Cos


Also found in: Dictionary, Thesaurus, Medical, Legal, Financial, Acronyms, Wikipedia.

Cos,

Greece: see KósKós
, Lat. Cos, island (1991 pop. 26,379), 111 sq mi (287 sq km), SE Greece, in the Aegean Sea; 2d largest of the Dodecanese, near the Bodrum peninsula of Turkey. Although it rises to c.2,870 ft (875 m) in the southeast, the island is mostly low-lying.
..... Click the link for more information.
.
The Columbia Electronic Encyclopedia™ Copyright © 2013, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/
The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Cos

 

a Greek island in the Aegean Sea, part of the Southern Sporades, near Asia Minor. Length, approximately 40 km; width, up to 10 km; area, 267 sq km. Hilly plains and plateaus predominate; in the east there are low mountains, reaching an elevation of 846 m. The vegetation is primarily of a Mediterranean shrub type. There is subtropical agriculture. The island’s principal city is also named Cos.

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.

cos

(mathematics)
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.

cos

, cos lettuce
a variety of lettuce with a long slender head and crisp leaves
Collins Discovery Encyclopedia, 1st edition © HarperCollins Publishers 2005

COS

(1)
Cray Operating System.

COS

(2)
This article is provided by FOLDOC - Free Online Dictionary of Computing (foldoc.org)

COS

(1) See class of service.

(2) See Corporation for Open Systems.

(3) (Console Operating System) See VMware.

(4) (Cray Operating System) An operating system used in Cray computers. See Cray.
Copyright © 1981-2019 by The Computer Language Company Inc. All Rights reserved. THIS DEFINITION IS FOR PERSONAL USE ONLY. All other reproduction is strictly prohibited without permission from the publisher.
References in periodicals archive ?
[e.sub.3] = (-cos [phi] cos [theta] sin [psi] - sin [phi] cos [psi], -sin [phi] cos [theta] sin [psi] + cos [phi] cos [psi], sin [theta] sin [psi]).
(46), [sin.sup.2] [beta]([cos.sup.2] [alpha] - [sin.sup.2] [alpha]), is calculated by making use of the fact that sin [beta] cos [alpha] is the first component of z, and sin [beta] sin [alpha] is the second:
= 1/3[[sin.sup.2] 0 [cos.sup.2] [phi] - [sin.sup.2] [theta] [sin.sup.2][phi] + [(cos [phi] cos [theta] cos [psi] - sin [phi] sin [psi]).sup.2] - [(sin [phi] cos [theta] cos [psi] + cos [phi] sin [psi]).sup.2] + [(cos [phi] cos [theta] sin [psi] + sin [phi] cos [psi]).sup.2] - [(sin [phi] cos [theta] sin [psi] - cos [phi] cos [psi]).sup.2]], (67)