The Effect of Changes of Urban Surfaces on Rainfall Phenomenon as Determined by a Non-Hydrostatic Mesoscale Model
スポンサーリンク
概要
- 論文の詳細を見る
A non-hydrostatic, mesoscale model, LOCALS, is used to investigate the effect of land surface changes on precipitation in an urban area. The horizontal mesh used in the model is approximately 5km and the domain includes Tokyo and central Japan. Land surfaces identified as pavement or urban are transformed into forested land and model simulations are performed for both the current urban land surface and the hypothetical forested land surface. Detailed analysis is performed for two sample cases. On 5 August 2003, increased heating by the urban surfaces increases the height of the urban boundary layer resulting in much more rainfall. On 25 July 2001, air that is advected over Tokyo but forms a precipitating cloud away from the urban core carries less moisture and therefore produces less rainfall. These case studies suggest that changes to land surface types in urban areas may increase or decrease rainfall in the urban area and further research is necessary before it is possible to generalize these results.
- 社団法人日本気象学会の論文
- 2008-10-25
著者
関連論文
- NUMERICAL ANALYSIS OF HEAT ISLAND PHENOMENA FOR THE CONTROL OF COOLING ENERGY IN CITIES
- A Turbulent Closure Model for the Urban Area
- Wind tunnel test of air flow and temperature field around a rectangular building
- Utilization of porous pavement for the improvement of summer urban climate
- Climate analysis for urban planning in Tokyo
- Analysis the Thermal Environment and Wild Field at the District Scale Based on a LES Model
- The Effect of Changes of Urban Surfaces on Rainfall Phenomenon as Determined by a Non-Hydrostatic Mesoscale Model