Exchange processes in the atmospheric boundary layer over mountainous terrain

S Serafin, B Adler, J Cuxart, SFJ De Wekker, A Gohm… - Atmosphere, 2018 - mdpi.com
The exchange of heat, momentum, and mass in the atmosphere over mountainous terrain is
controlled by synoptic-scale dynamics, thermally driven mesoscale circulations, and …

Diurnal mountain wind systems

D Zardi, CD Whiteman - … research and forecasting: Recent progress and …, 2012 - Springer
Diurnal mountain wind systems are local thermally driven wind systems that form over
mountainous terrain and are produced by the buoyancy effects associated with the diurnal …

Severe convective storms—An overview

CA Doswell III - Severe convective storms, 2001 - Springer
In general, convection refers to the transport of some property by fluid movement, most often
with reference to heat transport. As such, it is one of the three main processes by which heat …

Fluid dynamics of urban atmospheres in complex terrain

HJS Fernando - Annual review of fluid mechanics, 2010 - annualreviews.org
A majority of the world's urban centers are located in complex terrain, in which local airflow
patterns are driven by pressure gradients and thermal forcing, while being strongly …

A review of recent advances in understanding the mesoand microscale properties of the severe Bora wind

B Grisogono, D BelusŠIĆ - Tellus A: Dynamic Meteorology and …, 2009 - Taylor & Francis
A gusty downslope windstorm that blows at the eastern Adriatic coast is called bora. Similar
winds exist at many other places on virtually all continents. Related hourly mean wind …

[HTML][HTML] Mechanisms of up-valley winds

G Rampanelli, D Zardi… - Journal of the atmospheric …, 2004 - journals.ametsoc.org
Mechanisms of Up-Valley Winds in: Journal of the Atmospheric Sciences Volume 61 Issue
24 (2004) Jump to Content Logo Logo Logo Logo Logo Logo JOURNALS Artificial …

The influence of topography on meteorogical variables and surface-atmosphere interactions

MR Raupach, JJ Finnigan - Journal of Hydrology, 1997 - Elsevier
Topography perturbs practically every process and variable relevant to land-atmosphere
interactions, including radiation, air temperature and saturation deficit, wind and turbulence …

Structure of turbulence in katabatic flows below and above the wind-speed maximum

AA Grachev, LS Leo, SD Sabatino… - Boundary-layer …, 2016 - Springer
Measurements of small-scale turbulence made in the atmospheric boundary layer over
complex terrain during the Mountain Terrain Atmospheric Modeling and Observations …

[HTML][HTML] Long-term simulations of thermally driven flows and orographic convection at convection-parameterizing and cloud-resolving resolutions

W Langhans, J Schmidli, O Fuhrer… - Journal of Applied …, 2013 - journals.ametsoc.org
Long-Term Simulations of Thermally Driven Flows and Orographic Convection at
Convection-Parameterizing and Cloud-Resolving Resolutions in: Journal of Applied …

[HTML][HTML] Observed and WRF-simulated low-level winds in a high-ozone episode during the Central California Ozone Study

JW Bao, SA Michelson, POG Persson… - Journal of Applied …, 2008 - journals.ametsoc.org
Observed and WRF-Simulated Low-Level Winds in a High-Ozone Episode during the Central
California Ozone Study in: Journal of Applied Meteorology and Climatology Volume 47 Issue 9 …