Microplankton And Optical Variability In The Sea: Fundamental Relationships

Several fundamental relationships appear to be important for the interpretation of biological and optical measurements made at sea: 1. The growth of phytoplankton and cyanobacteria supports the entire planktonic community and such growth can only occur by the absorp-tion of light downwelling through the water column. 2. Suspended marine particles are the major source of optical variability in the open ocean and many coastal waters. 3. The numerical concentration of particles of a given size varies as the inverse fourth power of the particles' diameter, thus small cells and detritus are major sources of light scattering and absorption. Since these small particles have relatively low indices of refraction, the complexity of applying Mie Lorentz theory is diminished. 4. For pathlengths of 1 m or less the attenuance of collimated light is sufficiently low so that measurements can be interpreted in terms of single scattering. 5. The efficiency with which light absorbed by a phytoplankter is converted into cellular material appears to be predictable, dependent only upon ambient light intensities. These relationships were then used to examine changes in the absorption and scattering properties of particles within the water column.

[1]  Albert W. Dibelka,et al.  Relationship between chlorophyll a fluorescence and underwater light transmission in coastal waters off Southern California , 1984 .

[2]  Annick Bricaud,et al.  Optical efficiency factors of some phytoplankters1 , 1983 .

[3]  L. Prieur,et al.  Analysis of variations in ocean color1 , 1977 .

[4]  K. Baker,et al.  The bio‐optical state of ocean waters and remote sensing 1 , 1978 .

[5]  D. Kiefer,et al.  Vertical distribution of phaeopigments—I. A simple grazing and photooxidative scheme for small particles , 1982 .

[6]  C. Yentsch The influence of phytoplankton pigments on the colour of sea water , 1960 .

[7]  E. Laws,et al.  Nutrient‐ and light‐limited growth of Thalassiosira fluviatilis in continuous culture, with implications for phytoplankton growth in the ocean , 1980 .

[8]  T. T. Bannister Quantitative description of steady state, nutrient‐saturated algal growth, including adaptation , 1979 .

[9]  H. Gordon,et al.  Two component mie scattering models of sargasso sea particles. , 1973, Applied optics.

[10]  Karen S. Baker,et al.  Optical classification of natural waters 1 , 1978 .

[11]  R. W. Austin,et al.  The effect of varying phytoplankton concentration on submarine light transmission in the Gulf of California1 , 1974 .

[12]  I. N. McCave Vertical flux of particles in the ocean , 1975 .

[13]  H. Gordon,et al.  Phytoplankton Pigments from the Nimbus-7 Coastal Zone Color Scanner: Comparisons with Surface Measurements , 1980, Science.

[14]  A. Bricaud,et al.  Theoretical results concerning light absorption in a discrete medium, and application to specific absorption of phytoplankton , 1981 .

[15]  Dale A. Kiefer,et al.  A simple, steady state description of phytoplankton growth based on absorption cross section and quantum efficiency1 , 1983 .