Light absorption and fluorescence properties of chromophoric dissolved organic matter (CDOM), in the St Lawrence Estuary (Case 2 waters)

被引:120
作者
Nieke, B
Reuter, R
Heuermann, R
Wang, H
Babin, M
Therriault, JC
机构
[1] CARL VON OSSIETZKY UNIV OLDENBURG, FACHBEREICH PHYS, D-26111 OLDENBURG, GERMANY
[2] PHYS TECH BUNDESANSTALT, D-38100 BRAUNSCHWEIG, GERMANY
[3] UNIV PARIS 06, LPCM, F-06230 VILLEFRANCHE SUR MER, FRANCE
[4] MINIST PECHES & OCEANS, INST MAURICE LAMONTAGNE, MONT JOLI, PQ G5H 3Z4, CANADA
关键词
D O I
10.1016/S0278-4343(96)00034-9
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The absorption coefficient and the fluorescence emission of chromophoric (coloured) dissolved organic matter (CDOM) were determined along a 1200 km transect in the Estuary and Gulf of St. Lawrence. Fluorescence spectra were spectrally corrected against a reference standard and normalized to the water Raman signal to provide results in Raman units. Because CDOM originates mainly from freshwater river runoff in the St. Lawrence system, its optical properties were found to be inversely correlated with salinity (r = -0.95) and sigma-t (r = -0.99). These strong linear relationships can be used as a tool for monitoring surface circulation and salinity in these coastal waters. The relationships between CDOM absorption and fluorescence were also characterized in the UV and visible regions. In the UV region, the observed relationship was found to be consistent with previously published results. In the visible region a relationship was found that was different from that in the UV. Our results therefore support the possibility of using fluorescence characteristics for extensive monitoring of CDOM in coastal waters strongly influenced by freshwater runoff. Such relationships may prove useful for remote sensing to correct chi a values and the large-scale modelling of primary production in coastal waters. Copyright (C) 1996 Elsevier Science Ltd
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收藏
页码:235 / 252
页数:18
相关论文
共 59 条
[1]  
ANDRE JM, 1991, OCEANOL ACTA, V14, P3
[2]  
AUSTIN RW, 1977, LIGHT SEA, P121
[3]  
AUSTIN RW, 1977, LIGHT SEA, P104
[4]   VARIATIONS IN THE SPECIFIC ABSORPTION-COEFFICIENT FOR NATURAL PHYTOPLANKTON ASSEMBLAGES - IMPACT ON ESTIMATES OF PRIMARY PRODUCTION [J].
BABIN, M ;
THERRIAULT, JC ;
LEGENDRE, L ;
CONDAL, A .
LIMNOLOGY AND OCEANOGRAPHY, 1993, 38 (01) :154-177
[5]   BIO-OPTICAL CLASSIFICATION AND MODEL OF NATURAL-WATERS .2. [J].
BAKER, KS ;
SMITH, RC .
LIMNOLOGY AND OCEANOGRAPHY, 1982, 27 (03) :500-509
[6]   STRUCTURE AND SEASONAL CHARACTERISTICS OF THE GASPE CURRENT [J].
BENOIT, J ;
ELSABH, MI ;
TANG, CL .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1985, 90 (NC2) :3225-3236
[7]  
BRICAUD A, 1981, LIMNOL OCEANOGR, V26, P43
[8]   AIRBORNE LASER FLUOROSENSOR SURVEY OF THE COLUMBIA AND SNAKE RIVERS - SIMULTANEOUS MEASUREMENTS OF CHLOROPHYLL, DISSOLVED ORGANICS AND OPTICAL ATTENUATION [J].
BRISTOW, MPF ;
BUNDY, DH ;
EDMONDS, CM ;
PONTO, PE ;
FREY, BE ;
SMALL, LF .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1985, 6 (11) :1707-1734
[9]  
BRUNEL P, 1970, REV GEOGR MONTREAL, V24, P291
[10]   REFLECTANCE MODEL FOR QUANTIFYING CHLOROPHYLL-A IN THE PRESENCE OF PRODUCTIVITY DEGRADATION PRODUCTS [J].
CARDER, KL ;
HAWES, SK ;
BAKER, KA ;
SMITH, RC ;
STEWARD, RG ;
MITCHELL, BG .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1991, 96 (C11) :20599-20611