[HTML][HTML] An immersed boundary method for the weather research and forecasting model

KA Lundquist, FK Chow… - Monthly Weather …, 2010 - journals.ametsoc.org
An Immersed Boundary Method for the Weather Research and Forecasting Model in:
Monthly Weather Review Volume 138 Issue 3 (2010) Jump to Content Jump to Main …

[图书][B] Immersed boundary methods for high-resolution simulation of atmospheric boundary-layer flow over complex terrain

KA Lundquist - 2010 - search.proquest.com
Mesoscale models, such as the Weather Research and Forecasting (WRF) model, are
increasingly used for high resolution simulations, particularly in complex terrain, but errors …

Mesoscale and large-eddy simulations for wind energy

N Marjanovic - 2011 - osti.gov
Operational wind power forecasting, turbine micrositing, and turbine design require high-
resolution simulations of atmospheric flow over complex terrain. The use of both Reynolds …

Enhanced method for multiscale wind simulations over complex terrain for wind resource assessment

A Flores-Maradiaga, R Benoit… - Journal of Physics …, 2016 - iopscience.iop.org
Due to the natural variability of the wind, it is necessary to conduct thorough wind resource
assessments to determine how much energy can be extracted at a given site. Lately …

Review of wind energy forecasting methods for modeling ramping events

S Wharton, JK Lundquist, N Marjanovic, JL Williams… - 2011 - osti.gov
Tall onshore wind turbines, with hub heights between 80 m and 100 m, can extract large
amounts of energy from the atmosphere since they generally encounter higher wind speeds …

[PDF][PDF] Nested mesoscale to large-eddy simulations for wind energy applications

N Marjanovic, FK Chow… - The Fifth Int. Symposium on …, 2010 - 205.166.33.100
Wind turbine micrositing, operational wind power forecasting, and turbine design require
high-resolution simulations of atmospheric flow over complex terrain. We are developing …

[PDF][PDF] Figure A. 5–Coupes verticales de u/v/(en m2. s-2) aux résolutions 0.5 km (à gauche), 1 km (au centre) et 2 km (à droite) du flux de référence (a, b, c), issu de …

A Annexe - core.ac.uk
Figure A. 6–Coupes verticales du flux u/r/np (en g. kg-1. ms-1) pour les résolutions
horizontales de 0.5 km (à gauche), 1 km (au milieu) et 2 km (à droite) du flux de référence (a …

[HTML][HTML] Método mejorado de simulación multiescala del viento sobre terreno complejo para la evaluación del recurso eólico

A Flores-Maradiaga - Ingeniare. Revista chilena de ingeniería, 2016 - SciELO Chile
Debido a la variabilidad natural del viento y su fuerte dependencia en las condiciones
atmosféricas locales, es necesario realizar evaluaciones exhaustivas del recurso eólico …

[引用][C] Modélisation de la turbulence dans les nuages convectifs profonds aux résolutions kilométrique et hectométrique

A Verrelle - 2015