高分辨湖泊沉积和孢粉记录对气候、水文变化的响应   总被引：4，自引：2，他引：2  

于革 《沉积学报》2011,29(1):118-124

通过对长江中游网湖钻孔高精度分层样品(1.5年/样品)的沉积学和孢粉学研究,试图揭示过去百年网湖在由开放到封闭体系变化中,沉积孢粉与气候、水文动力变化的过程及其相互关系.相关分析和低频滤波分析,反映出沉积物和孢粉的变化对流域降水和长江流量的敏感响应.在过去130年中的多雨洪水年份,湖泊受长江倒灌影响,沉积物以黏土细颗粒...  相似文献   

循环冻融条件下安山岩和花岗岩的物理力学特性试验研究   总被引：5，自引：0，他引：5  

刘华  牛富俊  徐志英  林战举  许健 《冰川冻土》2011,33(3):557-563

结合青藏铁路块石护坡路基处于青藏高原特殊的气候条件,对用于青藏铁路护坡的两种主要岩石（花岗岩和安山岩）进行循环冻融试验.结果表明:两种岩石在经历了数次冻融循环后都出现了微细裂纹;声波监测表明,超声波速同冻融循环周期呈指数下降关系,显示了冻融循环对岩石风化的影响以及循环后岩石物理力学参数变化的趋势.结果说明,花岗岩的冻融...  相似文献   

物理守恒律保真全球谱模式辐射—云—对流过程的改进   总被引：1，自引：0，他引：1  

钟琦  钟青  沈元芳 《气候与环境研究》2011,16(4):407-418

辐射—云一对流相互作用的正确和合理描述是改进湿物理过程描述和数值模式的重要方面.在一个物理守恒律保真的全球模式中引入描述更细致的云参数化方案和辐射参数化方案,对6个30天实时资料数值积分进行分析.结果表明,通过云参数化方案中云描述的细化,改进了模式对云分布、云量、以及云水、云冰不同相态的模拟;辐射方案中对这些云水物质的...  相似文献   

Tall building vibration control using a TM‐MR damper assembly: Experimental results and implementation     

Rene Zemp  Juan C. de la Llera  Paul Roschke 《地震工程与结构动力学》2011,40(3):257-271

This paper summarizes the relevant results of the design, construction, testing, and implementation of a nominal 120 kN magnetorheological damper developed to control a free‐plan tall building in Santiago, Chile, equipped with two 160‐ton tuned masses. Cyclic as well as hybrid simulation tests were performed on the prototype damper. Global building responses using measured MR properties showed good correlation with analytical estimations. Also, a proposed physical controller for the MR damper was validated through hybrid and building pull‐back tests. Its performance is essentially equivalent to that of an LQR controller, but the information needed in its implementation is considerably less. Pull‐back tests of 10 cm amplitude were performed on one mass along the flexible edge of the building and its response controlled using the passive and controlled modes of the MR damper. The MR damper was capable of controlling the TM displacements very effectively, as well as the simulated building response for different ground motions and harmonic excitation. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

Tall building vibration control using a TM‐MR damper assembly     

Rene Zemp  Juan C. de la Llera  José L. Almazán 《地震工程与结构动力学》2011,40(3):339-354

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Theoretical constraints to gully erosion research: time for a re‐evaluation of concepts and assumptions?     

Rafaello V. Bergonse  Eusébio J. Reis 《地球表面变化过程与地形》2011,36(11):1554-1557

Gullies are conceptualized in the literature as essentially fluvial forms with dimensional boundaries arbitrarily defined between rills and river channels. This notion is incompatible with the existing variability of form and process, as mass movements frequently exert a fundamental control on gully initiation and expansion, to the point of features outgrowing their original contributing area. The inability of a conceptual framework to incorporate existing observations inevitably constrains methodologies and research results. In this commentary, several examples of published results are contrasted with the prevailing assumption of an essentially fluvial nature, with the purpose of encouraging discussion on the need for a revised conceptual framework in gully erosion research. Copyright © 2011 John Wiley & Sons, Ltd.  相似文献   

Surface circulation downstream of the Point Arena upwelling center     

Christopher M. Halle  John L. Largier 《Continental Shelf Research》2011,31(12):1260-1272

Measurements from recently installed 5 MHz high-frequency radar (CODAR) stations south of Point Arena, California, are used to describe surface current patterns during the upwelling season (June-August 2007). The systems provide hourly current maps on a 5-km grid, covering a region from approximately 10 to 150 km offshore (the continental shelf into the deep ocean). These HF-radar observations provide an unprecedented view of circulation in this “coastal transition zone”, between the wind-driven circulation over the shelf and the California Current circulation offshore. Circulation patterns include: (1) bifurcation of the coastal upwelling jet downstream of Point Arena into an along-shelf (down-coast) branch and an offshore branch, and (2) a large-scale anticyclonic meander that often develops into an eddy-like recirculation south of the bifurcation. The “recirculation” feature extends well offshore, with surface currents 50-100 km from the coast consistently opposing the wind stress. The spatial and temporal evolution of the surface current features during upwelling events affects surface transport from Point Arena to areas in the south, increasing the travel time of a substantial fraction of newly upwelled water from a few days to roughly two weeks. Thus, surface currents even far offshore influence coastal transport of nutrients, phytoplankton and larvae on ecologically relevant timescales, with resultant connectivity patterns very different than implied by a simple examination of the mean flow.  相似文献   

冬季青藏高原大气热状况分析Ⅱ：年际变化   总被引：4，自引：3，他引：1  

宇婧婧  刘屹岷  吴国雄 《气象学报》2011,69(1):89-98

通过诊断3套再分析资料的非绝热加热场,研究冬季青藏高原上空大气的热力特征.结果表明,与夏季为强热源的特征不同,冬季高原上空不是欧亚大陆上最强的冷源中心.冬季高原上空整体是偏弱的冷源,在高原西侧及东南地区上空甚至出现非绝热加热正值区,这一分析对以往研究提出的高原是冷源的特性给出了修正.各种非绝热加热分量的诊断表明,冬季高原上空这种总的非绝热加热分布主要是由于高原主体的长波辐射冷却较周边地区弱,以及西侧至东南地区凝结潜热释放造成的.为了说明再分析的非绝热加热资料对冬季高原上空大气的这种热力特征描述的可信性,文中还利用了地表辐射能量、TRMM及PREC/L降水、垂直速度等资料进一步辅助分析,证实了由于高原位势较高造成大气整层温度偏低,向外长波辐射偏少,以及高原地势的隆起造成局地较强的上升运动,高原西侧至东南角降水大值区潜热偏大,最终造成高原上空总非绝热加热负值偏小.最后理想高原隆起的水球试验结果说明,冬季,高原的存在减弱了陆地上空的冷却效应,因而其上为弱冷源,再次证实了资料分析的结果.  相似文献   

The Impact of Soil Freezing/Thawing Processes on Water and Energy Balances     

ZHANG Xi  SUN Shufen 《大气科学进展》2011,28(1):169-177

A frozen soil parameterization coupling of thermal and hydrological processes is used to investigate how frozen soil processes affect water and energy balances in seasonal frozen soil. Simulation results of soil liquid water content and temperature using soil model with and without the inclusion of freezing and thawing processes are evaluated against observations at the Rosemount field station. By comparing the simulated water and heat fluxes of the two cases, the role of phase change processes in the water and energy balances is analyzed. Soil freezing induces upward water flow towards the freezing front and increases soil water content in the upper soil layer. In particular, soil ice obviously prevents and delays the infiltration during rain at Rosemount. In addition, soil freezingthawing processes alter the partitioning of surface energy fluxes and lead the soil to release more sensible heat into the atmosphere during freezing periods.  相似文献   

Impact of Cloud Microphysical Processes on the Simulation of Typhoon Rananim near Shore. Part II: Typhoon Intensity and Track          下载免费PDF全文

CHENG Rui  YU Rucong  XU Youping  FU Yunfei 《Acta Meteorologica Sinica》2011,25(4):456-466

The impact of cloud microphysical processes on the simulated intensity and track of Typhoon Rananim is discussed and analyzed in the second part of this study. The results indicate that when the cooling effect due to evaporation of rain water is excluded, the simulated 36-h maximum surface wind speed of Typhoon Rananim is about 7 m s⁻¹ greater than that from all other experiments; however, the typhoon landfall location has the biggest bias of about 150 km against the control experiment. The simulated strong outer rainbands and the vertical shear of the environmental flow are unfavorable for the deepening and maintenance of the typhoon and result in its intensity loss near the landfall. It is the cloud microphysical processes that strengthen and create the outer spiral rainbands, which then increase the local convergence away from the typhoon center and prevent more moisture and energy transport to the inner core of the typhoon. The developed outer rainbands are supposed to bring dry and cold air mass from the middle troposphere to the planetary boundary layer (PBL). The other branch of the cold airflow comes from the evaporation of rain water itself in the PBL while the droplets are falling. Thus, the cut-off of the warm and moist air to the inner core and the invasion of cold and dry air to the eyewall region are expected to bring about the intensity reduction of the modeled typhoon. Therefore, the deepening and maintenance of Typhoon Rananim during its landing are better simulated through the reduction of these two kinds of model errors.  相似文献