Selection of environmental conditions for nearshore structure design     

DONGSheng GANBuhong HAOXiaoli 《中国海洋大学学报(英文版)》2004,3(1):111-114

1　Introduction　InChina ,coastalcitiesaremostlyregionaleconomicdevelopmentcenters.Becauseoftheirspecialgeogra phiclocations ,typhoonsandassociatedstormsurgescauseheavylossesoflivesandproperties.In 1 992 Qing daowasfloodedduetothecoincidenceoftheastrono m…  相似文献   

建筑结构抗震研究若干基本问题概述及讨论   总被引：3，自引：1，他引：2  

孙景江 《震灾防御技术》2006,1(2):87-96

本文介绍和讨论了结构抗震研究中的一些基本问题,包括地震反应分析选择地面运动输入应注意的问题,高层结构地震模拟试验问题和结构地震反应分析中的主要分析方法和存在的问题,最后简要介绍了目前常用结构反应分析程序。  相似文献   

Instabilities of the tidally induced bottom boundary layer in the rotating frame and their mixing effect     

K. Sakamoto  K. Akitomo 《Dynamics of Atmospheres and Oceans》2006,41(3-4):191-211

To investigate the stability of the bottom boundary layer induced by tidal flow (oscillating flow) in a rotating frame, numerical experiments have been carried out with a two-dimensional non-hydrostatic model. Under homogeneous conditions three types of instability are found depending on the temporal Rossby number Ro_t, the ratio of the inertial and tidal periods. When Ro_t < 0.9 (subinertial range), the Ekman type I instability occurs because the effect of rotation is dominant though the flow becomes more stable than the steady Ekman flow with increasing Ro_t. When Ro_t > 1.1 (superinertial range), the Stokes layer instability is excited as in the absence of rotation. When 0.9 < Ro_t < 1.1 (near-inertial range), the Ekman type I or type II instability appears as in the steady Ekman layer. Being much thickened (100 m), the boundary layer becomes unstable even if tidal flow is weak (5 cm/s). The large vertical scale enhances the contribution of the Coriolis effect to destabilization, so that the type II instability tends to appear when Ro_t > 1.0. However, when Ro_t < 1.0, the type I instability rather than the type II instability appears because the downward phase change of tidal flow acts to suppress the latter. To evaluate the mixing effect of these instabilities, some experiments have been executed under a weak stratification peculiar to polar oceans (the buoyancy frequency N²  10⁻⁶ s⁻²). Strong mixing occurs in the subinertial and near-inertial ranges such that tracer is well mixed in the boundary layer and an apparent diffusivity there is evaluated at 150–300 cm²/s. This suggests that effective mixing due to these instabilities may play an important role in determining the properties of dense shelf water in the polar regions.  相似文献   

DInSAR技术对不同方位形变的敏感性研究   总被引：3，自引：1，他引：2  

查显杰  傅容珊  戴志阳 《测绘学报》2006,35(2):133-137

以DEM数据为假想的地面目标,只考虑距离对相位的影响,模拟竖直向、距离向和方位向形变的干涉纹图,从而研究DInSAR技术对空间不同方位形变的敏感性。在所有模拟参数和形变位移大小都相同的情况下,三个不同方位形变所产生的相位从0到2π变化的完整干涉环的数目是各不相同的,揭示DInSAR技术对不同方位地表形变的敏感性存在差异,且敏感性由大到小依次为:竖直向、距离向和方位向。  相似文献   

《海洋数值模拟》课程建设的探索     

吕海滨 《地理空间信息》2012,10(6):170-171,16

《海洋数值模拟》是淮海工学院面向海洋技术专业本科生开设的专业选修课程。以培养海洋科学专业学生的数值模拟技能为目标,以研究海洋环境动力机制为导向,研究了《海洋数值模拟》课程的教学案例,提出了关于该课程建设上的思考,教学实践表明,学生的基本技能得到明显提高,学习兴趣普遍增强。  相似文献   

自然降雨条件下不同生态措施坡地的径流数值模拟     

李新虎  赵成义  杨洁 《山地学报》2012,(1):10-15

从动量定理和水量平衡原理出发,以Saint Venant方程为基础推导出自然降雨条件下不同生态措施(即同时考虑变雨强、降雨动量和不同生态措施影响下的坡地径流过程)坡地的径流基本方程。在考虑一般问题定解条件的基础上,采用Preissmann隐式格式对模型进行数值求解。利用3个处理(裸地、百喜草覆盖和百喜草+果树覆盖)、5组实测资料(不同雨型)对模型进行了验证,结果表明3个处理的计算值与实测值的平均相对误差分别为:14.97%、13.59%、15.15%,说明模型的计算结果是可靠的,对于模拟预测自然降雨条件下不同生态措施坡地径流过程是可行的。  相似文献   

Snow water equivalent over Eurasia in the next 50 years projected by aggregated CMIP3 models     

LiJuan M  Yong Luo  DaHe Qin 《寒旱区科学》2012,4(2):0093-0106

Based on remote sensing snow water equivalent (SWE) data, the simulated SWE in 20C3M experiments from 14 models attending the third phase of the Coupled Models for Inter-comparison Project (CMIP3) was first evaluated by computing the different percentage, spatial correlation coefficient, and standard deviation of biases during 1979–2000. Then, the diagnosed ten models that performed better simulation in Eurasian SWE were aggregated by arithmetic mean to project the changes of Eurasian SWE in 2002–2060. Results show that SWE will decrease significantly for Eurasia as a whole in the next 50 years. Spatially, significant decreasing trends dominate Eurasia except for significant increase in the northeastern part. Seasonally, decreasing proportion will be greatest in summer indicating that snow cover in warmer seasons is more sensitive to climate warming. However, absolute decreasing trends are not the greatest in winter, but in spring. This is caused by the greater magnitude of negative trends, but smaller positive trends in spring than in winter. The changing characteristics of increasing in eastern Eurasia and decreasing in western Eurasia and over the Qinghai-Tibetan Plateau favor the viewpoint that there will be more rainfall in North China and less in the middle and lower reaches of the Yangtze River in summer. Additionally, the decreasing rate and extent with significant decreasing trends under SRES A2 are greater than those under SRES B1, indicating that the emission of greenhouse gases (GHG) will speed up the decreasing rate of snow cover both temporally and spatially. It is crucial to control the discharge of GHG emissions for mitigating the disappearance of snow cover over Eurasia.  相似文献   

基于情景模拟的天津市滨海新区2020年暴雨内涝风险评估   总被引：4，自引：0，他引：4  

胡蓓蓓  周俊  王军  许世远  孟伟庆 《地理科学》2012,(7):846-852

基于多灾种复合动态风险评估理论,依据滨海新区2020年人口规划、土地利用规划以及社会经济发展计划,根据地面沉降和海平面上升预测结果设计了最不利、适中和最理想化三种情景;在此基础上,自行开发了基于GIS的洪水淹没区计算模块,模拟计算不同重现期暴雨内涝的淹没范围、淹没深度及淹没损失。结果表明:2020年,发生1 000 a一遇、200 a一遇和50 a一遇暴雨时,在最不利的情景一下:天津市滨海新区分别将有32.73%,29.34%和26.01%的土地不同程度受淹,受淹人口分别为338万、305万和264万,淹没损失分别达220.89亿元、181.39亿元和139.12亿元。  相似文献   

库姆塔格沙漠春季近地面风场、温度场特征   总被引：1，自引：1，他引：0  

吕萍  董治宝 《中国沙漠》2012,32(2):442-446

 利用中尺度区域预报模式系统对库姆塔格沙漠及其周边地区春季近地层风场与温度场分布特征进行了模拟和分析。结果发现,受青藏高原地形影响,偏北气流向南运行在途经库姆塔格沙漠的过程中发生3个分支:①在沙漠东部气流逐渐转变为西北风吹向甘肃省;②中西部气流以较强的东北风流向塔克拉玛干沙漠;③另一部分气流继续顺势南下流入青海省。沙漠区域温度从北向南逐渐降低,在青海省的边界上出现一个低温带,然后温度又开始增加。  相似文献   

近540 a东亚夏季海平面气压场的重建及其与数值模拟的比较   总被引：1，自引：0，他引：1  

李茜  魏凤英  李栋梁 《中国沙漠》2012,32(4):1017-1024

 基于中国东部地区旱涝分布和东亚夏季海平面气压存在密切关系的基础上,利用1470—2008年中国东部地区旱涝等级资料、1850—2008年东亚夏季海平面气压资料,运用主成分回归的方法重建了1470—2008年的东亚地区夏季海平面气压场,并对重建结果进行了检验,同时对1470—2008年东亚夏季海平面气压重建场和FGOALS_gl数值模式模拟的海平面气压场进行了对比分析。结果表明:①1850—2008年重建的东亚夏季海平面气压场在东亚夏季风关键区（中国内陆地区以及西北太平洋部分地区）重建效果相对于其他地区要好。②1470—2008年重建的东亚夏季海平面气压场主要存在高纬与中纬气压差异、海洋与陆地差异的两种空间分布型;1470—1999年FGOALS_gl数值模拟的东亚夏季海平面气压主要体现了海陆气压差异。③根据重建的东亚夏季海平面气压场定义的1470—2008年东亚夏季风指数的演变具有明显的阶段性,16世纪中期到17世纪初东亚夏季风偏强,17世纪偏弱,18世纪经历了“弱-强-弱-强-弱”的变化,19世纪则是“强-弱-强-弱”的变化,20世纪是明显的“弱-强-弱”变化。而1470—1999年数值模拟的东亚夏季风指数序列与重建序列的主要差异出现在16世纪末和18世纪末,两者的变化趋势相反,其他时段的变化趋势基本一致。  相似文献