摘要
对南岭地区乐昌站和乳源站1968—1998年31年的雾日气候资料进行了统计分析,对比分析发现,在背风坡雾产生的日数明显较多,即南岭地区存在显著的小地形背风坡雾现象。同时,利用CSU-RAMS中尺度数值模式进一步研究局地小地形背风坡雾的作用,模拟结果表明,小地形动力作用对背风坡雾有重要影响。
The climatic character of 31-year fog in Lechang and Ruyuan is statistically analyzed. The results show that the fog is considerably influenced by local micro-topography, and the day numbers of lee fog occurrence obviously increase. At the same time, by means of CSU-RAMS model, the effect of local micro-topography on lee side fog is further studied. The simulated results show that the dynamic function of micro-topography to lee side fog has important action, and the forming and developing of the lee side fog are to gain some dynamic profits from local micro-topography.
出处
《高原气象》
CSCD
北大核心
2004年第5期709-713,共5页
Plateau Meteorology
基金
国家自然科学基金"南岭山地浓雾的物理结构与能见度研究"(49975001)资助
关键词
局地小地形
背风坡雾
气候分析
数值模拟
Micro-topography
Lee side fog
Climatic analysis
Numerical simulation