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contributor authorBanta, Robert M.
contributor authorPichugina, Yelena L.
contributor authorNewsom, Rob K.
date accessioned2017-06-09T14:38:22Z
date available2017-06-09T14:38:22Z
date copyright2003/10/01
date issued2003
identifier issn0022-4928
identifier otherams-23348.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159899
description abstractIn the nighttime stable boundary layer (SBL), shear and turbulence are generated in the layer between the maximum of the low-level jet (LLJ) and the earth's surface. Here, it is investigated whether gross properties of the LLJ?its height and speed?could be used to diagnose turbulence intensities in this subjet layer. Data on the height and speed of the LLJ maximum were available at high vertical and temporal resolution using the high-resolution Doppler lidar (HRDL). These data were used to estimate a subjet layer shear, which was computed as the ratio of the speed to the height of the jet maximum, and a jet Richardson number RiJ, averaged at 15-min intervals for 10 nights when HRDL LLJ data were available for this study. The shear and RiJ values were compared with turbulence kinetic energy (TKE) values measured near the top of the 60-m tower at the Cooperative Atmosphere?Surface Exchange Study-1999 (CASES-99) main site. TKE values were small for RiJ greater than 0.4, but as RiJ decreased to less than ?0.4, TKE values increased, indicating that RiJ does have merit in estimating turbulence magnitudes. Another interesting finding was that shear values tended to cluster around a constant value of 0.1 s?1 for TKE values that were not too small, that is, for TKE greater than ?0.1 m2 s?2.
publisherAmerican Meteorological Society
titleRelationship between Low-Level Jet Properties and Turbulence Kinetic Energy in the Nocturnal Stable Boundary Layer
typeJournal Paper
journal volume60
journal issue20
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(2003)060<2549:RBLJPA>2.0.CO;2
journal fristpage2549
journal lastpage2555
treeJournal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 020
contenttypeFulltext


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