Received date: 2003-04-07
Revised date: 2003-08-12
Online published: 2003-10-01
Ocean and atmosphere are the most important parts of earth system, which have exerted great effects on global climate change. As the first new project in IGBP II, Surface Ocean-Low Atmosphere Study (SOLAS) will focus on research topics of linked ocean-atmosphere interactions at the ocean-atmosphere interface, including the atmospheric boundary layer (typically to about 1 km) and the upper-ocean boundary layer (typically 100m). SOLAS can contribute to our understanding of the interaction processes and mechanisms between ocean and atmosphere by interdisciplinarity studies. SOLAS science is underway in many countries. Reports on the status of SOLAS activity in 16 countries are received. China has drawn the draft national science plan, which mainly focus on scientific questions in Chinese coastal areas about the input of atmospheric species to the sea, the emissions of green house gases from the sea, exchange processes at the air-sea interface in order to understand and quantify the role that ocean-atmosphere interactions play in the regulation of climate and environmental changes.
Yan Ju, Li Xin, Wang Hui . SURFACE OCEAN-LOW ATMOSPHERE STUDY[J]. Advances in Earth Science, 2003 , 18(5) : 812 -816 . DOI: 10.11867/j.issn.1001-8166.2003.05.0812
[1] Bange H W, Rapsomanikis s, Andreae M O. Nitrous oxide in coastal waters[J]. Global Biogeochemical Cycles, 1996,10: 197-207.
[2] Bates T S, Kelly K C, Johnson J E, et al. A revaluation of the open ocean source of methane to the atmosphere[J]. Journal Geophysical Research, 1996,101: 6 953-6 961.
[3] Bock E J, Hara T, Frew N M, et al. Relationship between air-sea gas transfer and short wind waves[J]. Journal Geophysical Research, 1999,104: 25 821-25 831.
[4] Coale K H, Johnson K S, Fitzwater S E, et al. A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean[J]. Nature, 1996,383: 495-501.
[5] De Angelis M A, Lee C. Methane production during zooplankton grazing on marine phytoplankton[J]. Limnology Oceanography, 1994,39: 1 298-1 308.
[6] Dore J E, Karl D M. Nitrification in the euphotic zone as a source for nitrite, nitrate, and nitrous oxide at station ALOHA[J]. Limnology Oceanography, 1996, 41: 1 619-1 628.
[7] Duce R A, Liss P S, Merrill J T, et al. The atmospheric input of trace species to the world ocean[J]. Global Biogeochemical Cycles, 1991,5: 193-259.
[8] Falkowski P G. Evolution of the nitrogen cycle and its influence on the biological CO2 pump in the ocean[J]. Nature, 1997,387: 272-275.
[9] Gabric A J, Whetton P H, Boers R, et al. The impact of simulated climate change on the air-sea flux of dimethylsulphide in the subantarctic Southern Ocean[J]. Tellus,1998,50B: 388.
[10] Johnson K S, Gordon R M, CoaleK H. What controls dissolved iron in the world ocean?[J]. Marine Chemistry, 1997,57: 137-161.
[11] Nevison C D, Weiss R F, Erickson D J III. Global oceanic emissions of nitrous oxide[J]. Journal Geophysical Research, 1995,100: 15 809-15 820.
[12] Nightingale P D, Liss P S, Schlosser P. Measurements of air-sea gas transfer during an open ocean algal bloom[J]. Geophysical Research Letters, 2000,27: 2 117-2 120.
[13] Liss P. SOLAS-Surface Ocean-Lower Atmosphere Study[J]. Global Change Newsletter, IGBP, 2002,50:15-18.
[14] Watson A J. Surface Ocean-Lower Atmosphere Study (SOLAS)[J]. Global Change Newsletter, IGBP, 1997,31: 9-12.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
