Marine Physics

Spectral absorption properties of colored dissolved organic matter along 6°N transect of tropical eastern Indian Ocean

  • HU Shui-bo ,
  • CAO Wen-xi ,
  • LIN Jun-fang ,
  • YANG Yue-zhong ,
  • WANG Gui-fen ,
  • ZHOU wen
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  • 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China; 2. University of Chinese Academy of Sciences, Beijing 100049, China;

Received date: 2011-09-05

  Revised date: 2011-10-25

  Online published: 2013-10-30

Abstract

The spectral absorption properties of colored dissolved organic matter (CDOM) is important for building bio-optical model and for quantitative ocean color remote sensing. During the Eastern Indian Ocean Integrated Scientific Investigation Cruise from April 1 to mid-May, 2011, CDOM was sampled at nine stations along 6°N. Based on the dataset of 36 samples, we examined the relationship between spectral absorption coefficients and the slope of absorption curve (S). Over the whole transect, aCDOM (355) spanned the range of 0.131-0.524 m-1 with an average value of 0.272 m-1, and aCDOM(375) varied between 0.081 and 0.453 m-1 with an average value of 0.242 m-1. The concentration of CDOM was lower than that of nearshore waters, similar to the findings along 18°N of the South China Sea. There exists low correlation between chlorophyll a and absorption coefficient of CDOM. S300—500nm varied between 0.008 and 0.019 nm-1, averaging 0.012 nm-1; S300—350nm was a good indication to M, the molecular relative weight of CDOM. Absorption coefficient and Sof CDOM showed a good negative correlation, so did Mand absorption coefficient. By analyzing CTD data along the 6oN section, water mass with high salinity at depth 30-90 m was found to have an impact on horizontal and vertical distribution of Mand aCDOM(355).

Cite this article

HU Shui-bo , CAO Wen-xi , LIN Jun-fang , YANG Yue-zhong , WANG Gui-fen , ZHOU wen . Spectral absorption properties of colored dissolved organic matter along 6°N transect of tropical eastern Indian Ocean[J]. Journal of Tropical Oceanography, 2013 , 32(4) : 13 -21 . DOI: 10.11978/j.issn.1009-5470.2013.04.003

References

[1]CARDER K L, STEWARD R G, HARVEY G R, et al. Marine humic and fulvic acids: Their effects on remote sensing of oceanchlorophyll[J]. Limnol Oceanogr, 1989, 34: 68-81.
[2]KIRK J T O. Light and photosynthesis in aquatic ecosystem[M]. Cambridge: Cambridge University Press, 1994, 52-90.
[3]GRANSKOG M A, MACDONALD R W, MUNDY C J, et al. Distribution, characteristics and potential impacts of chromophoric dissolved organic matter(CDOM)in Hudson Strait and Hudson Bay, Canada[J]. Cont Shelf Res, 2007, 27: 2032-2050.
[4]BRICAUD A,MOREL A,PRIEUR L. Absorption by dissolved organic matter of the sea (yellow substance) in the UV and visible domain[J]. Limnol Oceanor, 1981, 26(1): 43-53.
[5]STEDMON C A, MARKAGER S. The optics of chromophoric dissolved organic matter (CDOM) in the Greenland Sea: an algorithm for differentiation between marine and terrestrially derived organic matter[J]. Limnol Oceanogr, 2004, 46: 2087-2093.
[6]CARDER K L, HAWES S K, BAKER K A, et al. Reflectance model for quantifying chlorophyll a in the presence of productivity degradation products[J]. J Geophys Res, 1991, 96: 20599-20611.
[7]NELSON N B, SIEGELD A, MICHAELS A F. Seasonal dynamics of colored dissolved organic material in the Sargasso Sea[J]. Deep-Sea Res I, 1998, 45: 931-957.
[8]BRICAUD A, BABIN M, CLAUSTRE H, et al. Light absorption properties and absorption budget of Southeast Pacific waters[J]. J Geophys Res, 2010, 115: C08009.
[9]MORRIS D P, HARGREAVES B P. The role of photochemical degradation of dissolved organic carbon in regulating the UV transparency of three lakes on the Pocono Plateau[J]. Limnol Oceanogr, 1997, 42(2): 239-249.
[10]CHEN Z Q, LI Y, PAN J M. The distributions of the optical properties of colored dissolved organic matter and dissolved organic carbon in the Pearl River Estuary[J]. Continent Shelf Research, 2004, 24: 1845-1856.
[11]FERRARI G M, DOWELL M D, GROSSI S, et al. Relationship between the optical properties of chromophoric dissolved organic matter and total concent ration of dissolved organic carbon in the southern Baltic Sea region[J]. Mar Chem, 1996, 55: 299-316.
[12]ZHAO J, CAO W X, WANG G F, et al. The variations in optical properties of CDOM throughout an algal bloom event[J]. Estuar Coast Shelf Sci, 2009, 82: 225-232.
[13]陈楚群, 潘志林, 施平. 海水光谱模拟及其在黄色物质遥感反演中的应用[J] . 热带海洋学报, 2003, 22(5): 33-39.
[14]HONG H S, WU J Y, SHANG S L, et al. Absorption and fluorescence of chromophoric dissolved organic matter in the Pearl River Estuary, South China[J]. Mar Chem, 2005, 97: 78-89.
[15]MARKAGER S, VINCENT W F. Spectral light attenuation and the absorption of UV and blue light in natural waters[J]. Limnol Oceanogr, 2000, 45: 642-650.
[16]HAAN D H. Solar UV light penetration and photodegradation of humic substances in peaty lake water[J]. Limnol Oceanor, 1993, 38(5): 1072-1076.
[17]HELMS J R, STUBBINS A, RITCHIEJ D, et al. Absorption spectral slopes and slope ratios as indicators of molecular weight, source, and photobleaching of chromophoric dissolved organic matter[J]. Limnol Oceanogr, 2008, 53: 955-969.
[18]PEGAU W, GRAY D, ZANEVELD J R V. Absorption and attenuation of visible and near-infrared light in water:dependence on temperature and salinity[J]. Appl Opt, 1997, 36: 6035-6046.
[19]STEDMON C A, AMON R, RINEHART A J, et al. The supply and characteristics of colored dissolved organic matter (CDOM) in the Arctic Ocean: Pan Arctic trends and differences[J]. Mar Chem, 2011, 124: 108-118.
[20]NELSON N B, SIEGEL D A, CARLSON C A, et al. Hydrography of chromophoric dissolved organic matter in the North Atlantic[J]. Deep-Sea Res Ⅰ, 2007, 54: 710-731.
[21]FINE R A, SMETHIE W M, BULLISTER J L, et al. Decadal ventilation and mixing of Indian Ocean waters[J]. Deep-sea Res, 2008, 55: 20-37.
[22]AHMAD S M, BABU G A, PADMAKUMARI V M, et al. Surface and deep water changes in the northeast Indian Ocean during the last 60 ka inferred from carbon and oxygen isotopes of planktonic and benthic foraminifera[J]. Palaeogeography, 2008, 262: 162-188.
[23]KANTHA L, ROJSIRAPHISAL T, LOPEZ J. The North Indian Ocean circulation and its variability as seen in a numerical hindcast of the years 1993-2004[J]. Prog Oceanogr, 2008, 76: 111-147.
[24]MUELLER J L, FARGION G S, MCCLAINC R, et al. Ocean optics protocols for satellite ocean color sensor validation, Revision 4, Volume Ⅳ: Inherent Optical Properties: Instruments, Characterization, Field Measurements and Data Analysis Protocols[R]. Mitchell B G, 2003: 39.
[25]PARSONS T R, MAITA Y, LALLI C M. A manual of chemical and biological methods for seawater analysis[M]. Oxford: Pergamon Press, 1984: 260-289.
[26]BABIN M, STMMSK D, FERRAR G M, et al.Variations in the light absorption coefficients of phytoplankton, nonalgal particles, and dissolved organic matter in coastal waters around Europe[J]. J Geophys res, 2003, 108: 1-20.
[27]COBLE P, HU C, GOULD R W J R, et al. Colored dissolved organic matter in the coastal ocean: an optical tool for coastal zone environmental assessment and management[J]. Oceanography, 2004, 17: 50-59.
[28]STEDMON C A, MARKAGER S, KAAS H. Optical properties and signatures of chromophoric dissolved organic matter (CDOM) in Danish coastal waters [J]. Estuar Coast Shelf Sci, 2000, 51: 267-278.
[29]ASTORECA R, ROUSSEAU V, LANCELOT C. Coloured dissolved organic matter(CDOM) in Southern North Sea Waters: Optical characterization and possible origin[J]. Estuar Coast Shelf Sci, 2009, 85: 633-640.
[30]KOWALCZUK P, STEDMON C A, MARKAGER S. Modeling absorption by CDOM in the Baltic Sea from season,salinity and chlorophyll[J]. Mar Chem, 2006, 101: 1-11.
[31]KOPELEVICH O V, BURENKOV V I. Relation between the spectral values of the light absorption coefficients of sea water, phytoplanktonic pigments, and the yellow substance[J]. Oceanology, 1977, 17: 278-282.
[32]张运林. 水体中有色可溶性有机物的研究进展[J]. 海洋湖沼通报, 2006, 3: 119-127.
[33]王林, 赵冬至, 杨建洪, 等. 黄海北部CDOM近紫外区吸收光谱特性研究[J]. 光谱学与光谱分析, 2010, 3: 3379-3383.
[34]VODACEK A, BLOUGH N V, DEGRANDPRE M D, et al. Seasonal variation of CDOM and DOC in the middle Atlantic Bight: Terrestrial inputs and photooxidation[J]. Limnol Oceanogr, 1997, 42(4): 674-686.
[35]PIOTROWSKI A M, BANAKAR V K, SCRIVNER A E, et al. Indian Ocean circulation and productivity during the last glacial cycle[J]. Earth Planet Sc Lett, 2009, 285: 179-189.
[36]CHEN R F, BADA J L. The fluorescence of dissolved organic matter in seawater[J]. Mar Chem, 1992, 37: 191-221.
[37]MOORE T S, MATEAR R J, MARRA J, et al. Phytoplankton variability off the Western Australian Coast: Mesoscale eddies and their role in cross-shelf exchange[J]. Deep- Sea Res II, 2007, 54: 943-960.
[38]SWAN C M, SIEGEL D A, NELSON N B, et al. Biogeochemical and hydrographic controls on chromophoric dissolved organic matter distribution in the Pacific Ocean[J]. Deep-Sea Res Ⅰ, 2009, 56: 2175-2192.
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