[1] 秦大河. 全球碳循环[M0]. 北京: 气象出版社, 2003: 1?192.
[2] 张志强, 孙成权. 全球变化研究十年新进展[J]. 科学通报, 1999, 44 (5): 464?477.
[3] 曲建升, 孙成权, 张志强, 等. 全球变化科学中的碳循环研究进展与趋向[J]. 地球科学进展, 2003, 18 (6): 980?987.
[4] 殷建平, 王友绍, 徐继荣, 等. 海洋碳循环研究进展[J]. 生态学报, 2006, 26(2): 566?575.
[5] SIEGENTHALER U, SARMIENTO J I. Atmospheric carbon dioxide and the ocean[J]. Nature, 1993, 365: 119?125.
[6] IPCC. Climate change 2001: the scientific basis[R]. Combridge: Combridge University Press, 2001: 881?883.
[7] 徐永福. 二氧化碳生物地球化学循环研究的进展[J]. 地球科学进展, 1995, 10(4): 367?372.
[8] EPPLEY R W, PETERSON B J. Particulate organic matter flux and planktonic new production in the deep ocean[J]. Nature, 1979, 282: 677?680.
[9] EPPLEY R W, CHAVEZ F P, BARBER R T. Standing stocks of particulate carbon and nitrogen in the equatorial Pacific at 150°W [J]. J Geophys Res, 1992, 97: 655?661.
[10] VOLK T, HOFFERT M I. Ocean carbon pumps: Analysis of relative strengths and efficiencies in ocean-driven atmospheric CO2 changes[C]// SUNDQUIST E T, BROECKER W S. The carbon cycle and atmospheric CO2: Natural variations archean to present. Washington D C: American Geophysical Union,1985: 99-110.
[11] LONGHURST A R, HARRISON W G. The biological pump: Profiles of plankton production and consumption in the upper ocean[J]. Prog Oceanogr, 1989, 22: 47?123.
[12] 潘德炉, 白雁. 我国海洋水色遥感应用工程技术的新进展[J]. 中国工程科学, 2008, 10(9): 14?24.
[13] YODER J. Ocean colour radiometry: Early successes and a look towards the future[C]// HALL J, HARRISON D E, STAMMER D. Proceedings of OceanObs’09: Sustained ocean observations and information for society. Venice, Italy: ESA Publication, 2010: 43?55
[14] GARDNER W D, RICHARDSON M J, CARLSON C A, et al. Determining true particulate organic carbon: Bottle, pumps and methodologies[J]. Deep-Sea ResⅡ, 2003, 50: 655?674.
[15] MENZEL DW, VACCARO R F. The measurement of dissolved organic and particulate carbon in seawater[J]. Limnol Oceanogr, 1964, 9: 138?142.
[16] GORDON D C. Distribution of particulate organic carbon and nitrogen at an oceanic station in the central pacific[J]. Deep-Sea Res Ⅰ, 1971, 18: 1127?1134.
[17] BISHOP J K B, EDMOND J M. A new large volume filtration system for the sampling of oceanic particulate matter[J]. J Mar Res, 1976, 34: 181?198.
[18] BISHOP J K B, SCHUPACK D, SHERREL R M, et al. A multiple unit large volume in situ filtration system for sampling oceanic particulate matter in mesoscale environments[C]// ZIRINO A. Mapping strategies in chemical oceanography. Washington D C: American Chemical Society, 1985: 155-175.
[19] MORAN S B, CHARETTE M A, PIKE S M, et al. Differences in seawater particulate organic carbon concentration in samples collected using small- and large-volume methods: the importance of DOC adsorption to the filter blank[J]. Mar Chem, 1999, 67: 33-42.
[20] KNAP A, MICHAELS A, CLOSE A, et al. Protocols for the Joint Global Ocean Flux Study (JGOFS) core measurements[R]// JGOFS report No. 19. Reprint of the IOC Manuals and Guides No. 29. Paris: UNESCO, 1994: 1?170.
[21] BISHOP J K B. Transmissometer measurement of POC[J]. Deep-Sea Res Ⅰ, 1999, 46 (2): 353-369.
[22] BISHOP J K B, CALVERT S E, SOON M Y S. Spatial and temporal variability of POC in the northeast Subarctic Pacific[J]. Deep-Sea Res Ⅱ, 1999, 46 (11-12): 2699-2733.
[23] STRAMSKI D, REYNOLDS R A, BABIN M, et al. Relationships between the surface concentration of particulate organic carbon and optical properties in the eastern South Pacific and eastern Atlantic Oceans[J]. Biogeosciences, 2008, 5: 171-201.
[24] HUNG C C, GONG G C, CHUNG W C, et al. Enhancement of particulate organic carbon export flux induced by atmospheric forcing in the subtropical oligotrophic northwest Pacific Ocean[J]. Mar Chem, 2009, 113: 19-24.
[25] 国家质量监督检验检疫总局. GB/T 12763.9-2007海洋调查规范——海洋生态调查指南[S]. 北京: 中国标准出版社, 2007: 9-10.
[26] O’REILLY J E, MARITORENA S, MITCHELL B G, et al. Ocean color chlorophyll algorithms for SeaWiFS[J]. J Geophys Res, 1998, 103: 24937?24953.
[27] O’REILLY J E, MARIT0RENA S, SIEGEL D A, et al. Ocean color chlorophyll a algorithms for SeaWiFS. OC2 and OC4: Version 4[C]//HOOKER S B, FIRESTONE E R. SeaWiFS postlaunch technical report series, Vo1. 11. Greenbelt Maryland: NASA Goddard Space Flight Center, 2000: 9?23．
[28] MELIN F. Global Distribution of the Random Uncertainty Associated With Satellite-Derived Chl a[J]. Geoscience and Remote Sensing Letters, 2010, 7: 220?224.
[29] MOREL A. Optical modeling of the upper ocean in relation to its biogenous matter content (case Ⅰ waters) [J]. J Geophys Res, 1988, 93: 10749-10768.
[30] MOREL A, GENTILI B, CHAMI M, et al. Bio-optical properties of high chlorophyll Case 1 waters and of yellow-substance-dominated Case 2 waters [J]. Deep-Sea Res Ⅰ, 2006, 53: 1439?1459.
[31] HUNG J J, WANG S M, CHEN Y L. Biogeochemical controls on distributions and fluxes of dissolved and particulate organic carbon in the Northern South China Sea[J]. Deep-Sea Res Ⅱ, 2007, 54: 1486?1503.
[32] SATHYENDRANATH S, STUART V, NAIR A, et al. Carbon-to-chlorophyll ratio and growth rate of phytoplankton in the sea [J]. Mar Ecol Prog Ser, 2009, 383: 73?84.
[33] GORDON H R, MOREL A. Remote assessment of ocean color for interpretation of satellite visible imagery —A review[M]//Lecture notes on coastal and estuarine studies, New York: Springer-Verlag, 1983: 1?114.
[34] DOXARAN D, FROIDEFOND J M, CASTAING P. A reflectance band ratio used to estimate suspended matter concentrations in sediment-dominated coastal waters[J]. Int J Remote Sens, 2002, 23: 5079-5085.
[35] SIEGEL D A, DICKEY T D, WASHBURN L, et al. Optical determination of particulate abundance and production variations in the oligotrophic ocean[J]. Deep-Sea ResⅠ, 1989, 36: 211-222.
[36] CULLEN J J, LEWIS M R, DAVIS C O, et al. Photosynthetic characteristics and estimated growth rates indicate grazing is the proximate control of primary production in the Equatorial Pacific[J]. J Geophys Res, 1992, 97: 639?654.
[37] WALSH I D, CHUNG S P, RICHARNSON M J, et al. The diel cycle in the integrated particle load in the equatorial Paci?c: A comparison with primary production[J]. Deep-Sea Res Ⅱ, 1995, 42: 465?479.
[38] BOHREN C F, HUFFMAN D R. Absorption and scattering of light by small particles[M]. New York: Wiley, 1983: 57?81.
[39] VERITY P G, ROBERTSON C Y, TRONZO C R, et al. Relationships between cell volume and the carbon and nitrogen content of marine photosynthetic nanoplankton[J]. Limnol Oceanogr, 1992, 37: 1434-1446.
[40] MONTAGNES D J, BERGES J A, HARRISON P J, et al. Estimation of carbon, nitrogen, protein, and chlorophyll a from volume in marine phytoplankton[J]. Limnol Oceanogr, 1994, 39: 1044-1060.
[41] STRAMSKI D. Refractive index of planktonic cells as a measure of cellular carbon and chlorophyll a content[J]. Deep-Sea Res Ⅰ, 1999, 46: 335-351.
[42] DURAND M D, GREEN R E, SOSIK H M, et al. Diel variations in optical properties of Micromonas pusilas (Prasinophyceae) [J]. J Phycol, 2002, 38: 1132-1142.
[43] STRAMSKI D, MOREL A. Optical properties of photosynthetic picoplankton in different physiological states as affected by growth irradiance [J]. Deep-Sea ResⅠ, 1990, 37: 245-266.
[44] STRAMSKI D, REYNOLDS R A. Diel variations in the optical properties of a marine diatom[J]. Limnol Oceanogr, 1993, 38: 1347-1364.
[45] VAILLANCOURT R D, BROWN C W, GUILLARD R R L, et al. Light backscattering properties of marine phytoplankton: Relationships to cell size, chemical composition and taxonomy[J]. J Plankton Res, 2004, 26: 191- 212.
[46] GROB C, ULLOA O, CLAUSTRE H, et al. Contribution of picoplankton to the total particulate organic carbon concentration in the eastern South Pacific[J]. Biogeosciences, 2007, 4: 837-852.
[47] STRAMSKI D, BOSS E, BOGUCKI D, et al. The role of seawater constituents in light backscattering in the ocean[J]. Prog Oceanog, 2004, 61: 27?56.
[48] GARDNER W D, WALSH I D, RICHARDSON M J. Biophysical forcing of particle production and distribution during a spring bloom in the North Atlantic[J]. Deep-Sea Res Ⅱ, 1993, 40: 171-195.
[49] GARDNER W D, MISHONOV A V, RICHARDSON M J. Global POC concentrations from in-situ and satellite data[J]. Deep-Sea Res Ⅱ, 2006, 53: 718-740.
[50] VILLAFANE V, HELBLING W, HOLM-HANSON O. Phytoplankton around Elephant Island, Antarctica[J]. Polar Biol, 1993, 13: 183-191.
[51] MARRA J, LANGDON C, KNUDSON C A. Primary production, water column changes, and the demise of a Phaeocystis bloom at the Marine Light-Mixed Layer site (59°N, 21°W) in the northeast Atlantic Ocean[J]. J Geophys Res, 1995, 100: 6633-6643.
[52] CLASUSTRE H, MOREL A, BABIN M, et al. Variability in particle attenuation and chlorophyll fluorescence in the tropical Pacific: Scales, patterns, and biogeochemical implications[J]. J Geophys Res, 1999, 104: 3401-3422.
[53] MISHONOV A V, GARDNER W D, RICHARDSON M J. Remote sensing and surface POC concentration in the South Atlantic[J]. Deep-Sea Res Ⅱ, 2003, 50: 2997-3015.
[54] STRAMSKI D, REYNOLDS R A, KAHRU M, et al. Estimation of particulate organic carbon in the ocean from satellite remote sensing [J]. Science, 1999, 285: 239-242.
[55] LOISEL H, BOSC E, STRAMSKI D, et al. Seasonal variability of the backscattering coefficients in the Mediterranean Sea based on Satellite SeaWiFS imagery[J]. Geophys Res Lett, 2001, 28(22): 4203?4206.
[56] STRAMSKI D, BRICAUD A, MOREL A. Modeling the inherent optical properties of the ocean based on the detailed composition of the planktonic community[J]. Appl Opt, 2001, 40: 2929?2945.
[57] PABI S, ARRIGO K R. Satellite estimation of marine particulate carbon in waters dominated by different phytoplankton taxa[J]. J Geophys Res, 2006, 110: C10018. doi: 10. 1029/ 2005JC 003137.
[58] LEE Z P, CARDER K L, ARNONE R. Deriving inherent optical properties from water color: A multi-band quasi-analytical algorithm for optically deep waters [J]. Appl Opt, 2002, 41: 5755?5772.
[59] GARVER S A, SIGEL D. Inherent optical property inversion of ocean color spectra and its biogeochemical interpretation 1. Time series from the Sargasso Sea [J]. J Geophys Res, 1997, 102: 18607?18625.
[60] MARITORENA S, SIEGEL D A, PETERSON A R. Optimization of a semianalytical ocean color model for global-scale applications [J]. Appl Opt, 2002, 41: 2705?2714.
[61] LEE Z P. Remote sensing of inherent optical properties: Fundamentals, tests of algorithms, and applications [M]. Dartmouth, Canada: International Ocean-Colour Coordinating Group, 2006: 73?93.
[62] STRAMSKA M, STRAMSKI D. Variability of particulate organic carbon concentration in the north polar Atlantic based on ocean color observations with Sea-viewing Wide Field of-View Sensor (SeaWiFS)[J]. J Geophys Res, 2005, 111: C09003. doi: 10. 1029/2004JC 002762.
[63] SON Y B, GARDNER W D, MISHONOV A V, et al. Multispectral remote sensing algorithms for particulate organic carbon (POC) in the Gulf of Mexico [J]. Remote Sens Environ, 2009, 113: 50?61.
[64] ALLISON D B, STRAMSKI D, MITCHELL B G. Empirical ocean color algorithms for estimating particulate organic carbon in the Southern Ocean[J]. J Geophys Res, 2010, 115: C10044. doi: 10. 1029/2009JC006040.
[65] STRAMSKA M. Particulate organic carbon in the global ocean derived from SeaWiFS ocean color[J]. Deep- Sea Res Ⅰ, 2009, 56: 1459-1470.
[66] GAURIER LD, LOISEL H, DESSAILLY D, et al. Estimates of particulate organic carbon over the euphotic depth from in situ measurements: Application to satellite data over the global ocean [J]. Deep-Sea Res Ⅰ, 2010, 57(3): 351?367.
[67] STRAMSKA M. Diffusive component of the vertical flux of particulate organic carbon in the north polar Atlantic [J]. Ocenolog, 2006, 48(4): 455?477.
[68] STRAMSKA M. The diffusive component of particulate organic carbon export in the North Atlantic estimated from SeaWiFS ocean color [J]. Deep-Sea Res Ⅰ, 2010, 57: 284?296.
[69] ALLISON D B, STRAMSKI D, MITCHELL B G. Seasonal and interannual variability of particulate organic carbon within the Southern Ocean from satellite ocean color observation [J]. J Geophys Res, 2010, 115: C06002.
[70] BEHRENFELD M J, BOSS E. The beam attenuation to chlorophyll ratio: an optical index of phytoplankton photoacclimation in the surface ocean? [J]. Deep-Sea Res Ⅰ, 2003, 50: 1537?1549.
[71] BEHRENFELD M J, BOSS E, SIEGEL D A, et al. Carbon-based ocean productivity and phytoplankton physiology from space[J]. Global Biogeochem Cycles, 2005, 19: GB1006. doi: 10.1029/2004GB002299.
[72] BEHRENFELD M J, FALKOWSKI P G. Photosynthetic rates derived from satellite-based chlorophyll concentration [J]. Limnol Oceanogr, 1997, 42: 1?20.
[73] WESTBERRY T, BEHRENFELD M J, SIEGEL D A, et al. Carbon-based primary productivity modeling with vertically resolved photoacclimation[J]. Global Biogeochem Cycles, 2008, 22: GB2024. doi: 10.1029/2007GB003078.
[74] OUBELKHEIR K, SCIANDRA A. Diel variations in particle stocks in the oligotrophic waters of the Ionian Sea (Mediterranean)[J]. J Mar Syst, 2008, 74: 364?371.
[75] GERNEZ P, ANTONIE D, HUOT Y. Diel cycles of the particulate beam attenuation coefficient under varying trophic conditions in the northwestern Mediterranean Sea: Observations and modeling[J]. Limnol Oceanogr, 2011, 56(1): 17?36.
[76] STRAMSKA M, DICKEY T D. Variability of bio-optical properties of the upper ocean associated with diel cycles in phytoplankton population[J]. J Geophys Res, 1992, 97: 17873-17887.
[77] CLAUSTRE H, HUOT Y, OBERNOSTERER I, et al. Gross community production and metabolic balance in the South Pacific Gyre, using a non intrusive bio-optical method[J]. Biogeosciences, 2008, 5: 463?474.
[78] KARP-BOSS L, WHEELER P A, HALES B, et al. Distributions and variability of particulate organic matter in a coastal upwelling system [J]. J Geophys Res, 2004, 109: C09010. doi: 10.1029/2003JC002184.
[79] BISHOP J K B, DAVIS R E, SHERMAN J T. Robotic observations of dust storm enhancement of carbon biomass in the North Pacific[J]. Science, 2002, 298: 817-821.
[80] BISHOP J K B. Autonomous observations of the ocean biological carbon pump[J]. Oceanography, 2009, 22(2): 182-193.
[81] 戴民汉, 魏俊峰, 翟惟东. 南海碳的生物地球化学研究进展[J]. 厦门大学学报:自然科学版, 2001, 40(2): 545?551.
[82] 李宁, 李学刚, 宋金明. 海洋碳循环研究的关键生物地球化学过程[J]. 海洋环境科学, 2005, 24(2): 75?80.
[83] 孙云明, 宋金明. 中国海洋碳循环生物地球化学过程研究的主要进展(1998—2002)[J]. 海洋科学进展, 2002, 20(3): 110?118.
[84] 金海燕, 林以安, 陈建芳, 等. 黄海、东海颗粒有机碳的分布特征及其影响因子分析[J]. 海洋学报, 2005, 27(5): 46?53.
[85] 黄自强, 傅天保, 张远辉. 东海海水中POC的分布特征[J]. 台湾海峡, 1997, 16(2): 145?152.
[86] 刘占飞, 彭兴跃, 徐立, 等. 台湾海峡1997年夏季和1998年冬季两航次颗粒有机碳研究[J]. 台湾海峡. 2000, 19(1): 95?101.
[87] 赵继胜, 姬泓巍, 郭志刚. 冬季东海典型海域颗粒有机碳的垂直分布[J]. 海洋科学, 2003, 27(6): 59?63．
[88] 张乃星, 宋金明, 贺志鹏. 海水颗粒有机碳(POC)变化的生物地球化学机制[J]. 生态学报, 2006, 26(7): 2328-2339.
[89] 严宏强, 余克服, 谭烨辉. 夏季南海北部水体中颗粒有机碳的分布特征[J]. 热带地理, 2011, 31(2): 133?137.
[90] 叶翔, 李炎, 黄邦钦, 等. 台湾海峡南部夏季的颗粒有机碳[J]. 海洋学报, 2009, 31(6): 87?99.
[91] 白雁. 中国近海固有光学量及有机碳卫星遥感反演研究[D]. 北京: 中国科学院上海技术物理研究所, 2007: 1?159.
[92] 魏建伟, 方习生, 石学法, 等. 海水光衰减变化与颗粒有机碳估算—以菲律宾海为例[J]. 海洋科学进展, 2007, 25(4): 460?467.
[93] WANG G F, ZHOU W, CAO W X, et al. Variation of particulate organic carbon and its relationship with bio- optical properties during a phytoplankton bloom in the Pearl River estuary[J]. Mar Pollut Bull, 2011, 62: 1939-1947.
