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Journal ArticleDOI

The Coastal Transition Zone program

Kenneth H. Brink, +1 more
- 15 Aug 1991 - 
- Vol. 96, pp 14637-14647
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TLDR
The main focus of the Coastal Transition Zone (CTZ) program as discussed by the authors was to find cold surface features often found in eastern boundary current regions, and these features represent the main focus for the coastal transition zone program, which took place in 1987 and 1988 off the northern coast of California.
Abstract
Filaments are cold surface features often found in eastern boundary current regions. A typical filament originates near the shelf and extends as a narrow (100 km or less) tongue extending hundreds of kilometers offshore. These features represent the main focus of the the Coastal Transition Zone program, which took place in 1987 and 1988 off the northern coast of California. The historical background for the program is discussed, as well as the questions that motivated it. The general approach of the program is described, followed by an overview of the initial findings, representing a summary of our current understanding of these features and their relation with eastern boundary current dynamics.

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Citations
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Mesoscale to Submesoscale Transition in the California Current System. Part I: Flow Structure, Eddy Flux, and Observational Tests

TL;DR: In this paper, a submesoscale transition in the eddy variability as the horizontal grid scale is reduced to O(1) km is described in terms of the emergent flow structure and the associated time-averaged eddy fluxes.
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Seasonal cycles of pelagic production and consumption

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Atlas of modern organic-walled dinoflagellate cyst distribution

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Patterns and processes in the California Current System

TL;DR: In this article, a simplified case of winds and a linear coast, then consider variability characteristic of the California Current System (CCS), and conclude by considering future change is considered.
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Spatiotemporal Complexity of Plankton and Fish Dynamics

TL;DR: The results show that modeling by reaction-diffusion equations is an appropriate tool for investigating fundamental mechanisms of complex spatiotemporal plankton dynamics, fractal properties of planktivorous fish school movements, and their interrelationships.
References
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Journal ArticleDOI

A one‐dimensional model of the seasonal thermocline II. The general theory and its consequences

TL;DR: In this article, a theory of layer formation due to surface processes is presented, which is more general than that used in the preceding paper I. The theory is applicable to arbitrary forms of heating, including intermittent or continuous processes, and could be used to investigate diurnal and seasonal effects.
Journal ArticleDOI

The California current system—hypotheses and facts☆

TL;DR: In this article, the authors describe the seasonal variation of the various currents which comprise the California Current System, the California Undercurrent, the Davidson Current and the Southern California Countercurrent and investigate qualitatively the dynamical relationships among these currents.
Journal ArticleDOI

Drifter observations of coastal surface currents during CODE: The method and descriptive view

TL;DR: In this article, near-surface coastal currents were made off the Northern California coast during the Coastal Dynamics Experiment (CODE) by using 164 current-following drifters, and the results disclosed a number of energetic mesoscale features that dominate across-shelf transport.
Journal ArticleDOI

The nature of the cold filaments in the California Current system

TL;DR: In this article, the velocity fields and water properties associated with cold filaments in the California Current are described on the basis of data from the Coastal Transition Zone experiment, combined with previous field surveys and satellite imagery, these show seasonal variability with maximum dynamic height ranges and velocities in summer and minimum values in late winter and early spring.
Journal ArticleDOI

A poleward flow along the Atlantic coast of the Iberian peninsula

TL;DR: In this article, the authors show that poleward flow over the continental slope of the Atlantic coast of Resolution Radiometer (AVHRR) imagery and Argos the Iberian Peninsula in a narrow (approximately tracked drifters have revealed the existence of a 100 km) vein, centered at a depth around 1000 m narrow surface poleward current along the (Lacombe, 1971; Reid, 1979).
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