收稿日期: 2006-01-09
修回日期: 2006-05-15
网络出版日期: 2006-07-15
基金资助
教育部重点科研项目“上海近海海洋水文气候环境变化过程—及对全球气候增暖响应的评估”(编号: 206051);上海市科委项目“上海区域海洋水文气候、环境的年季变化过程研究”(编号: 042512031);上海市浦江人才计划“上海海域海洋温盐过程与化学物质传输过程的研究”(编号: 05PJ14080)资助.
The New Progresses on Global Sea Level Change
Received date: 2006-01-09
Revised date: 2006-05-15
Online published: 2006-07-15
综述了近10年来海平面变化研究的主要成果,分析了影响海平面变化的主要因素,探讨了海平面变化研究中存在的一些问题。结果表明:①近10年全球平均海平面上升幅度大约为2.5~3.84 mm/a,热膨胀是引起海平面上升的主因;②海平面变化具有时空分布差异——西太平洋和东印度洋地区上升最快,其值高出全球平均值的10倍以上;大西洋与太平洋30~40°N地区季节变化最明显;③将海平面季节高值时段与北半球热带气旋出现时间进行对比,发现每年8~10月份,在20~50°N的西北太平洋与北大西洋沿岸地区出现海平面最高值与热带气旋相叠加的全球危险海岸带,该地带包括中国大陆东部、日本沿海地区、美国东部海岸带、墨西哥湾地区和加勒比海地区。
王芳 , , 吴涛 , 郑琰明 , 康建成 . 全球海平面变化研究新进展[J]. 地球科学进展, 2006 , 21(7) : 730 -737 . DOI: 10.11867/j.issn.1001-8166.2006.07.0730
The research of global sea level change of the last 10 years has been comprehensively reviewed and the main results of it have been obtained:(1) the global sea level rising ratios was around 2.5 mm/a to 3.84 mm/a, and the main contribution is from the thermal expansion of sea water; (2) there were some space differences for sea level rise, and the value in the West Pacific Ocean and the East Indian Ocean was especially more 10 times higher than the global average; (3) the seasonal fluctuation of sea level was obvious in areas of the Pacific Ocean and the Atlantic Ocean with north latitude 30-40 degree. When the season of the highest sea level was compared with the term of the typhoon and hurricane occurring annually, it could be found that there were global dangerous seacoasts, which were vulnerable by sea level rise, located in the regions of the Northwest Pacific Ocean and the North Atlantic Ocean with north latitude 20-50 degree during the seasons of Typhoon in August and October. The region includes coast areas as Chinese Mainland East Seacoast, Japanese Seacoast, American East Seacoast, Mexico Bay Seacoast and Caribbean Seacoast.
[1] Assessing impact and vulnerability[EB/OL]. http://www.unep.org/geo/yearbook/yb2004/07-2.htm, 2005-12-22.
[2] Wang Ying, ed. China Ocean Geography[M]. Beijing: Science Press,1996.[王颖主编.中国海洋地理[M].北京:科学出版社,1996.]
[3] Liu Zhongmin, Zhang Demin. Ocean domain unconventional safety intimidate and the present international connection influence[J]. Journal of Ocean University of China,2004,(4): 60-64. [刘中民,张德民.海洋领域的非传统安全威胁及其对当代国际关系的影响[J].中国海洋大学学报,2004,(4):60-64.]
[4] Fan Daidu, Li Congxian. Complexities of chinese coast in response to climate change[J]. Advances in Climate Change Research,2005,1(3):111-114. [范代读,李从先.中国沿海响应气候变化的复杂性[J].气候变化研究进展, 2005,1(3):111-114.]
[5] Webster P J, Holland G J, Curry J A, et al. Changes in Tropical Cyclone Number, Duration, and Intensity in a Warming Environment[J]. Science,2005,16(309): 844-846.
[6] Chinese Ocean Bureau. Chinese Ocean Disaster Report in 2004[R].2005.[国家海洋局.中国海洋灾害公报2004[R].2005.]
[7] Hurricane attack America[EB/OL].http://news.sina.com.cn/z/jfxjmg/index.shtml,2005-12-22.[飓风卡特里娜袭击美国[EB/OL].http://news.sina.com.cn/z/jfxjmg/index.shtml,2005-12-22.]
[8] Description of psmsl 'RLR' and 'metric' datasets[EB/OL]. http://www.pol.ac.uk/psmsl/data-info/psmsl.hel, 2005-12-22.
[9] The Global Sea Level Observing System (GLOSS)[EB/OL]. http://www.pol.ac.uk/psmsl/pr-ogrammes /gloss.info.html, 2005-12-22.
[10] Tide gauge estimates of global sea level rise[EB/OL]. http://sealevel.colorado.edu/tidegaug-es.html, 2005-12-22.
[11] Chambers D P, Ries J C, Shum C K, et al. On the use of tide gauges to determine altimeter drift[J]. Geophysical Research,1998,103(C6):12 885-12 890.
[12] Douglas B C. Sea level change in the era of the recording tide gauge[C]∥Douglas B C, Kearney M S, Leatherman S P. Sea Level Rise, History and Consequences.San Diego, California: Academic,2001: 37-64.
[13] Cazenave A, Dominh K, Ponchaut F, et al. Sea level changes from TOPEX/Poseid on altimetry and tide gauge, and vertical crustal motions from DORIS[J]. Geophy-sical Research Letters, 1999,26(14): 2 077-2 080.
[14] Chelton D B, Ries J C, Haines B J, et al, Satellite altimetry[C]∥Fu L L,Cazenave A. Satellite Altimetry and Earth Sciences. San Diego Calif: Academic,2001:1-131.
[15] Nerem R S, Hendricks B J, Minster J F, et al. Improved determination of global mean sea level variations using TOPEX/POSEIDON altimeter data[J]. Geophysical Research Letters,1997, 24(11):1 331-1 334.
[16] Cazenave A, Nerem R S. Present-day sea level change:Observation and causes[J]. Reviews of Geophysics, 2004,42:RG3001,1-20.
[17] Minster J-F, Brossier C, Rogel P. Variation of the mean sea level from TOPEX/ POSEIDON data[J]. Geophysical Research,1995,100(C12): 25 153-25 162.
[18] Cabanes C, Cazenave A, Provost C L. Sea level change from TOPEX-Poseidon altimetry for 1993-1999 and possible warming of the southern oceans[J]. Geophysical Research Letters,2001,28(1): 9-12.
[19] Cazenave A, Dominh K, Gennero M C, et al. Global mean sea level changes observed by TOPEX-Poseidon and ERS-1[J]. Physical Chemical Earth,1998,23(9/10):1 069-1 075.
[20] Ivica Vilibi. Global sea level rise? New techniques for the absolute sea level measurement[J]. Geofizika, 1997, 14:119-131.
[21] Andrey P, Vladinir P, Robert H B. Sea level rise in the Arctic Ocean[J]. Geophysical Research Letters, 2001, 28(11): 2 237-2 240.
[22] Chen J L, Wilson C R, Chambers D P, et al. Seasonal global water mass budget and mean sea level variations[J]. Geophysical Research Letters,1998,25(19):3 555-3 558.
[23] Cubasch U, Meehl G A, Boer G J, et al. Projections of future climate change[C]∥Houghton J T, et al. Climate Change 2001: The Scientific Basis, Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. New York :Cambridge Univorsity Press, 2001: 525-582.
[24] Church J, Gregory J M, Huybrechts P, et al. Changes in sea level[C]∥Houghton J T, et al. Climate Change 2001: The Scientific Basis, Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change.New York :Cambridge University Press, 2001: 639-693.
[25] Gill A E. Atmosphere-Ocean Dynamics[M]. San Diego,California: Academic,1982.
[26] Cabanes C, Cazenave A, Provost C L. Sea level rise during past 40 years determined from satellite and in situ observations[J]. Science,2001,294:840-842.
[27] Lombarb A, Cazenave A, Traon P Y L, et al. Contrubution of thermal expansion to present-day sea-level change revisited[J]. Global and Planetary Change,2005,47: 1-16.
[28] Antonov J I, Levitus S, Boyer T P. Steric sea level variations during 1957-1994: Importance of salinity[J]. Geophysical Research, 2002,107(12):8 013.
[29] Miller L, Douglas B C. Mass and volume contributions to 20th century global sea level rise[J]. Nature,2004,428: 406-409.
[30] Levitus S, Stephens C, Antonov J I, et al. Yearly and year-Season upper ocean temperature anomaly fields, 1948-1998, NOAA Atlas NESDIS 40, Natlina Oceanic and Atmospheric Administration, Silver Spring, Md. 2000[EB/OL]. http:// www.nodc.noaa.gov/OC5/ PDF/ATLAS/nesdis40.pdf,2005-12-22.
[31] Ishii M, Kimoto M, Kachi M. Historical ocean subsurface temperature analysis with error estimates[J]. Monthly Weather Review,2003,131:51-73.
[32] Jacobs S S, Giulivi C F, Mele P A. Freshening of the Ross Sea during the late 20th century[J]. Science, 2002,297:386-389.
[33] Dyurgerov. Glacier mass balance and regime[R]. Institute of Arctic and Alpine Research, University of Colorado, Boulder, 2002.
[34] Arendt A A, Echelmeyer K A, Harrison W D, et al. Rapid wastage of Alaska glaciers and their contribution to rising sea level[J]. Science, 2002,297:382-386.
[35] Meier M F, Dyurgerov M. How Alaska affects the world[J]. Science, 2002, 297:350-351.
[36] Rignot E, Rivera A, Casassa G. Contribution of the Patagonia ice fields of South America to sea level rise[J]. Science,2003,302: 434-437.
[37] Abdalati W, Krabill W, Frederick E, et al. Outlet glacier and margin elevation change: Near-coastal thinning of the Greenland ice sheet [J]. Geophysical Research, 2001,106(D24): 33 729-33 742.
[38] Davis C H, Kluever C A, Haines B J, et al. Improved elevation-change measure-ment of the southern Greenland ice sheet from satellite radar altimetry[J]. IEEE Transaction on Geoscience Remote Sensing,2000,38(4):1 367-1 378.
[39] Thomas R, Akins T, Csatho B, et al. Mass balance of the Greenland ice sheet at high elevations[J]. Science, 2000, 289: 426-428.
[40] Zwally H J, Abdalati W, Herring T, et al. Surface melt-induced acceleration of Greenland ice-sheet flow[J]. Science, 2002, 297: 218-222.
[41] Krabill W, Abdalati W, Frederick E, et al. Greenland ice sheet: High-elevation balance and peripheral thinning[J]. Science, 2000, 289: 428-430.
[42] Rignot E, Thomas R. Mass balance of polar ice sheets[J]. Science,2002,297: 1 502-1 506.
[43] Gille S T. Warming of the Southern Ocean since the 1950s[J]. Science, 2002, 295: 1 275-1 277.
[44] Mitrovica J X, Tamisiea M E, Davis J L, et al. Recent mass balance of polar ice sheets inferred from patterns of global sea level change[J]. Nature,2001,409:1 026-1 029.
[45] Davis C H, Li Y H, McConnell J R, et al. Snowfall-driven growth in east Antarctic ice sheet mitigates recent sea-level rise[J]. Science,2005,308:1 898-1 901.
[46] Gornitz V, Rosenzweig C, Hillel D. Effects of anthropogenic intervention in the land hydrological cycles on global sea level rise[J]. Global Planet Change,1997,14:97-116.
[47] Mitrovica J X, Forte A. A new inference of mantle viscosity based upon joint inversion of convection and glacial isostatic adjustment data[J]. Earth and Planetary Science Letter,2004,225:177-189.
[48] Peltier W R, Jiang X H. Glacial isostatic adjustment and Earth rotation: Refined constraints on the viscosity of the deepest mantle[J]. Geophysical Research,1996, 101(B2):3 269-3 290.
[49] Richards M A, Bunge H P, Ricard Y, et al. Polar wandering in mantle convection models[J]. Geophysical Research Letters,1999, 26(12): 1 777-1 780.
[50] Mitrovica J X, Peltier W R. Pleistocene deglaciation and the global gravity field [J]. Geophysical Research,1989, 94(B10): 13 651-13 671.
[51] Vaughan D G. How does the Antarctic ice sheet affect sea level rise?[J]. Science,2005,308(5 730):1 877-1 878.
[52] The First Clic International Science Conference[EB/OL].http://www.cma.gov.cn/netcenter_news / qhbh /t20050411_67656.phtml,2005-12-22.
[53] International development trend and foreground analysis[EB/OL]. http://center.shao.ac.cn/shcar/fzdt.htm, 2005-12-22.
[54] Wahr J,Wingham D,Bentley C. A method of combining ICESAT and GRACE satellite data to constrain Antarctic mass balance[J]. Geophysical Research,2000,105(B7): 16 279-16 294.
[55] Cui Shuhong, Xie Zhiren, Zhong Hexiang, et al. The prmary researches that T/P sea height data is used for revised ground rise or fall at the tide gauge station[J]. Adcances in Earth Secience,2005,20(6):643-648.[崔树红,谢志仁,钟鹤翔,等.利用T/P海面高度数据校验验潮站地面升降的初步研究[J]. 地球科学进展,2005,20(6):643-648.]
[56] Liu Jinfang, Hao Peizhang, Yu Mugeng, et al. Feature and varied rule of typhoon storm surge along the coast of south east China sea[J]. Journal of Ocean Forecasts,2002,19(1):81-88.[刘金芳,赫培章,俞慕耕,等.东南沿海台风风暴潮特点[J].海洋预报,2002,19(1):81-88.]
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