Sentence examples for deep eddies from inspiring English sources

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Deep eddies develop in a pattern where the deep fields were offset and leading upper meanders consistent with developing baroclinic instability.

However, the main channel is extremely deep (>200 m) in some regions [ 20], and the presence of numerous crevices created by large boulders extending along alternately shallow and deep shoreline habitats, as well as high levels of suspended particulate matter and deep eddies, may create extremely low-light conditions in the system [ 24].

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Look to the Deep Eddy Vodka acquisition as one.

During Loop Current Eddy detachment and formation events, a marked increase in deep eddy kinetic energy occurs coincident with the growth of a large-scale meander along the northern and eastern parts of the Loop Current.

Instead, entrepreneur Sean Cusack, Clayton Christopher — formerly of Deep Eddy Vodka — and distiller Daniel Barnes start their drink with Floridian orange wine.

Hands down the best dive bar in town, Deep Eddy encapsulates the old small-town Austin that so many newer establishments unsuccessfully chase.

The main waterfall, known variously as Celilo Falls, The Chutes, Great Falls, or Columbia Falls, consisted of three sections: a cataract, called Horseshoe Falls or Tumwater Falls; a deep eddy, the Cul-de-Sac; and the main channel.

The deep lower-layer eddies, constrained by the closed topography of the southeastern Gulf, propagated westward across the detachment zone and appear to assist in achieving separation.

My personal view is that Sally got caught unawares in the great, deep, and confusing eddy of contingency, which has other contingency streams running into it, some visible, some too deep-coursing for us to know about.

"My personal view," Frank says, "is that Sally got caught unawares in the great, deep and confusing eddy of contingency, which has other contingency streams running into it, some visible, some too deep-coursing below the surface to know about.

Passing into the Atlantic, the Stream becomes less a current than a drift of water, fanning out in three main directions: southward into the Sargasso Sea; northward into the Norwegian Sea, where it forms eddies and deep vortexes; eastward to warm the coast of Europe, and to pass into the Mediterranean.

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