海洋二氧化碳的研究进展

doi:10.11867/j.issn.1001-8166.2000.05.0559

地球科学进展 ›› 2000, Vol. 15 ›› Issue (5): 559 -564. doi: 10.11867/j.issn.1001-8166.2000.05.0559

海洋二氧化碳的研究进展

张远辉^①,王伟强^①,陈立奇^②

①国家海洋局第三海洋研究所,福建厦门 361005;②国家海洋局极地考察办公室,北京 100860

收稿日期:1999-10-13 修回日期:2000-02-28 出版日期:2000-10-01
通讯作者: 张远辉(1962-),男,福建惠安人,副研究员,主要从事海洋碳化学研究
基金资助:
国家自然科学基金重点项目“南大洋海冰区碳循环的研究”(编号:49836001)和福建省自然科学基金项目“厦门海域二氧化碳通量及循环研究”(编号:D96009)联合资助。

ADVANCES IN STUDIES OF OCEANIC CARBON DIOXIDE

ZHANG Yuan-hui ^①, WANG Wei-qiang ^①, CHEN Li-qi ^②

①Third Institute of Oceanography,SOA,Xiamen 361005,China;②Chinese Arctic and Antarctic Administration,SOA,Beijing 100860,China

Received:1999-10-13 Revised:2000-02-28 Online:2000-10-01 Published:2000-10-01

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海洋是一个巨大的碳库,具有潜在的缓冲大气CO₂增加的能力,研究CO₂在海洋中的转移和归宿,对于预测未来大气CO₂含量乃至全球气候变化具有重要意义。综述了海洋CO₂的研究现状,着重介绍海洋CO₂的源与汇、海—气CO₂通量的估算以及海洋环流、生物泵和海洋生态在海洋碳循环中的作用,并对该研究领域的发展趋势进行了总结。

关键词: 海洋CO₂, 海—气通量, 生物泵, 海洋环流, 海洋生态系统

The oceans are a huge reservoir for CO₂,containing 50 times more than the atmosphere and 20 times more than the biosphere,furthermore,they play an important role in regulating the levels of atmospheric CO₂,and hence global climate.The CO₂ between the oceans and the atmosphere is out of equilibrium ,the equatorial Pacific and Atlantic oceans are supersaturated with CO₂and hence are strong CO₂ source areas,on the other hand,the Southern and the North Atlantic oceans are strong sinks of atmospheric CO₂.The oceans have taken up large amounts of anthropogenic CO₂,models of global carbon cycle yield a mean oceanic CO₂ uptake of 2.0 Gt C/a.The oceans' capacity to take up CO₂ depends laregely on the effect of the biological pump and the dynamics of ocean circulation.Future concentration of atmospheric CO₂ is hard to predict because of our incomplete understanding of how the oceans would respond to the global warming.To improve our ability to estimate future CO₂ concentration,intense further research on oceanic CO₂is necessary.

Key words: Oceanic CO2, Air-sea flux, Biological pump, Ocean circulation, Marine ecosystem.

中图分类号:

P734.4+5

[1] Wong C S. Marine carbon research[A].In:Page J S,Bellegay R D,eds. Annual Review of Activities[C]. Sidney:Institute of Ocean Sciences, 1983. 48～49.
[2] Manabe S, Tang W, Fu L L. Century-scale effects of increased atmospheric CO₂on the ocean-atmosphere system[J].Nature,1993,364:215～218.
[3] 詹滨秋,赵永平.二氧化碳,海洋与气候[J].海洋与湖沼,1989,20(1):92～98.
[4] Chen C T. Rates of calcium carbonate dissolution and organic carbon dioxide decomposition in the North Pacific Ocean[J].J Oceanogr,1990,46:201～210.
[5] 赖利J P,斯基罗主编.化学海洋学(第二卷)[M].崔清晨,钱佐国,唐思齐译.北京:海洋出版社,1974.1～211.
[6] Tsunogai S, Yamahata H, Kudo S. Calcium in the Pacific Ocean[J]. Deep-Sea Research,1973,20:717～726.
[7] Siegenthaler U, Sarmiento J L. Atmospheric carbon dioxide and the ocean[J]. Nature,1993,365:119～125.
[8] Keeling C D. Carbon dioxide in surface ocean water[J]. J Geophys Res, 1968,73:4 543～4 553.
[9] Takahashi T, Goddard S, Sutherland D W. Seasonal and geo-graphic variability of carbon dioxide sink/source in the oceanic areas[J]. J Geophys Res,1986,91:10 517～10 527.
[10] Tans P P, Fung I Y, Takahashi T. Observational constraints on the global atmospheric carbon dioxide budget[J].Science,1990,247:1 431～1 438.
[11] Tans P P, Conway T J, Nakazawa T. Latitudinal distribution of the sources and sinks of atmospheric carbon dioxide derived from surface observations and an atmospheric transport model[J]. J Geophys Res,1989,94:5 151～5 173.
[12] Takahashi T. The carbon dioxide puzzle[J]. Oceanus,1989,32(2):22～29.
[13] Elliot W P, Angell J K. On the relation between atmospheric CO₂ and equatorial sea-surface temperature[J]. Tellus,1987,39B:171～183.
[14] Bacastow R, Adams J A, Keeling C D. Response of atmospheric carbon dioxide to the weak 1975 El Niño[J]. Science,1980,210:66～68.
[15] Sarmiento J L. Atmospheric CO₂stalled[J]. Nature,1993,365:697～698.
[16] Wong C S, Chan Y H, Page G E. Change in equatorial CO₂ flux and new production estimated from CO₂and nutrient levels in Pacific surface waters during the 1986/87 El Nino[J].Tellus,1993,43B:64～79.
[17] Feely R A, Wanninkohof C C, Cosca P P. CO₂distributionin the equatorial Pacific during 1991～1992 ENSO event[J].Deep-Sea Research,1995,42:365～386.
[18] Mccarrthy J L, Brewer P G,Feldman G. Global ocean flux[J]. Oceanus,1986,29(4):16～26.
[19] Murphy P P, Feely R A, Gammon R H. Assessment of the air-sea exchange of CO₂in the South Pacific during austral autumn[J]. J Geophys Res,1991,96:20 455～20 465.
[20] Takahashi T, Olafsson J, Broecker W S. Seasonal variability of the carbon-nutrient chemistry in the ocean areas west and north of Iceland[J].J Mar Res,1985,9:20～36.
[21] Feely R A, Sabine C L, Key R M. Estimating the anthropogenic carbon dioxide sink in the Pacific ocean[J]. US JGOFS News,1999,9(4):1～4.
[22] Sarmiento J L,Orr J C. A perturbation simulation of CO₂ uptake in an ocean general circulation model[J]. J Geophys Res,1992,97:3 621～3 645.
[23] Bacastow R, Maier R E. Ocean-circulation model of the carbon cycle[J]. Climate Dynamics,1990,4:95～125.
[24] Frankgnoule M. Field measurement of air-sea CO₂exchange[J]. Limnol Oceanogr, 1988,33(2):313～322.
[25] Liss P S , Merlivat L. Air-sea gas exchange rates: introduction and synthesis[A]. In: Buatmenard P,ed.The Role of Air-sea Exchange in Geochemical Cycling [C]. Dordrecht:Reidel Pub,1986.113～127.
[26] Wanninkhof R.Relationship between wind speed and gas exchange over the ocean[J].J Geophys Res,1992,97:7 373～7 382.
[27] Peng T H, Takahashi T, Broecker W S. Seasonal variability of carbon dioxide, nutrients and oxygen in the northern North Atlantic surface water: Observations and a model[J].Tellus,1987,39B:439～458.
[28] Quay P D, Tilbrook B, Wong C S. Oceanic uptake of fossil fuel CO₂: Carbon-13 evidence[J]. Nature,1992,256:74～79.
[29] 焦秀玲,詹滨秋.大气和海洋δ¹³C研究的进展及意义[J].海洋科学,1996,103(1):30～32.
[30] 王荣.海洋生物泵与全球变化[J].海洋科学,1992,99(1):18～21.
[31] Berger W H, Fischer, Lai C. Primary production and organic carbon flux in the world ocean[J].Deep-Sea research,1987,34:227～244.
[32] Wong C S. The relative efficiency of air-sea processes and the biological pump in sequestering anthropogenic CO₂into ocean storage[A].In:Tsunogai S S,Watanabe J,eds. Global Carbon Cycle[C].Tsukuba:Hokkaido University,1995.210.
[33] Reiner S. Modeling the nutrient and carbon cycles of North Atlantic. 2.New production, particle, fluxes, CO₂gas exchange[J].J Gopherys Res,1989,94:1 2781～1 2794.
[34] Sarmiento J L, Toggweiler J R. A new model for the role oceans in determining atmosphericp(CO₂)[J]. Nature,1984,306:624～626.
[35] Martin J H, Gordon R M, Fitzuater S E. Iron in Antarctic water[J]. Nature,1990,345:156～158.
[36] Sarmiento J L, Orr J C. Three-dimensional simulations of the impact of Southern Ocean nutrient depletion on atmospheric CO₂and ocean chemistry [J]. Limnol Oceanogr,1991,36(8):1 928～1 950.

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