Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Wensong Weng"'
Autor:
Yongsheng Chen, Soudeh Afsharian, George A. Isaac, Zheqi Chen, Wensong Weng, Terry Bullock, Peter A. Taylor, Li Cheng
There have been many studies of marine fog, some using WRF and other models. Several model studies report over-predictions of near surface liquid water content (Qc) leading to visibility estimates that are too low. This study has found the same. One
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::97c57d80bacd187561ec918252c87f0a
https://acp.copernicus.org/preprints/acp-2021-344/
https://acp.copernicus.org/preprints/acp-2021-344/
Autor:
Khalid Malik, Peter A. Taylor, Wensong Weng, Zheng Qi Wang, Shama Sharma, Mathew Corkum, Wayne K. Hocking
Publikováno v:
Atmosphere-Ocean. 55:1-11
Upper-level winds are primarily measured by tracking the position of radiosonde balloons as they rise through the atmosphere. Radiosondes are released from a global network at 0000 utc and 1200 utc each day, and data are quickly available to the worl
Autor:
Taylor, Peter A., Zheqi Chen, Li Cheng, Afsharian, Soudeh, Wensong Weng, Isaac, George A., Bullock, Terry W., Yongsheng Chen
Publikováno v:
Atmospheric Chemistry & Physics Discussions; 6/28/2021, p1-24, 24p
Publikováno v:
Journal of Wind Engineering and Industrial Aerodynamics. 98:121-132
Based on the 1-D planetary boundary layer model of Weng and Taylor with E – l turbulence closure, a 2-D numerical model is developed to study the atmospheric boundary-layer flow over single or multiple changes in surface conditions. These changes c
Publikováno v:
Boundary-Layer Meteorology. 125:305-328
A time and height dependent eddy diffusion model is used to investigate possible scenarios for the size distribution of dust in the lower atmosphere of Mars. The dust is assumed to either have been advected from a distant source or to have originated
Autor:
Peter A. Taylor, Wensong Weng
Publikováno v:
Boundary-Layer Meteorology. 118:305-323
The atmospheric boundary layer (ABL) model of Weng and Taylor with E−l turbulence closure is applied to simulate the one-dimensional stably stratified ABL. The model has been run for nine hours from specified initial wind, potential temperature and
Autor:
Wensong Weng1
Publikováno v:
Boundary-Layer Meteorology. Aug1998, Vol. 88 Issue 2, p333-340. 8p.
Autor:
F Freedman, Gunilla Svensson, Anton Beljaars, Jocelyn Mailhot, Veniamin Perov, Kuan-Man Xu, Guy Schayes, Robert J. Beare, A Cheng, David C. Lewellen, Michael Ek, Albert A. M. Holtslag, Gert-Jan Steeneveld, Geert Lenderink, Joan Cuxart, H. Kitagawa, Alan R. Kerstein, R Hamdi, Thorsten Mauritsen, Eric Bazile, Peter A. Taylor, L. Conangla, Scott Wunsch, Wensong Weng
Publikováno v:
Boundary-Layer Meteorology 118 (2006) 2
Boundary-Layer Meteorology, 118(2), 273-303
Boundary-Layer Meteorology, 118(2), 273-303
The parameterization of the stably stratified atmospheric boundary layer is a difficult issue, having a significant impact on medium-range weather forecasts and climate integrations. To pursue this further, a moderately stratified Arctic case is simu
Autor:
Peter A. Taylor, Wensong Weng
Publikováno v:
Boundary-Layer Meteorology. 107:371-400
Several commonly used turbulence closure schemes forthe atmospheric boundarylayer (ABL) are applied to simulate neutral, nocturnal and diurnal cyclesituations in a one-dimensional ABL. Results obtained with the differentschemes, E-l, E-e and its modi