Analysis on the sea level anomaly high of 2012 in China coastal area
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摘要: 2012年,中国沿海海平面变化最突出的特点是海平面升高显著。海平面总体比常年高122 mm,较2011年偏高53 mm,达1980年以来最高位。本文使用中国沿海及西北太平洋区域近30 a的水位、海温、气温、气压和风等水文气象资料,详细分析了中国沿海海平面2012年异常偏高的成因。结果表明:2010-2012年中国沿海海平面处于2~3 a、8~9 a和准19 a周期震荡的高位,几个周期震荡高位叠加,对海平面上升起了明显的影响;2012年,沿海气温和海温分别较常年偏高0.4℃和0.3℃,气压较常年低1.2 hPa,气压达历史最低位;2012年,中国南海夏季风爆发时间较常年偏早,结束较常年偏晚,季风持续时间较常年偏长,导致2012年5-6月和8月,在黄海和东海海域,东北风持续偏强,南海海域南风偏强,风场的异常导致黄海、东海和南海沿海海水长时间堆积,是造成海平面升高的原因之一;2012年,热带气旋登陆时间集中,影响范围广,北上和影响东北地区的台风数量均为历史之最,特别是2012年8月,有6个热带气旋相继影响我国沿海,对当月海平面升高影响明显;另外,2012年副热带高压偏北、偏东、偏弱的特点对东海和南海的海平面上升也有一定影响。Abstract: In 2012,the sea level anomaly high was the most prominent feature of sea level change in China coastal. The sea level was 122 mm higher than normal,53 mm higher than 2011,reached its highest level since 1980. Based on the 30 years water level,sea surface temperature,air temperature,barometric pressure and wind hydrological and meteorological data,the sea level anomaly high of 2012 in the China coastal area is investigated. The research results show: the coincidence of several long-period vibration made the sea level high during 2010 to 2012. In 2012,China coastal area air temperature and ocean temperature were higher than normal,the barometric pressure was 1.2 hpa lower than normal,reaching the lowest level in history; in 2012,SCSSM time was earlier than normal,and later than normal end,the South China Sea strongest southerly wind lead China Yellow Sea,East China Sea and South China Sea coastal waters for a long time accumulation,which caused sea level rise. In 2012,tropical cyclones landing time was focus,the number of typhoons affecting a wide range of northern regions were the most of history,especially in August 2012,there were six tropical cyclones affecting China's coastal area,sea level rise for the month obviously. In addition,the subtropical high was northerly,easterly and weakness,which also have some impact on the sea level rise of the East China Sea and South China Sea in 2012.
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Key words:
- sea level rise /
- significant period /
- air pressure /
- monsoon /
- tropical cyclones
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于宜法.中国近海海平面变化研究进展[J].中国海洋大学学报(自然科学版), 2004, 34(5):713-719. Intergovernmental Panel on Climate Change(IPCC). Climate Change 2007: The physical Science Basis[R]. Contribution of Working Group I to the Fourth Assessment Report of the intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 2007. 左军成, 于宜法, 陈宗镛.中国沿岸海平面变化原因的探讨[J].地球科学进展, 1994, 9(5):48-53. 国家海洋局.2011年中国海平面公报[R].2012. 国家海洋局.2012年中国海平面公报[R].2013. Zhang Jianli, Chen Manchun, Chen Meixiang, et al. Characteristics of SST variation/change in the coastal region of the East China Sea[C]//Proceeding of the Nineteenth(2009) International Offshore and Polar Engineering Conference.Japan, 2009:483-489. 方国洪, 郑文振, 陈宗镛, 等.潮汐和潮流的分析和预报[M].北京:海洋出版社, 1986, 268-281. 郑文振, 陈宗镛.我国海平面年速率的分布和长周期分潮的变化[J].海洋学报, 1999, 21:65-74. 王慧, 范文静, 李琰, 等.渤黄海沿海2月份海平面异常偏高成因分析[J].海洋通报, 2012, 31(3):255-261. 王慧, 范文静, 张建立, 等.中国沿海近31年冬季海平面变化特征[J].海洋通报, 2012, 30(6):637-643. 王慧, 范文静, 高志刚, 等.渤黄海沿海季节性海平面异常偏高影响及成因分析[J].海洋通报, 2012, 31(6):613-620. 左军成, 杜凌, 陈美香, 等.气候变化背景下海平面变化及其影响与应用[M].北京:科学出版社, 2013. 蔡榕硕, 等.气候变化对中国近海生态系统的影响[M].北京:海洋出版社, 2010. 李崇银.异常东亚季风和ENSO循环[M].北京:海洋出版社, 2001. 王慧, 刘克修, 张建立, 等.三沙市海域海平面变化[J]. 海洋学报, 2013, 35(3): 11-17. 陈上及, 马继瑞.海洋数据处理分析方法及其应用[M].北京:海洋出版社, 1991. Farge M. Wavelet transforms and their applications to turbulence[J]. Annu Rev Fluid Mech, 1992, 24∶95-457. Lau K-M, Weng Hengyi. Climate Signal Detection Using Wavlet Transform:How to Make a Time Series Sing[J]. American Meteorological Society, 1995, 76(12):2391-2402. 国家海洋局.2010年中国海平面公报[R].2011. 国家气象局.2012年中国气候公报[R].2013. 丁荣荣, 左军成, 杜凌, 等.南海海平面变化及其比容高度和风场的关系[J].中国海洋大学学报, 2007, 37(增刊2):23-30.
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