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Oceanography of the British Columbia Coast

TLDR
Thomas et al. as mentioned in this paper described the physical aspects of the sea as exemplified by the Pacific Ocean and the contiguous waters of the British Columbia coast, and attempted to elucidate the nature of oceanic motions and to relate them to everyday experience for the general interest of the casual reader and for the practical benefit of the professional mariner, scientist, or engineer.
Abstract
THOMSON, R.E. 1981. Oceanography of the British Columbia coast. Can. Spec. Publ. Fish. Aquat. Sci. 56: 291p. This book deals with the physical aspects of the sea as exemplified by the Pacific Ocean and the contiguous waters of the British Columbia coast. Although principally devoted to waves, currents, and tides, the book spans a broad spectrum of topics ranging from meteorology and marine biology to past and present marine geology. It attempts to elucidate the nature of oceanic motions and to relate them to everyday experience for the general interest of the casual reader and for the practical benefit of the professional mariner, scientist, or engineer.

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Citations
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Oceanography of the U.S. Pacific Northwest coastal ocean and estuaries with application to coastal ecology

TL;DR: In this article, the authors suggest that mesoscale features have important effects on the magnitude and timing of macronutrients or micronutrient delivery to the plankton and that these features are potentially important as well to transport pathways and residence times of planktonic larvae and to the development of harmful algal blooms.
Journal ArticleDOI

Climate change in the Fraser River watershed: flow and temperature projections

TL;DR: In this article, an analysis of the historic flows and water temperatures of the Fraser River system has detected trends in both the annual flow profile and the summer temperatures, which suggests that the historical trends may already be related to climate change.
Journal ArticleDOI

Herbivore grazing increases polyphenolic defenses in the intertidal brown alga fucus distichus

Kathryn L. Van Alstyne
- 01 Jun 1988 - 
TL;DR: Herbivorous snails (Littorina sitkana) showed a preference for clipped plants after they were wounded, however, over a 2-wk period the snails shifted their preference towards the uninjured control plants, corresponding with the increase in polyphenolic levels within the experimentally damaged plants.
Journal ArticleDOI

Temporal and spatial occurrence of thin phytoplankton layers in relation to physical processes

TL;DR: In this article, three cruises were conducted to simultaneously quantify the fine-scale optical and physical structure of the water column, and data from 120 profiles were used to investigate the temporal occurrence and spatial distribution of thin layers of phytoplankton as they relate to varia- tions in physical processes.
Journal ArticleDOI

‘What's larvae got to do with it?’ Disparate patterns of post‐glacial population structure in two benthic marine gastropods with identical dispersal potential

TL;DR: The genetic structure of two closely related northeastern Pacific gastropods that lack planktonic larvae but which have distributions extending more than 1000 km north of the southern limit of glaciers at the LGM are characterized to suggest that for some faunas, ecological differences between taxa may be more important than larval dispersal potential in determining species’ long‐term biogeographical responses to climate change.
References
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Journal ArticleDOI

On the generation of surface waves by shear flows

TL;DR: In this paper, an approximate solution to the boundary value problem is developed for a logarithmic profile and the corresponding spectral distribution of the energy transfer coefficient calculated as a function of wave speed.
Book

Waves in the ocean

TL;DR: In this article, the generation and dissipation of wave-current interactions were studied. But the authors focused on the critical layer absorption and stability of parallel flows. And they used statistical and probabilistic methods.
Journal ArticleDOI

On the generation of waves by turbulent wind

TL;DR: In this article, it was shown that the most prominent waves are ripples of wavelength λcr = 1·7 cm, corresponding to the minimum phase velocity c = (4gT/ρ)1/4 and moving in directions cos-1(c/Uc) to that of the mean wind, where Uc is the "convection velocity" of the surface pressure fluctuations of length scale λ cr or approximately the average wind speed at a height λCr above the surface.
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