中文摘要：

四个自动气象学的车站从沙滩在一根线被建立到对 Bohai 海湾的西方海岸垂直的内陆。在 2 m， 4 m 和 12 m 的高度的风方向和速度与 10 极小的间隔被调查。在“海陆地微风(SLB ) ”上天，到陆地微风的从海微风的转变在学习区域是很明显的。海微风的方向从 ENE 和 E 对海岸并且主要基本上垂直。当它到达内陆，车站的距离改变到海岸线的海微风的持续时间，和近海岸的风速度比内陆和减少的大。比在阴暗的天有在阳光充足的天的 SLB 的增加的开发。术语“气候的沿海的地区”能为 SLB 影响的区域被定义，它在一典型 SLB 天到达超过 74 km 内陆但是在一非典型的 SLB 天的不到 10 km。

英文摘要：

Four automatic meteorological stations were set up in a line from beach to inland perpendicular to the west coast of Bohai Bay. Wind direction and velocity at altitudes of 2 m, 4 m and 12 m were surveyed with 10 minute intervals. On ＂Sea-Land Breeze＂ （SLB） days, the transition from sea breeze to land breeze was very evident in the study area. Direction of sea breeze was basically perpendicular to the coast and mainly from the ENE and E. Duration of sea breeze varied by the stations＇ distance to the coastline, and the near-coast wind velocity was larger than that of the inland and decreases as it reaches inland. There was increased development of SLB on sunny days than on overcast days. The term ＂Climatic Coastal Zone＂ can be defined for the area influenced by SLB, which reaches more than 74 km inland on a typical SLB day but less than 10 km on a non-typical SLB day.