The relative importance of chlorophyll and colored dissolved organic matter (CDOM) to the prediction of the diffuse attenuation coefficient in shallow estuaries

被引:56
作者
Branco, AB [1 ]
Kremer, JN [1 ]
机构
[1] Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA
来源
ESTUARIES | 2005年 / 28卷 / 05期
关键词
D O I
10.1007/BF02732903
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The availability of underwater tight is a critical factor in the growth and abundance of primary producers in shallow embayments. The goal of this study was to examine the relative importance of factors influencing tight availability in this type of water body. Many simulation models of aquatic ecosystems predict tight attenuation from chlorophyll or phytoplankton stock. In the three southern New England sites studied here, no useful relationship was found to exist between chlorophyll and K-PAR (the diffuse attenuation coefficient of photosynthetically active radiation; Kirk 1994; Mobley 1994). In 40 of 53 cases, a regression of chlorophyll versus K-PAR was not statisticatly significant. Variation in K-PAR did demonstrate a correlation to salinity, implicating a freshwater source of light attenuating material. This was true even in a system with little freshwater inflow. Colored dissolved organic matter (CDOM) is one such terrestrial input that enters estuaries from their watersheds and can strongly influence the availability of light to aquatic primary producers. This study demonstrated that over 70% of the variability in the K-PAR coefficient can be attributed to CDOM in the shallow estuaries studied. This illustrates the need for improved model formulations that include CDOM in the prediction of light attenuation in shallow coastal systems. A new equation has been developed to predict K-PAR with CDOM.
引用
收藏
页码:643 / 652
页数:10
相关论文
共 73 条
[11]  
CERCO CF, 1994, HYDRODYNAMICS EUTROP
[12]   Coastal ocean optical influences on solar transmission and radiant heating rate [J].
Chang, GC ;
Dickey, TD .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2004, 109 (C1)
[13]   THE FLUORESCENCE OF DISSOLVED ORGANIC-MATTER IN SEAWATER [J].
CHEN, RF ;
BADA, JL .
MARINE CHEMISTRY, 1992, 37 (3-4) :191-221
[14]   High-resolution measurements of chromophoric dissolved organic matter in the Mississippi and Atchafalaya River plume regions [J].
Chen, RF ;
Gardner, GB .
MARINE CHEMISTRY, 2004, 89 (1-4) :103-125
[15]   TURBIDITY AS A CONTROL ON PHYTOPLANKTON BIOMASS AND PRODUCTIVITY IN ESTUARIES [J].
CLOERN, JE .
CONTINENTAL SHELF RESEARCH, 1987, 7 (11-12) :1367-1381
[16]  
Coble P. G., 2004, OCEANOGRAPHY, V17, P50, DOI DOI 10.5670/0CEAN0G.2004.47
[17]   Characterization of marine and terrestrial DOM in seawater using excitation emission matrix spectroscopy [J].
Coble, PG .
MARINE CHEMISTRY, 1996, 51 (04) :325-346
[18]   Distribution and optical properties of CDOM in the Arabian Sea during the 1995 Southwest Monsoon [J].
Coble, PG ;
Del Castillo, CE ;
Avril, B .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1998, 45 (10-11) :2195-2223
[20]   Analysis of the optical properties of the Orinoco River plume by absorption and fluorescence spectroscopy [J].
Del Castillo, CE ;
Coble, PG ;
Morell, JM ;
López, JM ;
Corredor, JE .
MARINE CHEMISTRY, 1999, 66 (1-2) :35-51