海陆风,sea-land breeze
1)sea-land breeze海陆风
1.Some characteristics of sea-land breeze circulation over the coat of Hangzhou Bay;杭州湾沿岸海陆风环流的若干特征
2.Numerical simulation of three dimensional structure of sea-land breeze at west coast of Liao Dong Bay辽东湾西岸三维海陆风特征的数值模拟
3.Based on the boundary layer meteorological sounding and automatic meteorological station s data of Xinken on the west coast of the Pearl River mouth in October 2004,the characteristics of the sea-land breeze are studied.根据2004年10月在珠江口西岸新垦观测的大气边界层探测资料和自动气象站资料,研究了珠江口西岸海陆风特征。
英文短句/例句

1.Observation Results and Characteristic Analysis of the Sea-Land Breeze over Ningde Coastal Region in Fujian福建宁德沿海海陆风观测结果及特征分析
2.Ionic Species Correlation Analysis of Particulate Matter at Inland and Offshore Sites in South Taiwan--Effect of Sea-land Breeze and Northeastern Monsoon台湾南部陆地及海面悬浮微粒中水溶性离子相关性分析——海陆风及东北季风的影响
3.The characteristics of land and sea breezes in different background conditions in Qingdao Olympic sailing venue青岛奥帆赛场不同背景条件下的海陆风特征
4.Numerical simulation of three dimensional structure of sea-land breeze at west coast of Liao Dong Bay辽东湾西岸三维海陆风特征的数值模拟
5.EFFECTS OF URBANIZATION ON LAND-SEA BREEZE OF GUANGXI IN SUMMER: WRF SIMULATION STUDY城市化对广西夏季海陆风影响的数值试验
6.(of winds) coming from the sea toward the land.(指风)来自大海吹向内陆。
7.On summer days coastal regions often experience onshore winds which at night are replaced by offshore winds.夏天,沿海地区经常白天刮海风,晚上刮陆风。
8.The storm blew fiercely over land and sea.暴风雨猛烈地吹过陆地和海面。
9.sea-breeze(.breeze blowing from the sea towards the land,esp during the day)海风(尤指白天刮向内陆的).
10.Overall Soft Landing Installation of Offshore Wind Turbine海上风力发电机组的整体软着陆安装
11.The basic reason is the same for a sea breeze as for a monsoon--difference in heating between the land and sea.形成海风的基本原因与形成季风的相同———都是由海陆加热差异造成。
12.Comparison between Continental Shelf Aeolian Residues and Coastal Palaeo Aeolian Sediments in Northern South China Sea南海北部大陆架残留风成沙与海岸带古风成沙的对比及关系研究
13.Relationship of Land-Sea Thermodynamic Anomaly and East Asian Summer Subtropic Monsoon;海陆热状况异常与东亚夏季副热带季风的关联
14.Study on Wind-induced Turbulent Mixing on the South China Sea Shelf and Long-term Mixing Observation南海陆架坡风致混合及长期混合观测方法研究
15.Most dangerous is the storm surge, a wall of water that sweeps across the coastline where hurricane makes landfall.最危险的是风暴潮,它会在飓风登陆处形成一道水墙,横扫海岸线。
16.Winds with continental provenances frequently have a higher dust content than those with maritime provenances.来自大陆的风比来自海洋的风通常具有更高的尘埃含量。
17.ASIAN-AUSTRALIAN MONSOON TROUGHS AND MONSOON PRECIPITATION INFLUENCED BY REGIONAL LAND-SEA HEATING CONTRASTS亚洲-澳大利亚海陆地形与热力季节演变下的季风槽和季风降水
18.NUMERICAL SIMULATION EXPERIMENTS OF THE IMPACTS OF LOCAL SEA-LAND THERMODYNAMIC CONTRASTS ON THE SCS SUMMER MONSOON ONSET局地海陆热力对比对南海夏季风爆发影响的数值试验
相关短句/例句

sea and land breezes海陆风
1.By using a three dimensional meso-scale meteorological model based on the hydrostatic equilibrium which is modified to indude the effect of abrupt terrain, the daily evolution and three dimensional structure of sea and land breezes over Qingdao area are simulated.本文采用 1个陡地形影响修正的三维中尺度流体静力的气象学模式 ,对青岛地区海陆风的日变化规律和三维结构进行了较细致的分析。
2.The sea and land breezes over Hong Kong on 28 September 2004 was investigated with mesoscale model MM5.利用MM5模式对香港地区的海陆风进行了显式数值研究,模拟的风向、风速和温度与站点的观测值比较一致,较详细地分析了海陆风的日变化规律和三维结构特征,结果显示香港地区海风分布复杂,主要受偏西、偏南和偏东海风气流的影响,形成多个辐合带,海风锋最远可以深入内陆约90km;陆风较简单,主要是偏北气流,陆风的风速和强度都比海风要弱,与山谷风、城市热岛环流等形成弱的辐合。
3)sea and land breeze海陆风
1.Analysis of the data observed from two automatic weather stations showed that the near surface wind field on the ice sheet was dominated by katabatic wind,while at seaboard a distinct feature is that this area was controlled by katabatic wind and sea and land breeze alternatively.自动气象站(Automatic Weather Station,AWS)观测数据的统计分析结果表明,夏季该地区冰盖上的近表面风场主要是由下降风控制,而沿海地区的风场则由于海陆热力学性质的差异呈现出冰盖下降风与局地海陆风交互作用的特点。
4)land sea wind海/陆风
5)wind speed on land and sea海陆风速
6)land-sea breeze陆海风
延伸阅读

海陆风海陆风seabreezeandlandbreeze在海岸附近昼夜间风向发生反向转变的风系。白天风从海上吹向陆地,称为海风,夜晚风从陆地吹向海洋,称为陆风,合称为海陆风。白天,地表受太阳辐射而增温,由于陆地土壤热容量比海水热容量小得多,陆地升温比海洋快得多,因此陆地上的气温显著地比附近海洋上的气温高。陆地上空气柱因受热膨胀,在水平气压梯度力的作用下,上空的空气从陆地流向海洋,然后下沉至低空,又由海面流向陆地,再度上升,遂形成低层海风和铅直剖面上的海风环流。海风从每天上午开始到傍晚,风力以下午为最强。日落以后,陆地降温比海洋快;到了夜间,海上气温高于陆地,就出现与白天相反的热力环流而形成低层陆风和铅直剖面上的陆风环流。海陆的温差,白天大于夜晚,所以海风较陆风强。海陆风在靠近海岸地区最强,距海岸愈远风愈弱。在较大湖泊的湖陆交界地,也可产生和海陆风环流相似的湖陆风。