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contributor authorOsborn, T. R.
date accessioned2017-06-09T14:43:44Z
date available2017-06-09T14:43:44Z
date copyright1973/07/01
date issued1973
identifier issn0022-3670
identifier otherams-25380.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162157
description abstractMeasurements of the vertical component of the temperature gradient in Powell Lake show phenomena similar to those observed in the ocean. The gradient is an irregular function of depth, with temperature inversions indicating static instability of the water column on the centimeter scale. The lower portion of the lake contains old sea water. Doubly diffusive layers were found only near the very bottom of the lake and another form of thermohaline circulation may exist for 60 m above the layers.
publisherAmerican Meteorological Society
titleTemperature Microstructure in Powell Lake
typeJournal Paper
journal volume3
journal issue3
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1973)003<0302:TMIPL>2.0.CO;2
journal fristpage302
journal lastpage307
treeJournal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 003
contenttypeFulltext


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