdecadal time scales[J]. Journal of Climate, 2017, 30(22):8987-9005.
[6] 宋春陽(yáng), 姜華, 張守文, 等. 2017年中國(guó)近海海表溫度特征[J]. 海洋預(yù)報(bào), 2019, 36(1):1-9.
[7] Smith T M, Peterson T C, Lawrimore J H, et al. New surface temperature analyses for climate monitoring[J]. Geophysical Research Letters, 2005, 32(14):L14712.
[8] Easterling D R, Wehner M F. Is the climate warming or cooling?[J]. Geophysical Research Letters, 2009, 36(8):L08706,.
[9] Medhaug I, Stolpe M B, Fischer E M, et al. Reconciling controversies about the'global warming hiatus'[J]. Nature, 2017, 545(7652):41-47.
[10] Kosaka Y, Xie S P. Recent global-warming hiatus tied to equatorial Pacific surface cooling[J]. Nature, 2013, 501(7467):403-407.
[11] Dai A G, Fyfe J C, Xie S P, et al. Decadal modulation of global surface temperature by internal climate variability[J]. Nature Climate Change, 2015, 5(6):555-559.
[12] McGregor S, Timmermann A, Stuecker M F, et al. Recent walker circulation strengthening and Pacific cooling amplified by Atlantic warming[J]. Nature Climate Change, 2014, 4(10):888-892.
[13] 譚紅建, 蔡榕碩, 黃榮輝. 中國(guó)近海海表溫度對(duì)氣候變暖及暫緩的顯著響應(yīng)[J]. 氣候變化研究進(jìn)展, 2016, 12(6):500-507.
[14] 徐萃薇, 孫繩武. 計(jì)算方法引論[M]. 3版. 北京:高等教育出版社, 2007.
[15] 劉秦玉, 謝尚平, 鄭小童. 熱帶海洋-大氣相互作用[M]. 北京:高等教育出版社, 2013:14.
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
大足县| 恩平市| 东港市| 固始县| 繁峙县| 咸阳市| 绥滨县| 涿州市| 岳阳县| 石楼县| 九龙坡区| 蕉岭县| 彭阳县| 旬阳县| 克东县| 咸丰县| 沧州市| 武平县| 南充市| 嵩明县| 贵南县| 博野县| 洮南市| 海宁市| 应城市| 洛南县| 普兰县| 东乡族自治县| 焦作市| 惠州市| 温宿县| 阿克陶县| 车险| 荃湾区| 达孜县| 广州市| 遂川县| 应用必备| 安康市| 黔江区| 大城县|