Index Catalog // ScholarsArchive@OSU

Creator:: Doel, Ronald E.
Resource Type:: Article
Full Text:: Chamberlin to Apollo] Isis 1999   Doel, Ronald E. Department of

Creator:: Doel, Ronald E.
Resource Type:: Article
Full Text:: .)] Isis 2006 Doel, Ronald E. Department of History (and Department of

Creator:: Zaneveld, J. Ronald
Abstract:: An expression is derived for the rate at which the diffuse attenuation coefficient for vector irradiance approaches its asymptotic value in a homogeneous medium. The asymptotic approach rate is shown to be a function of boundary conditions at the surface and the asymptotic diffuse attenuation coefficient which is an inherent...
Resource Type:: Article
Full Text:: ZANEVELD, J. RONALD V. An asymptotic closure theory for

Creator:: Doel, Ronald E.
Resource Type:: Article
Full Text:: 2000 Doel, Ronald E. Department of History (and Department of Geosciences), Oregon

Creator:: Doel, Ronald E.
Abstract:: Prior studies of modem scientific internationalism have been written primarily from the point of view of scientists, with little regard to the influence of the state. This study examines the state's role in international scientific relations. States sometimes encouraged scientific internationalism; in the mid-twentieth century,t hey often sought to restrict...
Resource Type:: Article
Full Text:: Doel, Ronald E. Department of History (and Department of Geosciences), Oregon State University

Creator:: Zaneveld, J. Ronald
Abstract:: An expression for the ratio of the upwelling nadir radiance L(π, z) and the downwelling scalar irradiance Eod(Z) is derived from the following equation of radiative transfer. This expression is given by RSR(z)=[L(π, z)]/Eod(Z) = [fb(z)bb(z)]/2π[k(π, z) + c(z) – fL(z)bf(z)], where bb(z) is the backscattering coefficient, k(π, z) is...
Resource Type:: Article
Full Text:: remotely sensed reflectance of the ocean on the inherent optical properties J. Ronald V. Zaneveld

Creator:: Zaneveld, J. Ronald V.
Abstract:: An exact expression for the remotely sensed reflectance (RSR, upwelling radiance divided by downwelling scalar irradiance) just beneath the surface of the ocean is derived from the equation of radiative transfer. It is shown that the RSR at a given depth in the ocean depends only on the inherent optical...
Resource Type:: Article
Full Text:: structure: a theoretical derivation J. Ronald V. Zaneveld An exact expression for the remotely sensed

Creator:: Boss, Emmanuel and Zaneveld, J. Ronald
Abstract:: Measurements of inherent optical properties (IOP) were conducted over bottoms with different substrates by use of a sampling package mounted on and operated by a SCUBA diver. It was found that in areas of low ambient currents the distribution of IOP varies with bottom type in (1) its value relative...
Resource Type:: Article
Full Text:: BOSS, EMMANUEL, AND J. RONALD V. ZANEVELD The effect of bottom

Creator:: Zaneveld, J. Ronald and Boss, Emmanuel
Abstract:: The reflectance of the bottom is of importance when interpreting optical data in shallow water. Closure studies of radiative transfer, interpretation of laser line scanner data, lidar, and remote sensing in shallow waters require understanding of the bottom reflectance. In the Coastal Benthic Optical Properties experiment (CoBOP), extensive measurements of...
Resource Type:: Article
Full Text:: ZANEVELD, J. RONALD V., AND EMMANUEL BOSS The influence of bottom

Creator:: Pak, Hasong and Zaneveld, J. Ronald
Abstract:: One hundred and seventy pairs of temperature and light transmission profiles were obtained by simultaneous conductivity-temperature-depth (CTD) and light transmissometer casts in three cruises on the R/V Yaquina over the continental shelf off Oregon. These were analyzed for bottom nepheloid layers (BNL) and bottom mixed layers layers (BML). Supplementing these...
Resource Type:: Article
Full Text:: . RONALD V. ZANEVELD School of Oceanography, Oregon State University, Corvallis, Oregon 97331 One

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