Transitional, entraining, cloudy, and coastal boundary layers

• Autorzy: Angevine W.
• Języki publikacji: EN

Abstrakty

EN

Atmospheric boundary layers are marvelously varied and complex. Recent re-search has examined some of that variety. Boundary layers over land undergo drastic changes throughout the day as the sun rises and sets, and as clouds form and dissipate. Air is entrained at the top of the boundary layer at varying rates. As air moves over the coast, the boundary layer reacts to changes in surface forcing. All of these changes affect pollutant transport and weather formation. In this paper, research attempting to understand transitional, cloud-topped, and coastal boundary layers, and boundary-layer top entrainment, is reviewed.

Słowa kluczowe

EN

transitional boundary layer; marine boundary layer; entrainment; coastal boundary layer; pollutant transport; advected turbulence

• Wydawca: Instytut Geofizyki PAN ; Springer
• Czasopismo: Acta Geophysica
• Rocznik: 2008
• Tom: Vol. 56, no. 1
• Strony: 2--20

Twórcy

autor

Angevine W.

• CIRES, University of Colorado and NOAA Earth System Research Laboratory, Boulder, Colorado, USA,

Bibliografia

• Angevine, W.M. (1999), Entrainment results including advection and case studies from the flatland boundary layer experiments, J. Geophys. Res. 104, 30,947-30,963.
• Angevine, W.M. (2005), An integrated turbulence scheme for boundary layers with shallow cumulus applied to pollutant transport, J. Appl. Meteor. 44, 1436-1452.
• Angevine, W.M., A.W. Grimsdell, S.A. McKeen, and J.M. Warnock (1998), Entrainment results from the flatland boundary layer experiments, J. Geophys. Res. 103, 13,689-13,701.
• Angevine, W.M., H. Klein Baltink, and F.C. Bosveld (2001), Observations of the morning transition of the convective boundary layer, Bound.-Layer Meteor. 101, 209-227.
• Angevine, W.M., A.B. White, C.J. Senff, M. Trainer, R.M. Banta, and M.A. Ayoub (2003), Urban-rural contrasts in mixing height and cloudiness over Nashville in 1999, J. Geophys. Res. 108, 4092, DOI: 10.1029/2001JD001061.
• Angevine, W.M., C.J. Senff, A.B. White, E.J. Williams, J. Koermer, S.T.K. Miller, R. Talbot, P.E. Johnston, S.A. McKeen, and T. Downs (2004), Coastal boundary layer influence on pollutant transport in New England, J. Appl. Meteor. 43, 1425-1437.
• Angevine, W.M., M. Tjernstrom, and M. Zagar (2006a), Modeling of the coastal boundary layer and pollutant transport in New England, J. Appl. Meteorol. Clim. 45, 137-154.
• Angevine, W.M., J. Hare, C.W. Fairall, D.E. Wolfe, R.J. Hill, W.A. Brewer, and A.B. White (2006b), Structure and formation of the highly stable marine boundary layer over the Gulf of Maine, J. Geophys. Res. 111, D23S22, DOI: 10.1029/2006JD007465.
• Barr, A.G., and A.K. Betts (1997), Radiosonde boundary-layer budgets above a boreal forest, J. Geophys. Res. 102, 29,205-29,212.
• Beare, R.J., J.M. Edwards, and A.J. Lapworth (2006), Simulation of the observed evening transition and nocturnal boundary layers: Large-eddy modeling, Quart. J. Roy. Meteor. Soc. 132, 81-99.
• Betts, A.K., and A.G. Barr (1996), First international satellite land surface climatology field experiment 1987 sonde budget revisited, J. Geophys. Res. 101, 23,285-23,288.
• Beyrich, F., and U. Goersdorf (1995), Composing the diurnal cycle of mixing height from simultaneous sodar and wind profiler measurements, Bound.-Layer Meteor. 76, 387-394.
• Boers, R., E.W. Eloranta, and R.L. Coulter (1984), Lidar observations of mixed layer dynamics: Tests of parameterized entrainment models of mixed layer growth rate, J. Climate Appl. Meteor. 23, 247-266.
• Conzemius, R., and E. Fedorovich (2006a), Dynamics of sheared convective boundary layer entrainment. Part I: Methodological background and large-eddy simulations, J. Atmos. Sci. 63, 1151-1178.
• Conzemius, R., and E. Fedorovich (2006b), Dynamics of sheared convective boundary layer entrainment. Part II: Evaluation of bulk model predictions of entrainment flux, J. Atmos. Sci. 63, 1179-1199.
• Craig, R.A. (1946), Measurements of temperature and humidity in the lowest 1000 feet of the atmosphere over Massachusetts Bay, Pap. Phys. Oceanogr. Meteor. 10, 1-47.
• Doran, J.C., and S.-E. Gryning (1987), Wind and temperature structure over a land-water-land area, J. Climate Appl. Meteor. 26, 973-979.
• Edwards, J.M., R.J. Beare, and A.J. Lapworth (2006), Simulation of the observed evening transition and nocturnal boundary layers: Single-column modelling, Quart. J. Roy. Meteor. Soc. 132, 61-80.
• Fairall, C.W. (1984), Wind shear enhancement of entrainment and refractive index structure parameter at the top of a turbulent mixed layer, J. Atmos. Sci. 41, 3472-3484.
• Fast, J.D., and W.E. Heilman (2003), The effect of lake temperatures and emissions on ozone exposure in the Western Great Lakes region, J. Appl. Meteor. 42, 1197-1217.
• Fedorovich, E., R. Conzemius, and D. Mironov (2004a), Convective entrainment into a shearfree, linearly stratified atmosphere: Bulk models reevaluated through large eddy simulations, J. Atmos. Sci. 61, 281-295.
• Fedorovich, E., R. Conzemius, I. Esau, F.K. Chow, D.C. Lewellen, C.-H. Moeng, P.P. Sullivan, D. Pino, and J. Vila-Guerau de Arellano (2004b), Entrainment into sheared convective boundary layers as predicted by different large eddy simulation codes, Proc. 16th Symposium on Boundary Layers and Turbulence, Portland, ME, Am. Meteor. Soc.
• Garratt, J.R. (1990), The internal boundary layer - a review, Bound.-Layer Meteor. 50, 171-203. Garratt, J.R. (1992), The Atmospheric Boundary Layer, Cambridge, Cambridge Univ. Press, 316 p.
• Grimsdell, A.W. (2003), The Afternoon Transition of the Continental Convective Boundary LayerProgram in Atmospheric and Oceanic Sciences, Boulder, University of Colorado, 150 p.
• Grimsdell, A.W., and W.M. Angevine (2002), Observations of the afternoon transition of the convective boundary layer, J. Appl. Meteor. 41, 3-11.
• Kim, S., S. Park, and C.-H. Moeng (2003), Entrainment processes in the convective boundary layer with varying wind shear, Bound.-Layer Meteor. 108, 221-245.
• Lapworth, A.J., 2006, The morning transition of the nocturnal boundary layer, Bound.-Layer Meteor. 119, 501-526.
• LeMone, M.A., R.L. Grossman, R.T. McMillen, K.-N. Liou, S.C. Ou, S. McKeen, W. Angevine, K. Ikeda, and F. Chen (2002), Cases-97: Late-morning warming and moistening of the convective boundary layer over the Walnut River watershed, Bound.-Layer Meteor. 104, 1-52.
• Lock, A.P., and J. Mailhot (2006), Combining non-local scalings with a tke closure for mixing in boundary-layer clouds, Bound.-Layer Meteor. 121, 313-338, DOI: 10.1007/s10546-006-9062-8.
• Mahrt, L., and D. Vickers (2005), Extremely weak mixing in stable conditions, Bound.-Layer Meteor. 119, 19-39, DOI: 10.1007/s10546-005-9017-5.
• Mahrt, L., J. Sun, W. Blumen, A.C. Delany, and S. Oncley (1998), Nocturnal boundary-layer regimes, Bound.-Layer Meteor. 88, 255-278.
• Mahrt, L., D. Vickers, J. Sun, T.L. Crawford, G. Crescenti, and P. Frederickson (2001), Surface stress in offshore flow and quasi-frictional decoupling, J. Geophys. Res. 106, 20,629-20,639.
• Pino, D., J. Vila-Guerau de Arellano, and P.G. Duynkerke (2003), The contribution of shear to the evolution of a convective boundary layer, J. Atmos. Sci. 60, 1913-1926.
• Rogers, D.P., D.W. Johnson, and C.A. Friehe (1995), The stable internal boundary layer over a coastal sea. Part I: Airborne measurements of the mean and turbulence structure, J. Atmos. Sci. 52, 667-683.
• Seibert, P., F. Beyrich, S.-E. Gryning, S. Joffre, A. Rasmussen, and P. Tercier (1997), Mixing height determination for dispersion modeling. In: COST Action 710: Pre-processing of meteorological data for atmospheric dispersion modeling, Report European Commission.
• Siebesma, A.P., and J. Teixeira (2000), An advection-diffusion scheme for the convective boundary layer: Description and 1d results, Proc. 14th Symposium on Boundary Layers and Turbulence, 7-11Aug, Aspen, CO, Am. Meteor. Soc., 4.16.
• Sillman, S., P.J. Samson, and J.M. Masters (1993), Ozone production in urban plumes transported over water: Photochemical model and case studies in the northeastern and midwestern united states, J. Geophys. Res. 98, 12,687-12,699.
• Smedman, A.-S., H. Bergstroem, and B. Grisogono (1997a), Evolution of stable internal boundary layers over a cold sea, J. Geophys. Res. 102, 1091-1099.
• Smedman, A.-S., U. Hoegstroem, and H. Bergstroem (1997b), The turbulence regime of a very stable marine airflow with quasi-frictional decoupling, J. Geophys. Res. 102, 21,049-21,059.
• Smith, E.A., M.M.-K. Wai, H.J. Cooper, and M.T. Rubes (1994), Linking boundary-layer circulations and surface processes during FIFE 89. Part I: Observational analysis, J. Atmos. Sci. 51, 1497-1529.
• Soares, P.M.M., P.M.A. Miranda, A.P. Siebesma, and J. Teixeira (2004), An eddy-diffusivity/ mass-flux parameterization for dry and shallow cumulus convection, Quart. J. Roy. Meteor. Soc. 130, 3245-3267.
• Sorbjan, Z. (1996), Effects caused by varying the strength of the capping inversion based on a large eddy simulation model of the shear-free convective boundary layer, J. Atmos. Sci. 53, 2015-2024.
• Sorbjan, Z. (2004), Large-eddy simulations of the baroclinic mixed layer, Bound.-Layer Meteor. 112, 57-80.
• Sorbjan, Z. (2007), A numerical study of daily transitions in the convective boundary layer, Bound.-Layer Meteor. (submitted).
• Stull, R.B. (1988), An Introduction to Boundary Layer Meteorology, Dordrecht, Kluwer Academic, 666 p.
• Tjernstrom, M., and A.-S. Smedman (1993), The vertical turbulence structure of the coastal marine atmospheric boundary layer, J. Geophys. Res. 98, 4809-4826.
• Vickers, D., and L. Mahrt (2004), Evaluating formulations of stable boundary layer height, J. Appl. Meteor. 43, 1736-1749.
• Vickers, D., L. Mahrt, J. Sun, and T.L. Crawford (2001), Structure of offshore flow, Mon. Weather Rev. 129, 1251-1258.
• Wyngaard, J.C. (1983), Lectures on the planetary boundary layer. In: D.K. Lilly and T. Gal-Chen (eds.), Mesoscale meteorology - theories, observations, and models, D. Reidel, Dordrecht, 603-650.