北太平洋海温与次年盛夏副热带高压的遥相关响应     

李德萍  孙正  郭丽娜  董海鹰 《山东气象》2007,27(3):6-9

选取1952-2005年北太平洋月平均海表温度（SST）资料，经过奇异值分解分析表明：6月份日界线附近西风漂流区的海温集中了北太平洋海温场的主要信息，西风漂流区与赤道冷水区的海温存在遥相关震荡，并且在6月份达到全年的最高值，11月份其振幅出现次高值。6月西风漂流区的海温（SST）可视为来年盛夏（7-8月）西太平洋副热带高压的强弱变化的信号：当6月份西风漂流区的海温（SST）偏低，则来年盛夏西太平洋副热带高压偏强；反之，则来年盛夏西太平洋副热带高压偏弱。  相似文献   

无线传感器网络中基于时钟漂移补偿的时间同步技术   总被引：4，自引：0，他引：4  

刘迪忻 《时间频率学报》2009,32(2):120-128

在分析和总结现有时间同步算法的特点及其存在问题的基础上,提出了一种在无线传感器网络的时间同步协议（TPSN）中同时考虑节点时钟偏移和频率漂移率的改进算法。该算法利用连续两次同步过程中所记录的时间信息来估算节点时钟的偏移和频率漂移率,并进行补偿。同传统算法相比,此算法通讯成本较低、精度较高。最后通过数学分析和仿真的方法对所提出的改进算法进行了验证。  相似文献   

The Enya mounds: a lost mound-drift competition     

D. Van Rooij  V. A. I. Huvenne  D. Blamart  J.-P. Henriet  A. Wheeler  H. de Haas 《International Journal of Earth Sciences》2009,98(4):849-863

The genesis and evolution of cold-water coral banks along the Northeastern Atlantic margin is known to be influenced by several factors, among which the palaeotopography and nature of the coral settling surface, the presence of bottom currents and sediment supply. In this paper, a case study is presented of the Enya mound cluster, located in the southernmost tip of the Belgica mound province, west of Ireland. Below this mound cluster, seismic stratigraphy revealed a yet unmapped local unconformity RD1b, being part of a composite erosion event (RD1). As such, from the Late Miocene to Late Pliocene, at least two erosional events have incised the margin, ending with the final RD1a “moundbase” unconformity, acting as a base for the Enya mounds. During the Quaternary the mounds became outgrown and were covered by a mounded contourite drift. In addition, they are closely associated with a cluster of seabed pockmarks. The bottom current regime which became active since the Middle Pleistocene has certainly influenced the fate of this mound cluster. The occurrence of the pockmarks seems to be related to relatively recent fluid migration processes, however leaving an open question if any previous seepage phases were involved in the growth or initiation of the coral banks.  相似文献   

FY-2C云迹风资料在中尺度数值模式中的应用研究   总被引：6，自引：1，他引：5  

李华宏  王曼  薛纪善  杞明辉 《气象学报》2008,66(1):50-58

利用探空观测资料对FY-2C云迹风资料进行统计检验和误差分析,并针对其误差特征进行偏差订正和热成风原理两种方法的质量控制.然后通过GRAPES-3Dvar同化到GRAPES-Meso模式中,对2005年7月1日00时至7月2日00时发生在中国西北部的一次暴雨过程进行了数值对比试验.结果表明:云迹风数量在垂直方向上主要集中分布于500 hPa以上的对流层中高层,在250 hPa附近数量分布概率最大;高度在500 hPa以下云迹风存在明显的风向误差和很大的风速误差,而且误差分布发散,可用性较差.500 hPa以上层次的云迹风误差较小,且误差分布呈高斯分布具有一定的系统特性,可用性较好;通过质量控制后,可以把风向错误或风速偏差太大的云迹风予以剔除,进一步提高云迹风的精度;同化云迹风资料后,在暴雨区附近初始风场低层的西南气流明显加强,有利于暴雨区水汽输送和水汽辐合,最终能很好地改善24 h暴雨预报的强度和落区.  相似文献   

Wave-influenced deltas: geomorphological implications for facies reconstruction   总被引：5，自引：0，他引：5  

Janok P. Bhattacharya  Liviu Giosan† 《Sedimentology》2003,50(1):187-210

ABSTRACT A process‐based facies model for asymmetric wave‐influenced deltas predicts significant river‐borne muds with potentially lower quality reservoir facies in prodelta and downdrift areas, and better quality sand in updrift areas. Many ancient barrier‐lagoon systems and ‘offshore bars’ may be better reinterpreted as components of large‐scale asymmetric wave‐influenced deltaic systems. The proposed model is based on a re‐evaluation of several modern examples. An asymmetry index A is defined as the ratio between the net longshore transport rate at the mouth (in m³ year^?1) and river discharge (in 10⁶ m³ month^?1). Symmetry is favoured in deltas with an index below ≈ 200 (e.g. Tiber, lobes of the Godavari delta, Rosetta lobe of the Nile, Ebro), whereas deltas with a higher index are asymmetric (e.g. Danube – Sf. Gheorghe lobe, Brazos, Damietta lobe of the Nile). Periodic deflection of the river mouth for significant distances in the downdrift direction occurs in extreme cases of littoral drift dominance (e.g. Mahanadi), resulting in a series of randomly distributed, quasi‐parallel series of sand spits and channel fills. Asymmetric deltas show variable proportions of river‐, wave‐ and tide‐dominated facies both among and within their lobes. Bayhead deltas, lagoons and barrier islands form naturally in prograding asymmetric deltas and are not necessarily associated with transgressive systems. This complexity underlines the necessity of interpreting ancient depositional systems in a larger palaeogeographic context.  相似文献   

RC框架结构薄弱层的层间位移可靠度水平考察   总被引：2，自引：0，他引：2  

吴波  李艺华 《地震工程与工程振动》2003,23(6):103-108

讨论了钢筋混凝土框架结构层间极限变形角的近似概率特性,考察了大震作用下20余幢钢筋混凝土框架结构薄弱层的层间位移可靠度水平,从而为直接基于位移可靠度的抗震设计中层间目标位移可靠度的确定提供了一定依据。  相似文献   

一个灵活的海洋——大气耦合环流模式   总被引：33，自引：13，他引：20  

Yu Yongqiang  Yu Rucong  Zhang Xuehong  Liu Hailong 《大气科学进展》2002,19(1):169-190

Based on the National Center for Atmospheric Research (NCAR) Climate System Model version 1(CSM-1), a Flexible coupled General Circulation Model version 0 (FGCM-0) is developed in this study through replacing CSM-1＇s oceanic component model with IAP L30T63 global oceanic general circulation model and some necessary modifications of the other component models. After the coupled model FGCM--0 is spun up for dozens of years, it has been run for 60 years without flux correction. The model does not only show the reasonable long-term mean climatology, but also reproduce a lot of features of the interannual variability of climate, e.g. the ENSO-like events in the tropical Pacific Ocean and the dipole mode pattern in the tropical Indian Ocean. Comparing FGCM-0 with the NCAR CSM-1, some common features are found, e.g. the overestimation of sea ice in the North Pacific and the simulated double ITCZ etc.The further analyses suggest that they may be attributed to errors in the atmospheric model.  相似文献   

Assessment of potential transport of pollutants into the Barents Sea via sea ice--an observational approach     

Korsnes R  Pavlova O  Godtliebsen F 《Marine pollution bulletin》2002,44(9):861-869

The present estimates of ice drift in the Arctic include utilization of satellite imagery data (special sensor microwave/imager) and a reconstruction of air pressure for the period 1899-1998. A significant part of the sea ice in the Arctic Ocean has its origin in the Kara Sea and melts in the Greenland and the Barents Sea (BS). Consequently there may be a particular risk of pollutants in the Kara Sea entering the food webs of the Greenland and BS. The ice export from the Kara Sea between 1988 and 1994 was about 208,000 km2 (154 km3) per year. The import of ice into the BS was during the same period 161,000 km2 (183 km3) per year while the ice drift through the Fram Strait into the Greenland Sea was 583,000 km2 (1859 km3) per year. Ice which formed adjacent to the Ob and Yenisey rivers in early January, drifted into the BS within two years (with a probability of about 50%.  相似文献   

风沙起电的风洞实验研究   总被引：3，自引：0，他引：3  

张鸿发  屈建军  言穆弘 《高原气象》2002,21(4):402-407

利用大型风沙物理风洞实验装置 ,模拟铺沙地面在不同风速条件下对不同粒径的沙样和混合沙的起电电场、电位和荷质比作实验测量。结果表明 :存在风沙起电效应。风洞内电场多为负极性 ,最大电场达到 - 2 9kV·m- 1 ,导线电位可达 12 0mV。沙粒越细 ,起电越强 ,且随风速增加而增大  相似文献   

1945－1995地磁场功率谱及其长期变化     

王月华  谭东海 《地球物理学进展》1996,(3)

本文根据最新修正的国际地磁参考场模型，研究了１９４５－１９９５地磁场中心偶极矩变化，地磁总场及其分量Ｘ、Ｙ、Ｚ的空间功率谱，地磁场长期变化谱的经向漂移和纬向漂移的功率谱和西向漂移速度。研究中发现最近５０年偶极矩仍在继续衰减，空间功率谱的变化也呈减小趋势。在经向谱的漂移中观察到１９７０年出现最小值，而在纬向漂移变化中１９７０年出现最大值，西向漂移速度的变化也在１９７０年出现最大值，这种现象正是１９７０年发生的地磁长期变化的突变，称作地磁＂Ｊｅｒｋ＂。  相似文献