Sensitivity of the regional climate model RegCM4.2 to planetary boundary layer parameterisation

2013 ◽  
Vol 43 (7-8) ◽  
pp. 1753-1772 ◽  
Author(s):  
Ivan Güttler ◽  
Čedo Branković ◽  
Travis A. O’Brien ◽  
Erika Coppola ◽  
Branko Grisogono ◽  
...  
Keyword(s):  
Boundary Layer ◽  
Regional Climate Model ◽  
Planetary Boundary Layer ◽  
Climate Model ◽  
Regional Climate

scholarly journals Influence of Sea Ice Treatment in a Regional Climate Model on Boundary Layer Values in the Fram Strait Region

2004 ◽  
Vol 132 (4) ◽  
pp. 985-999 ◽  
Author(s):  
Tido Semmler ◽  
Daniela Jacob ◽  
K. Heinke Schlünzen ◽  
Ralf Podzun
Keyword(s):  
Boundary Layer ◽  
Sea Ice ◽  
Regional Climate Model ◽  
Climate Model ◽  
Regional Climate ◽  
Fram Strait

scholarly journals The “urban meteorology island”: a multi-model ensemble analysis

2020 ◽  
Vol 20 (23) ◽  
pp. 15061-15077
Author(s):  
Jan Karlický ◽  
Peter Huszár ◽  
Tereza Nováková ◽  
Michal Belda ◽  
Filip Švábik ◽  
...  
Keyword(s):  
Boundary Layer ◽  
Wind Speed ◽  
Regional Climate Model ◽  
Cloud Cover ◽  
Climate Model ◽  
Regional Climate ◽  
Meteorological Variables ◽  
Layer Height ◽  
Boundary Layer Height ◽  
Induced Changes

Abstract. Cities and urban areas are well-known for their impact on meteorological variables and thereby modification of the local climate. Our study aims to generalize the urban-induced changes in specific meteorological variables by introducing a single phenomenon – the urban meteorology island (UMI). A wide ensemble of 24 model simulations with the Weather Research and Forecasting (WRF) regional climate model and the Regional Climate Model (RegCM) on a European domain with 9 km horizontal resolution were performed to investigate various urban-induced modifications as individual components of the UMI. The results show that such an approach is meaningful, because in nearly all meteorological variables considered, statistically significant changes occur in cities. Besides previously documented urban-induced changes in temperature, wind speed and boundary-layer height, the study is also focused on changes in cloud cover, precipitation and humidity. An increase in cloud cover in cities, together with a higher amount of sub-grid-scale precipitation, is detected on summer afternoons. Specific humidity is significantly lower in cities. Further, the study shows that different models and parameterizations can have a strong impact on discussed components of the UMI. Multi-layer urban schemes with anthropogenic heat considered increase winter temperatures by more than 2 ∘C and reduce wind speed more strongly than other urban models. The selection of the planetary-boundary-layer scheme also influences the urban wind speed reduction, as well as the boundary-layer height, to the greatest extent. Finally, urban changes in cloud cover and precipitation are mostly sensitive to the parameterization of convection.

scholarly journals Regional climate model assessment of the urban land-surface forcing over central Europe

2014 ◽  
Vol 14 (12) ◽  
pp. 18541-18589 ◽  
Author(s):  
P. Huszar ◽  
T. Halenka ◽  
M. Belda ◽  
M. Zak ◽  
K. Sindelarova ◽  
...  
Keyword(s):  
Boundary Layer ◽  
Regional Climate Model ◽  
Central Europe ◽  
Climate Model ◽  
Regional Climate ◽  
Urban Canopy ◽  
Anthropogenic Heat ◽  
Model Assessment ◽  
Layer Height ◽  
Boundary Layer Height

Abstract. For the purpose of qualifying and quantifying the climate impact of cities and urban surfaces in general on climate of central Europe, the surface parameterization in regional climate model RegCM4 has been extended with the Single Layer Urban Canopy Model (SLUCM). A set of experiments was performed over the period of 2005–2009 for central Europe, either without considering urban surfaces or with the SLUCM treatment. Results show a statistically significant impact of urbanized surfaces on temperature (up to 1.5 K increase in summer) as well as on the boundary layer height (increases up to 50 m). Urbanization further influences surface wind with a winter decrease up to −0.6 m s−1, though both increases and decreases were detected in summer depending on the location relative to the cities and daytime (changes up to 0.3 m s−1). Urban surfaces significantly reduce evaporation and thus the humidity over the surface. This impacts the simulated summer precipitation rate, showing decrease over cities up to −2 mm day−1. Significant temperature increases are simulated over higher elevations as well, not only within the urban canopy layer. With the urban parameterization, the climate model better describes the diurnal temperature variation, reducing the cold afternoon and evening bias of RegCM4. Sensitivity experiments were carried out to quantify the response of the meteorological conditions to changes in the parameters specific to the urban environment such as street width, building height, albedo of the roofs and anthropogenic heat release. The results proved to be rather robust and the choice of the key SLUCM parameters impacts them only slightly (mainly temperature, boundary layer height and wind velocity). Statistically significant impacts are modeled not only over large urbanized areas, but the influence of the cities is also evident over rural areas without major urban surfaces. It is shown that this is the result of the combined effect of the distant influence of the cities and the influence of the minor local urban surface coverage.

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