By Rochard W. Spinrad, Kendall L. Carder, Mary Jane Perry
ISBN-10: 0195068432
ISBN-13: 9780195068436
Because the ebook of Jerlov's vintage quantity on optical oceanography in 1968, the power to foretell or version the submarine mild box, given measurements of the inherent optical houses of the sea, has more desirable to the purpose that version fields are very on the subject of measured fields. within the final 3 many years, distant sensing functions have fostered robust types that may be inverted to estimate the inherent optical houses heavily with regards to elements vital for figuring out international organic productiveness, environmental caliber, and such a lot nearshore geophysical procedures. This quantity offers an eclectic mixture of data at the theories, experiments, and instrumentation that now represent the ways that optical oceanography is studied. throughout the process this interdisciplinary paintings, the reader is led from the actual innovations of radiative move to the experimental innovations utilized in the lab and at sea, to process-oriented discussions of the biochemical mechanisms accountable for oceanic optical variability. The textual content could be of curiosity to researchers and scholars in actual and organic oceanography, biology, geophysics, limnology, atmospheric optics, and distant sensing of ocean and worldwide weather switch.
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Additional resources for Ocean Optics (Oxford Monographs on Geology and Geophysics)
Sample text
This procedure is illustrated in Fig. 1-2. , directly relating the constituent concentrations to the apparent optical properties. Examples of this are relating the near-surface Kd(\) or the ratio of reflectances at two wavelengths to the phytoplankton pigment concentration. , several species of phytoplankton, and are therefore pooled to form a single constituent (the shaded box). With the exception of the empirical loop, all of the arrows flow from top to bottom through the radiative transfer segment.
In the case of Kd, the vertical attenuation coefficient for irradiance, perhaps all we need is the average increase in Kd for the waveband of interest per unit increase in concentration of any given component. We might, for example, use kc, the average increase in vertical attenuation coefficient for the photosynthetic waveband per mg phytoplankton chlorophyll per cubic meter. To a first approximation this is indeed often a useful approach. There are problems with it, however. The first is that we may not have the empirical relationship we need.
1-5) for these particle phase functions. For a more complete discussion of this subject, including utilizing (K} as well as A", the reader is referred to Gordon (1991). 84) can also be used to shed light on an important question in marine optics mentioned earlier. In the direct problem described earlier, measured values of the inherent optical properties are used to predict the apparent optical properties. However, the inherent optical properties are usually measured at significantly different spatial scales from the apparent optical properties.
Ocean Optics (Oxford Monographs on Geology and Geophysics) by Rochard W. Spinrad, Kendall L. Carder, Mary Jane Perry
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