1960
DOI: 10.1111/j.2153-3490.1960.tb01319.x
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Radiance Distribution in the Upper Layers of the Sea

Abstract: The angular distribution of underwater radiance for green light has been studied in the upper turbid layers of the Gullmar fjord by means of a radiance meter which is lowered in the sea along a guide wire with a fixed orientation. A theoretical discussion considers the different components entering into the light field, viz. direct sunlight, skylight, and scattered light. On the basis of available measurements of the volume scattering function the scattered light is evaluated by integrating light scattered fro… Show more

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Cited by 23 publications
(15 citation statements)
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“…In spite of these obvious experimental difficulties, a few determinations were made before World War II (Jerlov and Liljequist 1938;Pettersson 1938). Yet, an internally baffled tube (often called a Gershun tube), with an aperture limiting the acceptance angle and isolating a dV solid angle in a given direction at one end and at the other end a detector, provides a simple means of measuring radiance as defined above.…”
Section: Historical Backgroundmentioning
confidence: 99%
See 2 more Smart Citations
“…In spite of these obvious experimental difficulties, a few determinations were made before World War II (Jerlov and Liljequist 1938;Pettersson 1938). Yet, an internally baffled tube (often called a Gershun tube), with an aperture limiting the acceptance angle and isolating a dV solid angle in a given direction at one end and at the other end a detector, provides a simple means of measuring radiance as defined above.…”
Section: Historical Backgroundmentioning
confidence: 99%
“…Jerlov and Fukuda (1960) made measurements down to 30 m in a vertical plane with a fixed azimuth orientation by guiding the instrument along a taut wire anchored in Gullmar Fjord. Jerlov and Fukuda (1960) made measurements down to 30 m in a vertical plane with a fixed azimuth orientation by guiding the instrument along a taut wire anchored in Gullmar Fjord.…”
Section: Historical Backgroundmentioning
confidence: 99%
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“…The underwater radiance distribution is therefore the fundamental radiometric quantity from which all other optical quantities are derived. Because of this fundamental importance, measurement of the radiance distribution received a great deal of interest in the mid‐1900s [e.g., Jerlov and Fukuda , 1960; Lundgren and Højerslev , 1971; Sasaki et al , 1958; Tyler , 1960]. It is perhaps surprising however, that there have been few subsequent direct observations until recently [ Voss et al , 2003].…”
Section: Background and Basesmentioning
confidence: 99%
“…While in the upper layers of the open ocean the radiance distribution of light is strongly dependent upon the position of the sun, with increasing depth the underwater radiance distribution becomes more symmetrical about the vertical axis [38]. At a certain depth this can be approximated as being cylindrically symmetric about the vertical axis [9,39,40]. In this ideal open-ocean light environment, a vertical 100% reflective mirror provides an ideal form of camouflage, perfectly matching the intensity and spectral properties of the background light field (see fig.…”
Section: Introductionmentioning
confidence: 99%