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Donald H. Lenschow

Researcher at National Center for Atmospheric Research

Publications -  225
Citations -  14880

Donald H. Lenschow is an academic researcher from National Center for Atmospheric Research. The author has contributed to research in topics: Planetary boundary layer & Boundary layer. The author has an hindex of 66, co-authored 223 publications receiving 13792 citations. Previous affiliations of Donald H. Lenschow include University of Oklahoma & National Oceanic and Atmospheric Administration.

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The characteristics of turbulent velocity components in the surface layer under convective conditions

TL;DR: In this article, it was shown that the standard deviations of the horizontal velocity components to the friction velocity in the surface layer under convective conditions depend only on the height of the lowest inversion and the length of the Monin-Obukhov length.
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How Long Is Long Enough When Measuring Fluxes and Other Turbulence Statistics

TL;DR: In this article, it is determined how long a time series must be to estimate covariances and moments up to fourth order with a specified statistical significance, and the minimum value of T necessary to obtain systematic and random errors smaller than specified values.
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Mean-Field and Second-Moment Budgets in a Baroclinic, Convective Boundary Layer

TL;DR: In this article, the authors evaluated the second-moment budgets of turbulence kinetic energy, temperature and humidity variances, and temperature fluxes for a baroclinic, convective boundary layer using data obtained from the NCAR Electra aircraft during the AMTEX.
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Rain in Shallow Cumulus Over the Ocean: The RICO Campaign

TL;DR: Rain in Cumulus over the Ocean (RICO) field campaign as mentioned in this paper emphasized measurements of processes related to the formation of rain in shallow cumuli, and how rain subsequently modifies the structure and ensemble statistics of trade wind clouds.
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Structure of the Entrainment Zone Capping the Convective Atmospheric Boundary Layer

TL;DR: In this article, large-eddy simulation (LES) is used to investigate entrainment and structure of the inversion layer of a clear convectively driven planetary boundary layer (PBL) over a range of bulk Richardson numbers, Ri.