收稿日期: 2001-06-26
修回日期: 2001-07-23
网络出版日期: 2001-10-01
基金资助
国家重点基础研究发展规划项目“黄、东海生态系统动力学和生物资源可持续利用”(编号：G19990437)；国家自然科学基金项目“浅海沙波运动的卫星遥感分析”(编号： 49976011)资助.王启为中科院访问学者，得到中国科学院知识创新工程重要方向项目“西太平洋暖池动力过程与海气相互作用”（编号：KZCX2-205）资助.
SOME IMPORTANT RESEARCH TOPICS FOR CHINA IN OCEAN SCIENCES IN THE EARLY 21st CENTURY
Received date: 2001-06-26
Revised date: 2001-07-23
Online published: 2001-10-01
苏纪兰，李炎，王启 . 我国21世纪初海洋科学研究中的若干重要问题[J]. 地球科学进展, 2001 , 16(5) : 658 -663 . DOI: 10.11867/j.issn.1001-8166.2001.05.0658
Ocean sciences progressed rapidly in the 20th century, especially during its second half. At the same time, the important role of the oceans in the sustainable development of human society has also been recognized. It is suggested that China should pay special attention to two areas in ocean sciences research in the early 21st century. One is the role of the oceans in the climate variability at the seasonal, interannual and interdecadal time scales. The other is the response of the coastal systems and marine ecosystems to both natural environment variability and anthropogenic activities, including the global change. In this paper we discussed the related research topics for China in the early 21st century, after reviewing advances made worldwide in both ocean circulation and marine productivity in the 20th century.
[1] Broecker W S. The biggest chill[J]. Natural History Magazine, 1987, 97:74-82.
[2] Dugdale R C, Goering J J. Uptake of new and regenerated froms of nitrogen in primary production[J]. Limnal Oceanogr, 1967, 12: 196-206.
[3] Fuhrman J A, Ammerman J W, Azam F. Bacterioplanton in the coastal euphotic zone: Distribution, activity and possible relationships with phytoplankton [J]. Mar Biol, 1980, 60:201-207.
[4] KoblentzMishke O J, Volkovinsky V V, Kabanova J G. Plankton primary production of the world ocean[A]. In: Wooster W S, ed. Scientific Exploration of the South Pacific[C]. National Academy of Sciences, Washington D C, 1970. 183-193.
[5] Luyten J R, Pedlosky J, Stommel H. Upstream effects of the Gulf Stream on the structure of the mid-ocean thermocline [J]. Progress of Oceanography, 1985, 14:387-399.
[6] Pomeroy L R. The ocean’s food wed, a changing paradigm [J]. Bio Science, 1974, 24:499-639.
[7] Rhines P, Young W R. A theory of the winddriven circulation, I. Mid-ocean gyres[J]. Journal of Marine Research , 1982, 40(suppl):559-596.
[8] Rhines P, Young W R. Homogenization of potential vorticity in planetary gyres [J]. Journal of Fluid Mechanics, 1982, 122:347-367.
[9] Ryther J H. Photosynthesis of the sea [J]. Science, 1969, 130:602-608.
[10] Steeman-Nielsen E. The use of radioactive carbon (14C) for measuring organic production in the sea [J]. J Cons Int Explor Mer, 1952, 144:38-46.
[11] Stommel H. The westward intensification of winddriven ocean currents [J]. Transaction of American Geophysical Union, 1948, 29:202-206.
[12] Pedlosky J, Young W R. Ventilation, potential vorticity homogenization and the structure of the ocean circulation [J]. Journal of Physical Oceanography, 1983, 13:2 020-2 037.
[13] Stommel H, Arons A B. On the abyssal circulation of the world ocean I. Stationary planetary flow pattern on a sphere [J]. Deep-Sea Research, 1960, 6:140-154.
[14] Stommel H, Arons A B. On the abyssal circulation of the world ocean II. An idealized model of the circulation pattern and amplitude in oceanic basins [J]. DeepSea Research, 1960, 6:217-233.
[15] Sverdrup H U. Wind-driven currents in a baroclinic ocean: with application to the equatorial currents of the eastern Pacific [J]. Proceedings of National Academy of Sciences, 1947, 33:318-326.
[16] 50 Years of Ocean Discovery: NSF 1950-2000[M]. Washington D G: National Academy Press, 2000.
[17] 中国大百科全书编辑委员会.大气科学—海洋科学—水文科学[M].北京:中国大百科全书出版社, 1987.
[18] 中国海洋学会.21世纪中国海洋科学与技术展望[M].北京:海洋出版社,1998.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
