id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
esrj-21260	Villegas, Nancy	FINE THERMOHALINE STRUCTURE OF THE COLOMBIAN PACIFIC OCEAN	2004	7	.pdf	application/pdf	3334	196	57	MAY 2000 Numbers of station and type of stability Layers, m 1 5 14 17 29 33 42 43 47 49 79 81 107 111 114 0-10 LC AS AS AI AS LC AI AS AS SF AS SF SF AS AI 10-25 AS LC AS AS AS AS AS AS AS AS AS AS AS AS AS 25-50 AS AS AS AS AS AS AS AS AS AS SF SF AS AS SF 50-75 AS AS AS SF AS AS AS AS AS AS AS AS AS AS AS 75-100 AS AS AS AS AS SF SF AS SF SF SF SF AS SF AS 100-150 AS AS AS AS AS AS AS AS SF AS AS SF SF AS SF 150-200 AS SF AS SF SF SF AS SF SF AS SF AS SF SF AS 200-300 SF SF SF AS SF SF SF SF SF SF SF SF SF SF SF 300-400 – SF SF SF SF SF SF SF SF SF – SF SF SF SF 400-500 – SF SF – – SF AS SF – SF – AS SF SF SF 500-600 – – – – – – – – – SF – – SF – SF CONCLUSIONS Layers with predominance of different mechanisms of fine structure were determined. In shift instability of currents and internal waves, turbulence and elements of fine structure of hydrophysical fields arise under action of strong hydrodynamical instability in zones with high vertical gradients of speed current, like located areas observed as separate turbulent spots (Benilov, 1985, Maderich and Nikishev, 1986).	cache/esrj-21260.pdf	txt/esrj-21260.txt