南海黄岩岛珊瑚记录的1780-2013年的表层海温年代际变化特征

林丽芳; 余克服; 陶士臣; 韩韬; 张会领

doi:10.3969/j.issn.0253-4193.2018.09.003

南海黄岩岛珊瑚记录的1780-2013年的表层海温年代际变化特征

doi: 10.3969/j.issn.0253-4193.2018.09.003

1.
中国科学院南海海洋研究所中国科学院边缘海与大洋地质重点实验室, 广东广州 510301;中国科学院大学, 北京 100049
2.
中国科学院南海海洋研究所中国科学院边缘海与大洋地质重点实验室, 广东广州 510301;广西大学珊瑚礁研究中心, 广西南宁 530004
3.
中国科学院南海海洋研究所中国科学院边缘海与大洋地质重点实验室, 广东广州 510301
4.
广东海洋大学工程学院海洋工程系, 广东湛江 524088

基金项目: 国家自然科学基金重点项目（91428203）；国家重大科学研究计划项目（2013CB956102）。

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出版历程
- 收稿日期: 2017-10-13
- 修回日期: 2018-03-10

Interdecadal variability of sea surface temperature from 1780 to 2013 recorded in corals from the Huangyan Island in the South China Sea

1.
Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;University of Chinese Academy of Science, Beijing 100049, China
2.
Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Coral Reef Research Center of China, Guangxi University, Nanning 530004, China
3.
Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
4.
Department of Ocean Engineering, Faculty of Engineering, Guangdong Ocean University, Zhanjiang 524088, China

摘要

摘要: 基于南海中部黄岩岛滨珊瑚生长率与表层海温距平（SSTA）的正相关关系，重建了1780-2013年（共234年）黄岩岛海域SSTA年际变化序列。结果表明，1780-1890年SSTA总体偏低，平均为-0.2℃，最低SSTA为-1℃（1837年），对应于小冰期晚期；1890年以来SSTA总体呈阶段性上升，其中1971-1998年升温最快，1998年达到峰值（2℃），之后SSTA略呈下降趋势，冷暖变化与北半球陆地温度变化基本是同步的。频谱分析显示，黄岩岛海域SSTA在过去234年主要呈现出26~34 a的冷暖周期波动，其相位转变基本与太平洋年代际振荡冷-暖位相同步。近234年来南海中部黄岩岛海域SSTA的年代际变率并不是持续不变的，1890年以来该海域SST年代际变率出现明显增强，可能与全球变暖导致的海洋内部变率的变化有关。考虑到热带西南太平洋SST年代际变率同样在1890年也发生了一次转变，我们认为这些证据可能指示了整个热带太平洋内部变率在1890年以后发生了一次转变。
- 黄岩岛 /
- 珊瑚生长率 /
- SSTA /
- 小冰期 /
- 年代际变化
Abstract: The relationship between coral growth rate and sea surface temperature anomaly (SSTA) was used to reconstruct the SSTA in the central South China Sea Since 1780. Our reconstruction shows that SSTA over the period 1780-1890, which correspond to the latter part of Little Ice Age, was cold relatively, the average SSTA was -0.2℃, the coldest SSTA was -1℃ in 1837. After 1890, the SSTA increased most fast between 1971 to 1998, the highest SSTA was 2℃ in 1998, but there was a downward trend after 1998, which is basically synchronous with the change of land temperature in Northern Hemisphere. The spectral analysis shows a significant period of 26-34 a for the SSTA in the central of South China Sea, with the phase transitions correspond to the decadal shifts of the Pacific Decadal Oscillation. The wavelet analysis indicated that the interdecadal oscillation of the SSTA in the central South China Sea was not stable over the past 234 years. After entering the Current Warm Period, the interdecadal variability has enhanced distinctly, which may be related to the changes in the internal variability of the ocean associated with the global warming. Our result, together with the change in the decadal-scale SST variability of the tropical southwest Pacific in the 1890, suggested that the internal variability of the tropical Pacific has changed since 1890.
- Huangyan Island /
- coral growth rate /
- SSTA /
- Little Ice Age /
- interdecadal variability

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参考文献(55)

晏宏. 南海西沙群岛晚全新世高分辨率气候环境变化[D]. 合肥:中国科学技术大学, 2012. Yan Hong. High resolution climatic and environmental changes in Xisha Islands of South China Sea during the late Holocene[D]. Hefei:University of Science and Technology of China, 2012.

Trenberth K E, Hurrell J W. Decadal atmosphere-ocean variations in the Pacific[J]. Climate Dynamics, 1994, 9(6):303-319.

Liu Z. Dynamics of interdecadal climate variability:a historical perspective[J]. Journal of Climate, 2012, 25(6):1963-1995.

Balmaseda M A, Trenberth K E, Källén E. Distinctive climate signals in reanalysis of global ocean heat content[J]. Geophysical Research Letters, 2013, 40(9):1754-1759.

Kosaka Y, Xie S P. Recent global-warming hiatus tied to equatorial Pacific surface cooling[J]. Nature, 2013, 501(7467):403.

Meehl G A, Hu A, Arblaster J M, et al. Externally forced and internally generated decadal climate variability associated with the interdecadal Pacific oscillation[J]. Journal of Climate, 2013, 26(18):7298-7310.

Biondi F, Gershunov A, Cayan D R. North Pacific decadal climate variability since 1661[J]. Journal of Climate, 2001, 14(1):5-10.

D'arrigo R, Villalba R, Wiles G. Tree-ring estimates of Pacific decadal climate variability[J]. Climate Dynamics, 2001, 18(3/4):219-224.

Mann M E, Zhang Z, Rutherford S, et al. Global signatures and dynamical origins of the Little Ice Age and Medieval Climate Anomaly[J]. Science, 2009, 326(5957):1256-1260.

D'arrigo R, Wilson R, Liepert B, et al. On the ‘divergence problem’ in northern forests:a review of the tree-ring evidence and possible causes[J]. Global and Planetary Change, 2008, 60(3):289-305.

Yu K F, Zhao J X, Wei G J, et al. Mid-late Holocene monsoon climate retrieved from seasonal Sr/Ca and δ¹⁸O records of Porites lutea corals at Leizhou Peninsula, northern coast of South China Sea[J]. Global and Planetary Change, 2005, 47(2/4):301-316.

Yu K F. Coral reefs in the South China Sea:Their response to and records on past environmental changes[J]. Science China Earth Sciences, 2012, 55(8):1217-1229.

Linsley B K, Zhang P, Kaplan A, et al. Interdecadal-decadal climate variability from multicoral oxygen isotope records in the South Pacific Convergence Zone region since 1650 AD[J]. Paleoceanography, 2008, 23(2):PA2219.

Delong K L, Quinn T M, Taylor F W, et al. Sea surface temperature variability in the southwest tropical Pacific since AD 1649[J]. Nature Climate Change, 2012, 2(11):799-804.

Cole J E, Dunbar R B, Mcclanahan T R, et al. Tropical pacific forcing of decadal SST variability in the western indian ocean over the past two centuries[J]. Science, 2000, 287(5453):617-620.

李娟, 左军成, 李艳芳, 等. 南海海表温度的低频变化及影响因素[J]. 河海大学学报:自然科学版, 2011, 39(5):575-582. Li Juan, Zuo Juncheng, Li Yanfang, et al. Low-frequency variation and influence factors of sea surface temperature in South China Sea[J]. Journal of Hohai University:Natural Sciences, 2011, 39(5):575-582.

张秀芝, 裘越芳, 吴迅英. 近百年中国近海海温变化[J]. 气候与环境研究, 2005, 10(4):799-807. Zhang Xiuzhi, Qiu Yuefang, Wu Xunying. The long-term change for sea surface temperature in the last 100 years in the offshore sea of China[J]. Climatic and Environmental Research, 2005, 10(4):799-807.

林紫云, 余克服, 施祺, 等. 三沙市美济礁滨珊瑚记录的近百年海面温度变化[J]. 热带地理, 2016, 36(1):27-33. Lin Ziyun, Yu Kefu, Shi Qi, et al. Sea surface temperature variations during the last 100 years recorded in a Porites coral from the Mischief Reef of Sansha City[J]. Tropical Geography, 2016, 36(1):27-33.

Sun Y, Sun M, Wei G, et al. Strontium contents of a Porites coral from Xisha Island, South China Sea:A proxy for sea-surface temperature of the 20th century[J]. Paleoceanography, 2004, 19(2):1-10.

蔡榕硕, 张启龙, 齐庆华. 南海表层水温场的时空特征与长期变化趋势[J]. 台湾海峡, 2009, 28(4):559-568. Cai Rongshuo, Zhang Qilong, Qi Qinghua. Spatial and temporal oscillation and long-term variation in sea surface temperature field of the South China Sea[J]. Journal of Oceanography in Taiwan Strait, 2009, 28(4):559-568.

万道静. 南海海表盐度的分布特征[D]. 青岛:中国海洋大学, 2014. Wan Daojing. Distribution characteristics of the sea surface salinity of the South China Sea[D]. Qingdao:Ocean University of China, 2014.

Nie B F, Chen T G, Liang M T, et al. Relationship between coral growth rate and sea surface temperature in the northern part of South China Sea during the past 100 a[J]. Science in China Series D:Earth Sciences, 1997, 40(2):173-182.

Lough J M, Barnes D J. Environmental controls on growth of the massive coral Porites[J]. Journal of Experimental Marine Biology and Ecology, 2000, 245(2):225-243.

Saenger C, Cohen A L, Oppo D W, et al. Surface-temperature trends and variability in the low-latitude North Atlantic since 1552[J]. Nature Geoscience, 2009, 2(7):492-495.

Vásquez-Bedoya L F, Cohen A L, Oppo D W, et al. Corals record persistent multidecadal SST variability in the Atlantic Warm Pool since 1775 AD[J]. Paleoceanography, 2012, 27(3):PA3231.

聂宝符, 陈特固, 梁美桃,等. 近百年来南海北部珊瑚生长率与海面温度变化的关系[J]. 中国科学:D辑, 1996, 26(1):59-66. Nie Baofu, Chen Tegu, Liang Meitao, et al. Relationship between coral growth rate and sea surface temperature in the northern part of South China Sea during the past 100 a[J]. Science in China:Series D, 1996, 26(1):59-66.

黄博津, 余克服, 张会领, 等. 利用珊瑚生长率重建西沙海域罗马暖期中期海温变化[J]. 热带地理, 2013, 33(3):237-241. Huang Bojin, Yu Kefu, Zhang Huiling, et al. Sea surface temperature variations during the Middle Rome Warm Period as reconstructed by Porites coral growth rates in the Xisha Islands[J]. Tropical Geography, 2013, 33(3):237-241.

张会领, 余克服, 施祺, 等. 珊瑚生长率重建西沙海域中晚全新世海温变化[J]. 第四纪研究, 2014, 34(6):1296-1305. Zhang Huiling, Yu Kefu, Shi Qi, et al. Sea surface temperature variations during the Mid Late Holocene reconstructed by Porites coral growth rates in the Xisha Islands[J]. Quternary Sciences, 2014, 34(6):1296-1305.

苏瑞侠, 孙东怀. 南海北部滨珊瑚生长的影响因素[J]. 地理学报, 2003, 58(3):442-451. Su Ruixia, Sun Donghuai. The influencing factors of corals Porites in the northern part of the South China Sea[J]. Acta Geographica Sinica, 2003, 58(3):442-451.

施祺, 余克服, 陈天然, 等. 南海南部美济礁200余年滨珊瑚骨骼钙化率变化及其与大气CO₂和海水温度的响应关系[J]. 中国科学:地球科学, 2012, 42(1):71-82. Shi Qi, Yu Kefu, Chen Tianran, et al. Two centuries-long records of skeletal calcification in massive Porites colonies from Meiji Reef in the southern South China Sea and its responses to atmospheric CO₂ and seawater temperature[J]. Science China:Earth Sciences, 2012, 42(1):71-82.

黄金森. 南海黄岩岛的一些地质特征[J]. 海洋学报, 1980, 2(2):112-123. Huang Jinsen. Some geological features of the Huangyan Dao(Huangyan Island), South China Sea[J]. Haiyang Xuebao, 1980, 2(2):112-123.

Rayner N A, Parker D E, Horton E B, et al. Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century[J]. Journal of Geophysical Research Atmospheres, 2003, 108(D14):1063-1082.

Lough J M, Barnes D J. Several centuries of variation in skeletal extension, density and calcification in massive Porites colonies from the Great Barrier Reef:A proxy for seawater temperature and a background of variability against which to identify unnatural change[J]. Journal of Experimental Marine Biology and Ecology, 1997, 211(1):29-67.

聂宝符, 陈特固, 彭子成. 由造礁珊瑚重建南海西沙海区近220 a海面温度序列[J]. 科学通报, 1999, 44(17):1885-1889. Nie Baofu, Chen Tegu, Peng Zicheng. Sea surface temperature series in the Xisha sea area of the South China Sea by reef-building corals over the last 220 years[J]. Chinese Science Bulletin, 1999, 44(17):1885-1889.

施祺, 张叶春, 孙东怀. 海南岛三亚滨珊瑚生长率特征及其与环境因素的关系[J]. 海洋通报, 2002, 21(6):31-38. Shi Qi, Zhang Yechun, Sun Donghuai. Characteristics of growth rate of Porite coral from Sanya, Hainan Island and its relationship to environmental variables[J]. Marine Science Bulletin, 2002, 21(6):31-38.

江巧文, 曹志敏, 王道儒, 等. 琼东海域橙黄滨珊瑚骨骼生长特性及其主要影响因素[J]. 应用生态学报, 2016, 27(3):953-962. Jiang Qiaowen, Cao Zhimin, Wang Daoru, et al. Growth characteristics of Porites lutea skeleton in east sea area of Hainan Island, China and main affecting environmental factors[J]. Chinese Journal of Applied Ecology, 2016, 27(3):953-962.

Gorman M K, Quinn T M, Taylor F W, et al. A coral-based reconstruction of sea surface salinity at Sabine Bank, Vanuatu from 1842 to 2007 CE[J]. Paleoceanography, 2012, 27(3):PA3226.

Mann M E, Zhang Z, Hughes M K, et al. Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia[J]. The National Academy of Sciences of the USA, 2008, 105(36):13252-13257.

Hegerl G C, Crowley T J, Allen M, et al. Detection of human influence on a new, validated 1500-year temperature reconstruction[J]. Journal of Climate, 2007, 20(4):650-666.

Jones P D, Mann M E. Climate over past millennia[J]. Reviews of Geophysics, 2004, 42(2):RG2002.

Dong D P, Zhou W D, Yang Y, et al. On outflow passages in the South China Sea[J]. Advances in Atmospheric Sciences, 2010, 27(1):60-68.

Sagawa T, Kuwae M, Tsuruoka K, et al. Solar forcing of centennial-scale East Asian winter monsoon variability in the mid-to late Holocene[J]. Earth and Planetary Science Letters, 2014, 395:124-135.

Man W, Zhou T. Response of the East Asian summer monsoon to large volcanic eruptions during the last millennium[J]. Chinese Science Bulletin, 2014, 59(31):4123-4129.

Meehl G A, Arblaster J M, Fasullo J T, et al. Model-based evidence of deep-ocean heat uptake during surface-temperature hiatus periods[J]. Nature Climate Change, 2011, 1(7):360-364.

Lean J, Beer J, Bradley R S. Reconstruction of solar irradiance since 1610:Implications for climate cbange[J]. Geophysical Research Letters, 1995, 22(23):3195-3198.

Crowley T J, Unterman M B. Technical details concerning development of a 1200 yr proxy index for global volcanism[J]. Earth System Science Data, 2013, 5(1):187-197.

Macfarling Meure C, Etheridge D, Trudinger C, et al. Law dome CO₂, CH₄ and N₂O ice core records extended to 2000 years BP[J]. Geophysical Research Letters, 2006, 33(14):L14810.

Mantua N J, Hare S R, Zhang Y, et al. A Pacific interdecadal climate oscillation with impacts on salmon production[J]. Bulletin of the american Meteorological Society, 1997, 78(6):1069-1079.

刘羿, 彭子成, 程继满, 等. 海南岛东部海域滨珊瑚Sr/Ca比值温度计及其影响因素初探[J]. 第四纪研究, 2006, 26(3):470-476. Liu Yi, Peng Zicheng, Cheng Jiman, et al. The relationship between Sr/Ca values of Porites coral and sst values in eastern Hainan Island at the North of South China Sea and its influence factors[J]. Quaternary Sciences. 2006, 26(3):470-476.

Deng W, Wei G, Xie L, et al. Variations in the Pacific Decadal Oscillation since 1853 in a coral record from the northern South China Sea[J]. Journal of Geophysical Research:Oceans, 2013, 118(5):2358-2366.

Macdonald G M, Case R A. Variations in the Pacific Decadal Oscillation over the past millennium[J]. Geophysical Research Letters, 2005, 32(8):L08703.

D'arrigo R, Wilson R. On the Asian expression of the PDO[J]. International Journal of Climatology, 2006, 26(12):1607-1617.

Felis T, Suzuki A, Kuhnert H, et al. Pacific Decadal Oscillation documented in a coral record of North Pacific winter temperature since 1873[J]. Geophysical Research Letters, 2010, 37(14):L14605.

Shen C, Wang W C, Gong W, et al. A Pacific Decadal Oscillation record since 1470 AD reconstructed from proxy data of summer rainfall over eastern China[J]. Geophysical Research Letters, 2006, 33(3):L03702.

Minobe S. A 50-70 year climatic oscillation over the North Pacific and North America[J]. Geophysical Research Letters, 1997, 24(6):683-686.

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