环礁潟湖沉积物重建南沙群岛小冰期以来的热带气旋活动

doi:10.11978/2022016

热带海洋学报 ›› 2022, Vol. 41 ›› Issue (6): 171-182.doi: 10.11978/2022016CSTR: 32234.14.2022016

环礁潟湖沉积物重建南沙群岛小冰期以来的热带气旋活动

杨红强¹^,²^,³(), 谭飞¹^,²^,⁴, 徐辉龙¹^,², 张喜洋¹^,², 施祺¹^,², 陶士臣¹^,²

1.中国科学院边缘海与大洋地质重点实验室, 中国科学院南海海洋研究所, 中国科学院南海生态环境工程创新研究院, 广东广州 510301
2.南方海洋科学与工程广东省实验室(广州), 广东广州 511458
3.中国科学院南沙海洋生态环境实验站, 海南三沙 573199
4.中国科学院大学, 北京 100049

收稿日期:2022-01-27 修回日期:2022-04-14 出版日期:2022-11-10 发布日期:2022-04-18
通讯作者: 杨红强
作者简介:杨红强(1980—), 男, 河南省平顶山市人, 博士, 副研究员, 主要从事珊瑚礁现代过程和全球变化记录研究。email:hqyang@scsio.ac.cn
基金资助:
南方海洋科学与工程广东省实验室(广州)人才团队引进重大专项(GML2019ZD0206);中国科学院南海生态环境工程创新研究院自主部署项目(ISEE2018PY01);中国科学院战略性先导科技专项(A类)(XDA13010103)

Reconstruction of the tropical cyclones activity in the Nansha Islands since the Little Ice Age from the atoll lagoon sediments

YANG Hongqiang¹^,²^,³(), TAN Fei¹^,²^,⁴, XU Huilong¹^,², ZHANG Xiyang¹^,², SHI Qi¹^,², TAO Shichen¹^,²

1. Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China
2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
3. Nansha Marine Ecological and Environmental Research Station, Chinese Academy of Sciences, Sansha 573199, China
4. University of Chinese Academy of Sciences, Beijing 100049, China

Received:2022-01-27 Revised:2022-04-14 Online:2022-11-10 Published:2022-04-18
Contact: YANG Hongqiang
Supported by:
Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0206);Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences(ISEE2018PY01);Strategic Priority Research Program of the Chinese Academy of Sciences(XDA13010103)

摘要/Abstract

摘要：

热带气旋活动以及由此产生的风暴潮和强降雨对南海及周边沿海地区社会经济构成巨大威胁。对器测记录之前全新世热带气旋的研究有助于准确预测全球变暖背景下热带气旋活动的变化趋势。本文利用南沙群岛安乐礁潟湖沉积物重建了小冰期以来准年分辨率的热带气旋活动, 共识别28个风暴事件层。研究表明, 小冰期以来, 南沙群岛安乐礁热带气旋活动在年代际到百年尺度上频繁变化, 发育两个主要的风暴活跃期。在小冰期早期(AD 1471—1620)经历了最为强烈的风暴活跃期, 另一个风暴活跃期位于现代暖期的AD 1930—1960, 风暴活动虽有所加强, 但明显低于小冰期早期。与同期永暑礁重建结果的对比表明, 热带气旋活动存在明显的时空差异性, 更多来自相近区域的高分辨率风暴记录可有效降低古风暴活动重建的不确定性, 提高重建记录的准确度。

关键词: 热带气旋, 小冰期, 潟湖沉积, 古风暴, 南沙群岛, 南海

Abstract:

Tropical cyclones (TCs) and the resultant storm surges and heavy rainfall have posed huge socio-economic threats to the coastal areas of the South China Sea (SCS) and its surrounding areas. Holocene TCs studies before instrumental record help to accurately predict trends in TCs activity in the context of global warming. Here, we presented a new sub-annually resolved paleostorm record from the Anle reef lagoon sediments of the Nansha Islands in the southern SCS since the relative cold Little Ice Age (LIA) and a total of 28 storm event layers were identified. The new reconstruction indicates that the site has witnessed frequent TCs variations on a decadal to centennial-scale since the LIA, and two main storm active periods have been developed. The most intense storm activity period occurred in the early LIA (AD 1471~1620), and the other relatively active period was witnessed in the Current Warm Period (CWP) of AD 1930~1960. Although the storm activity in CWP was strengthened, it was significantly lower than that in the early LIA. Regional comparison with the storm reconstruction record of the Yongshu Reef during the same period reveals distinct spatio-temporal heterogeneity in the southern SCS. More high-resolution storm records from similar or adjacent regions could effectively reduce the uncertainty of storm reconstructions and increase the accuracy of reconstructed records.

Key words: tropical cyclones, Little Ice Age, lagoon sediments, paleostorm, Nansha Islands, South China Sea

中图分类号:

P722.7

杨红强, 谭飞, 徐辉龙, 张喜洋, 施祺, 陶士臣. 环礁潟湖沉积物重建南沙群岛小冰期以来的热带气旋活动[J]. 热带海洋学报, 2022, 41(6): 171-182.

YANG Hongqiang, TAN Fei, XU Huilong, ZHANG Xiyang, SHI Qi, TAO Shichen. Reconstruction of the tropical cyclones activity in the Nansha Islands since the Little Ice Age from the atoll lagoon sediments[J]. Journal of Tropical Oceanography, 2022, 41(6): 171-182.

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参考文献 43

[1]	高抒, 贾建军, 杨阳, 等, 2019. 陆架海岸台风沉积记录及信息提取[J]. 海洋学报, 41(10): 141-160.
	GAO SHU, JIA JIANJUN, et al, 2019. Obtaining typhoon information from sedimentary records in coastal-shelf waters[J]. Haiyang Xuebao, 41(10): 141-160. (in Chinese with English abstract)
[2]	廖菲, 李文婷, 张子然, 等, 2019. 1949-2017年南海海域热带气旋强度和路径快速变化统计特征[J]. 海洋学报, 41(9): 126-135.
	LIAO FEI, LI WENTING, ZHANG ZIRAN, et al, 2019. Analysis of rapid changes of tropical cyclones over the South China Sea for 1949-2017[J]. Haiyang Xuebao, 41(9): 126-135. (in Chinese with English abstract)
[3]	陶丽, 张艺帆, 王学兵, 2020. 南海与西北太平洋地区夏季热带气旋潜在生成指数的改进[J]. 大气科学学报, 43(4): 603-616.
	TAO LI, ZHANG YIFAN, WANG XUEBING, 2020. Improvement of genesis potential index for western North Pacific tropical cyclones[J]. Transactions of Atmospheric Sciences, 43(4): 603-616. (in Chinese with English abstract)
[4]	徐笑梅, 高抒, 周亮, 等, 2019. 海南岛东北部海岸极端波浪事件沉积记录[J]. 海洋学报, 41(6): 48-63.
	XU XIAOMEI, GAO SHU, ZHOU LIANG, et al, 2019. Sedimentary records of extreme wave events on the northeastern Hainan Island coast, southern China[J]. Haiyang Xuebao, 41(6): 48-63. (in Chinese with English abstract)
[5]	张敏, 罗军, 胡金磊, 等, 2019. 雷州市沿海风暴潮淹没危险性评估[J]. 热带海洋学报, 38(2): 1-12. doi: 10.11978/2018067
	ZHANG MIN, LUO JUN, HU JINLEI, et al, 2019. Inundation risk assessment of storm surge along Lei Zhou coastal areas[J]. Journal of Tropical Oceanography, 38(2): 1-12. (in Chinese with English abstract) doi: 10.11978/2018067
[6]	周亮, 高抒, 杨阳, 等, 2015. 海南岛东南部海湾350年古风暴事件沉积与历史文献记录对比[J]. 海洋学报, 37(9): 84-94.
	ZHOU LIANG, GAO SHU, et al, 2015. Comparison of paleostorm events between sedimentary and historical archives: A 350 year record from southeastern Hainan Island coastal embayments[J]. Haiyang Xuebao, 37(9): 84-94. (in Chinese with English abstract)
[7]	BACMEISTER J T, REED K A, HANNAY C, et al, 2018. Projected changes in tropical cyclone activity under future warming scenarios using a high-resolution climate model[J]. Climatic Change, 146(3-4): 547-560. doi: 10.1007/s10584-016-1750-x
[8]	BLAAUW M, CHRISTEN J A, 2011. Flexible paleoclimate age-depth models using an autoregressive gamma process[J]. Bayesian Analysis, 6(3): 457-474. doi: 10.1214/ba/1339616472
[9]	BRAITHWAITE C J R, 1973. Settling behaviour related to sieve analysis of skeletal sands[J]. Sedimentology, 20(2): 251-262. doi: 10.1111/j.1365-3091.1973.tb02048.x
[10]	BRAMANTE J F, FORD M R, KENCH P S, et al, 2020. Increased typhoon activity in the Pacific deep tropics driven by Little Ice Age circulation changes[J]. Nature Geoscience, 13(12): 806-811. doi: 10.1038/s41561-020-00656-2
[11]	CHEN H-F, LIU Y-C, CHIANG C-W, et al, 2019a. China's historical record when searching for tropical cyclones corresponding to Intertropical Convergence Zone (ITCZ) shifts over the past 2 kyr[J]. Climate of the Past, 15(1): 279-289. doi: 10.5194/cp-15-279-2019
[12]	CHEN TIANRAN, ROFF G, FENG YUEXING, et al, 2019b. Tropical sand cays as natural Paleocyclone archives[J]. Geophysical Research Letters, 46(16): 9796-9803. doi: 10.1029/2019GL084274
[13]	CHENG H, EDWARDS R L, HOFF J, et al, 2000. The half-lives of uranium-234 and thorium-230[J]. Chemical Geology, 169(1-2): 17-33. doi: 10.1016/S0009-2541(99)00157-6
[14]	CLARK T R, ROFF G, ZHAO JIANXIN, et al, 2014. Testing the precision and accuracy of the U-Th chronometer for dating coral mortality events in the last 100 years[J]. Quaternary Geochronology, 23: 35-45. doi: 10.1016/j.quageo.2014.05.002
[15]	CONTRERAS-ROSALES L A, JENNERJAHN T, STEINKE S, et al, 2019. Holocene changes in biome size and tropical cyclone activity around the Northern South China Sea[J]. Quaternary Science Reviews, 215: 45-63. doi: 10.1016/j.quascirev.2019.05.004
[16]	DIETRICH W E, 1982. Settling velocity of natural particles[J]. Water Resources Research, 18(6): 1615-1626. doi: 10.1029/WR018i006p01615
[17]	DONNELLY J P, HAWKES A D, LANE P, et al, 2015. Climate forcing of unprecedented intense-hurricane activity in the last 2000 years[J]. Earth’s Future, 3(2): 49-65. doi: 10.1002/2014EF000274
[18]	ISHIZAWA T, GOTO K, YOKOYAMA Y, et al, 2020. Dating tsunami deposits: Present knowledge and challenges[J]. Earth-Science Reviews, 200: 102971. doi: 10.1016/j.earscirev.2019.102971
[19]	KENCH P S, MCLEAN R F, 1996. Hydraulic characteristics of bioclastic deposits: New possibilities for environmental interpretation using settling velocity fractions[J]. Sedimentology, 43(3): 561-570. doi: 10.1046/j.1365-3091.1996.d01-23.x
[20]	KENCH P S, BRANDER R W, 2006. Response of reef island shorelines to seasonal climate oscillations: South Maalhosmadulu atoll, Maldives[J]. Journal of Geophysical Research: Earth Surface, 111(F1): F01001.
[21]	KLOSTERMANN L, GISCHLER E, STORZ D, et al, 2014. Sedimentary record of late Holocene event beds in a mid-ocean atoll lagoon, Maldives, Indian Ocean: Potential for deposition by tsunamis[J]. Marine Geology, 348: 37-43. doi: 10.1016/j.margeo.2013.11.014
[22]	KNUTSON T, CAMARGO S J, CHAN J C L, et al, 2020. Tropical cyclones and climate change assessment: Part II: Projected response to anthropogenic warming[J]. Bulletin of the American Meteorological Society, 101(3): E303-E322. doi: 10.1175/BAMS-D-18-0194.1
[23]	KNUTSON T R, SIRUTIS J J, ZHAO Ming, et al, 2015. Global projections of intense tropical cyclone activity for the late twenty-first century from dynamical downscaling of CMIP5/RCP4.5 scenarios[J]. Journal of Climate, 28(18): 7203-7224. doi: 10.1175/JCLI-D-15-0129.1
[24]	LANDSEA C W, HARPER B A, HOARAU K, et al, 2006. Can we detect trends in extreme tropical cyclones?[J]. Science, 313(5786): 452-454. doi: 10.1126/science.1128448
[25]	LANE P, DONNELLY J P, WOODRUFF J D, et al, 2011. A decadally-resolved paleohurricane record archived in the late Holocene sediments of a Florida sinkhole[J]. Marine Geology, 287(1-4): 14-30. doi: 10.1016/j.margeo.2011.07.001
[26]	LIN NING, LANE P, EMANUEL K A, et al, 2014. Heightened hurricane surge risk in northwest Florida revealed from climatological-hydrodynamic modeling and paleorecord reconstruction[J]. Journal of Geophysical Research: Atmospheres, 119(14): 8606-8623. doi: 10.1002/2014JD021584
[27]	LIU ENTAO, ZHAO JIANXIN, FENG YUEXING, et al, 2016. U-Th age distribution of coral fragments from multiple rubble ridges within the Frankland Islands, Great Barrier Reef: implications for past storminess history[J]. Quaternary Science Reviews, 143: 51-68. doi: 10.1016/j.quascirev.2016.05.006
[28]	LIU K B, SHEN CAIMING, LOUIE K S, 2001. A 1,000-year history of typhoon landfalls in Guangdong, southern China, reconstructed from Chinese historical documentary records[J]. Annals of the Association of American Geographers, 91(3): 453-464. doi: 10.1111/0004-5608.00253
[29]	MAIKLEM W R, 1968. Some hydraulic properties of bioclastic carbonate grains[J]. Sedimentology, 10(2): 101-109. doi: 10.1111/j.1365-3091.1968.tb01102.x
[30]	MEI WEI, XIE SHANGPING, PRIMEAU F, et al, 2015. Northwestern pacific typhoon intensity controlled by changes in ocean temperatures[J]. Science Advances, 1(4): e1500014. doi: 10.1126/sciadv.1500014
[31]	PEDUZZI P, CHATENOUX B, DAO H, et al, 2012. Global trends in tropical cyclone risk[J]. Nature Climate Change, 2(4): 289-294. doi: 10.1038/nclimate1410
[32]	RODYSILL J R, DONNELLY J P, SULLIVAN R, et al, 2020. Historically unprecedented Northern Gulf of Mexico hurricane activity from 650 to 1250 CE[J]. Scientific Reports, 10(1): 19092. doi: 10.1038/s41598-020-75874-0 pmid: 33154412
[33]	SORIA J L A, SWITZER A D, VILLANOY C L, et al, 2016. Repeat storm surge disasters of typhoon Haiyan and its 1897 predecessor in the Philippines[J]. Bulletin of the American Meteorological Society, 97(1): 31-48. doi: 10.1175/BAMS-D-14-00245.1
[34]	SUN LI, BI SHUOBEN, CHEN CHANGCHUN, et al, 2020. Typhoon frequency sequence reconstruction and characteristics analysis in the Southeast coastal area over China during the Ming and Qing dynasties[J]. Natural Hazards, 100(3): 1105-1116. doi: 10.1007/s11069-019-03851-6
[35]	TOOMEY M R, DONNELLY J P, WOODRUFF J D, 2013. Reconstructing mid-late Holocene cyclone variability in the Central Pacific using sedimentary records from Tahaa, French Polynesia[J]. Quaternary Science Reviews, 77: 181-189. doi: 10.1016/j.quascirev.2013.07.019
[36]	WALLACE E J, DONNELLY J P, HENGSTUM P J, et al, 2019. Intense Hurricane activity over the past 1500 years at South Andros Island, the Bahamas[J]. Paleoceanography and Paleoclimatology, 34(11): 1761-1783. doi: 10.1029/2019PA003665
[37]	WALLACE E J, COATS S, EMANUEL K, et al, 2021a. Centennial-scale shifts in storm frequency captured in paleohurricane records from the Bahamas arise predominantly from random variability[J]. Geophysical Research Letters, 48(1): e2020GL091145.
[38]	WALLACE E J, DONNELLY J P, VAN HENGSTUM P J, et al, 2021b. 1,050 years of hurricane strikes on long island in the Bahamas[J]. Paleoceanography and Paleoclimatology, 36(3): e2020PA004156.
[39]	WINKLER T S, VAN HENGSTUM P J, DONNELLY J P, et al, 2020. Revising evidence of hurricane strikes on Abaco Island (The Bahamas) over the last 700 years[J]. Scientific Reports, 10(1): 16556. doi: 10.1038/s41598-020-73132-x
[40]	YANG HONGQIANG, YU KEFU, ZHAO MEIXIA, et al, 2015. Impact on the coral reefs at Yongle Atoll, Xisha Islands, South China Sea from a strong typhoon direct sweep: Wutip, September 2013[J]. Journal of Asian Earth Sciences, 114: 457-466. doi: 10.1016/j.jseaes.2015.04.009
[41]	YU KEFU, ZHAO JIANXIN, SHI QI, et al, 2009. Reconstruction of storm/tsunami records over the last 4000 years using transported coral blocks and lagoon sediments in the southern South China Sea[J]. Quaternary International, 195(1-2): 128-137. doi: 10.1016/j.quaint.2008.05.004
[42]	YUE YUANFU, YU KEFU, TAO SHICHEN, et al, 2019. 3500-year western Pacific storm record warns of additional storm activity in a warming warm pool[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 521: 57-71. doi: 10.1016/j.palaeo.2019.02.009
[43]	ZUKI Z M, LUPO A R, 2008. Interannual variability of tropical cyclone activity in the southern South China Sea[J]. Journal of Geophysical Research: Atmosphere, 113(D6): D06106.

珊瑚礁区	半径范围	热带风暴及以上级别热带气旋	每百年频率	≥cat 1级别热带气旋	每百年频率	≥cat 2级别热带气旋	每百年频率	≥cat 3级别热带气旋	每百年频率
安乐礁	r<300km	75.0	100.0	17.0	22.7	9.0	12.0	3.0	4.0
	r=115km	16.0	21.3	5.0	6.7	3.0	4.0	1.0	1.3
	r=60km	10.0	13.3	2.0	2.7	1.0	1.3	1.0	1.3
永暑礁	r<300km	67.0	89.3	15.0	20.0	8.0	10.7	1.0	1.3
	r=115km	18.0	24.0	6.0	8.0	2.0	2.7	1.0	1.3
	r=60km	6.0	8.0	2.0	2.7	1.0	1.3	1.0	1.3

环礁潟湖沉积物重建南沙群岛小冰期以来的热带气旋活动

Reconstruction of the tropical cyclones activity in the Nansha Islands since the Little Ice Age from the atoll lagoon sediments

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