I am a Senior Scientist within the Earth Observation Laboratory of NCAR and the lead scientist for the Integrated Surface Flux Facility (ISFF). My personal interests encompass all aspects of turbulence, micrometeorology (in particular the measurement of surface fluxes), and boundary layer meteorology.
Horst, T.W., and D.H. Lenschow, 2008: Attenuation of scalar fluxes measured with spatially-displaced sensors. accepted for publication in Boundary Layer Meteorology.
Horst, T.W., and S.P. Oncley, 2006: Corrections to inertial-range power spectra measured by CSAT3 and Solent sonic anemometers, 1. Path-average errors. Boundary Layer Meteorology, 119, 375--395.
Venketram, A., and T.W. Horst, 2006: Approximating dispersion from finite line sources. Atmospheric Environment, 40, 2401--2408.
See below for links to additional papers.
Winners of the 2004 UCAR Outstanding Performance Awards
P.P. Sullivan, T.W. Horst, D.H. Lenschow, C.-H. Moeng, and J.C. Weil, 2003: Structure of subfilter-scale fluxes in the atmospheric surface layer with application to large-eddy simulation modeling. J. Fluid Mechanics, V. 482, 101--139.
T.W. Horst, J. Kleissl, D.H. Lenschow, C. Meneveau, C.-H. Moeng, M.B. Parlange, P.P. Sullivan, and J.C. Weil, 2004: HATS: Field observations to obtain spatially filtered turbulence fields from crosswind arrays of sonic anemometers in the atmospheric surface layer. J. Atmospheric Sciences, V. 61, 1566--1581.
Horst, T.W., S.P. Oncley, S.E. Larsen, M. Nielsen, and C.W. Fairall, 2005. Corrections to power spectra measured with CSAT3 and Solent sonic anemometers. EGU General Assembly, April 24--29, 2005, Vienna, Austria.
Horst, T.W., and D.H. Lenschow, 2008: Attenuation of scalar fluxes measured with spatially-displaced sensors. accepted for publication in Boundary Layer Meteorology.
Horst, T.W., and J.C. Weil, 1992. Footprint estimation for scalar flux measurements in the atmospheric surface layer. Boundary Layer Meteorology 59, 279--296.
Horst, T.W., and J.C. Weil, 1994. How far is far enough?: The fetch requirements for micrometeorological measurement of surface fluxes. J. Atmospheric Oceanic Technology, 11, 1019--1025.
Horst, T.W., and J.C. Weil, 1994. Corrigenda: How far is far enough?: The fetch requirements for micrometeorological measurement of surface fluxes. J. Atmospheric Oceanic Technology, 12, 447.
Finn, D., B. Lamb, M.Y. Leclerc, and T.W. Horst, 1996. Experimental evaluation of analytical and lagrangian surface layer flux footprint models. Boundary Layer Meteorology 80, 283--308.
Horst, T.W., 1999. The footprint for estimation of atmosphere-surface exchange fluxes by profile techniques. Boundary Layer Meteorology 90, 171--188.
Horst, T.W., 2001. Comments on: Footprint analysis: a closed analytical solution based on height-dependent profiles of wind speed and eddy viscosity. Boundary Layer Meteorology 101, 435--447.
Horst, T.W., 1977. A surface-depletion model for deposition from a Gaussian plume. Atmospheric Environment, 11, 41--46.
Horst, T.W., 1978. Comments on "A general Gaussian diffusion-deposition model for elevated point sources". J. Applied Meteorology, 17, 415--416.
Horst, T.W., 1979. Lagrangian similarity modeling of vertical diffusion from a ground-level source. J. Applied Meteorology, 18, 733--740.
Horst, T.W., 1984. The modification of plume models to account for dry deposition. Boundary Layer Meteorology, 30, 413-430.
Doran, J.C., and T.W. Horst, 1985. An evaluation of Gaussian plume-depletion models with dual-tracer field measurements. Atmospheric Environment, 19, 939--951.