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作 者:姜有山 王桂臣[2] 李进喜[3] 张榕[2] 张红华[2]
机构地区:[1]南京市气象局,南京210009 [2]连云港市气象局,江苏连云港222006 [3]江苏省气象台,南京210008
出 处:《气象科学》2011年第6期770-776,共7页Journal of the Meteorological Sciences
基 金:江苏省连云港市科学技术局项目(SH0719)
摘 要:通过对海州湾沿岸3座梯度测风塔和19座自动气象站一年的逐日24 h自记风资料的统计,得到海州湾沿岸的海陆风,在此基础上提出了海陆风"净值"的概念。结合海陆风"净值"分析海州湾沿岸的海陆风环流特征发现:海州湾沿岸南北两段的海陆风具有明显的差异,南北走向的海岸海陆风比西北—东南走向海岸的弱,且转换时间迟;并粗略地估计了海风向陆地内的水平伸展宽度在45 km左右,夏季海风的垂直伸展高度可达625 m或以上。Abstract Using the daily 24-h wind datasets, which are derived from 3 gradient anemometer towers and 19 automatic meteorological stations, we investigated the land-sea breeze in the coastwise area of Haizhou Bay and proposed the concept of net value of land-sea breeze. Combined with the net value anal- ysis of land-sea breeze circulation in the coast, it was demonstrated that the land-sea breeze in the southand north coasts exhibited significant differences: the land-sea breeze in the north-south coast was weaker than that in the northwest-southeast coast, and it had a later conversion time. The horizontal extension of sea-breeze towards land area was about 45 km. In summer, the vertical extension height could reach 625 m or above.
分 类 号:P463.1[天文地球—大气科学及气象学]
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