El Ni?o 事件期间南海环流的异常特征     

邢延松  程国胜  舒业强  王东晓 《海洋与湖沼》2012,43(2):201-209

基于CORA再分析资料对南海环流的季节特征和其受ElNio事件的响应进行了分析。结果表明,冬季整个南海海区表现为一个大的气旋式环流,夏季南海北部是气旋式环流,南部是一个反气旋式环流。通过对南海海区异常流场进行MV-EOF分解,分析其前两个模态,其空间型主要体现了南海环流冬季和夏季的特征,对应的时间系数与Nio3.4_NDJ指数有很好的相关性。通过分析南海环流在1986—2008年间ElNio年份的异常流场和异常流函数场,证明了MV-EOF分解后得到的联合时间系数所反映各阶段南海环流的季节特征与ElNio事件有相关性,即在8月[0],南海南部异常流函数场表现为反气旋式环流,北部为气旋式环流,南海夏季环流被增强,且ElNio事件时间尺度越长,北部的气旋式异常流场的影响范围就越大;在12月[0],南海除了东南部外,其余整个海区异常流函数场主要表现为反气旋式环流,冬季环流被减弱;在8月[+1],南海夏季流场强度都被削弱了。  相似文献   

Synoptic-scale disturbances over the northern South China Sea and their responses to El Ni(n)o     

ZENG Lili  LI Xixi  DU Yan  SHI Rui  YAO Jinglong  WANG Dongxiao  SUI Dandan 《海洋学报(英文版)》2012,31(5)

  相似文献   

Low-frequency variations in primary production in the Oman upwelling zone associated with monsoon winds     

廖晓眉  詹海刚  韦惺 《中国海洋湖沼学报》2012,30(6):1045-1053

Thirteen-year satellite-derived data are used to investigate the temporal variability of net primary production (NPP) in the Oman upwelling zone and its potential forcing mechanisms. The NPP in the Oman upwelling zone is characterized by an abnormal decrease during El Ni o events. Such an NPP decrease may be related to El Ni o-driven anomalous summertime weak wind. During the summer following El Ni o, the anomalous northeasterly wind forced by southwest Indian Ocean warming weakens the southwest monsoon and warms the Arabian Sea. The abnormal wind weakens the coastal Ekman transport, offshore Ekman pumping and horizontal advection, resulting in reduced upward nutrient supply to the euphotic zone. A slightly declining trend in NPP after 2000 associated with a gradual decrease in surface monsoon winds is discussed.  相似文献   

Perturbed solving method for interdecadal sea-air oscillator model   总被引：1，自引：0，他引：1  

Jiaqi Mo  Yihua Lin  Wantao Lin  Lihua Chen 《中国地理科学(英文版)》2012,22(1):42-47

A coupled system of the interdecadal sea-air oscillator model is studied.The El Nio-southern oscillation(ENSO) atmospheric physics oscillation is an abnormal phenomenon involved in the tropical Pacific ocean-atmosphere interactions.The oscillator model is involved with the variations of both the eastern and western Pacific anomaly pat-terns.This paper proposes an ENSO atmospheric physics model using a method of the perturbation theory.The aim is to create an asymptotic solving method for the ENSO model.Employing the perturbed method,the asymptotic solution of corresponding problem is obtained,and the asymptotic behaviour of the solution is studied.Thus we can obtain the prognoses of the sea surface temperature anomaly and related physical quantities.  相似文献   

营口市柳树镇M4．0级地震基于AutoSmart的震动图分析研究     

毕明鹏  陈方颖  姜博  张欣然  金震 《东北地震研究》2012,28(4)

2012年2月2日营口市柳树镇M4．0级地震,辽宁省强震动台网有5个强震台站记录到了地面运动,记录的最大加速度为138．747gal,初步展现了辽宁省强震动台网数字化建设的成效。由于我省数字化台站软件是和广东省Taide软件公司共同开发的,本次地震很好的总结了前一阶段的成果,并指出了很多不足的地方。本文对此次地震的强震记录的软件部分进行了初步分析。  相似文献   

2011年新西兰M_w6.1地震震源过程及强地面运动特征初步分析          下载免费PDF全文

孟令媛  史保平 《地球物理学报》2012,55(5):1601-1612

2011年2月21日新西兰南岛发生M_w6.1地震,震中位置43.58°S,172.70°E,震源深度约5.0 km,发震断层为新西兰第三大城市克赖斯特彻奇(Christchurch)南约9 km一条近东西走向的未知隐伏断层,为逆冲断层机制.地震已经造成163人遇难,Christchurch城内多处建筑物严重损毁,距震中约1 km的Heathcote Valley Primary School (HVSC)台站强地面运动峰值加速度(PGA)高达2.0g.针对新西兰M_w6.1地震近场强地面运动偏高这一现象,利用HVSC台站的强震观测记录,计算地震震源谱参数,应用Brune圆盘模型估算其近场强地面运动的理论值,并建立动态复合震源模型进行模拟计算.研究结果表明,新西兰M_w6.1地震近断层强地面运动偏高的主要原因为复杂震源破裂过程中有效应力降(动态应力降,Δσ_d)过高造成的.未来工作中,需要加强对可能发生的、距离城市较近的中小型地震的重视,防止地震对城市的加强型破坏.  相似文献   

中国大陆GPS连续观测站基线时间序列分析   总被引：4，自引：0，他引：4  

张风霜  武艳强  孙东颖 《地震》2011,31(4):86-97

本文根据中国地壳运动观测网络基准站1999年初至2010年9月底的资料, 对中国大陆90条GPS基线时间序列进行了分析, 讨论了这些基线在正常情况下的趋势性运动特征, 总结了2001年昆仑山口西和2008年汶川两次8级大震前GPS基线时间序列的异常变化, 并在此基础上分析了GPS基线近期变化情况。  相似文献   

极震区的地震动与潜在震源区内重大工程安全   总被引：11，自引：4，他引：7  

韩文峰宋畅  梁庆国 《工程地质学报》2004,12(4):346-353

潜在震源区是未来可能发生破坏性地震的震源所在地区 ,区内的地震属近场或直下型 ,其地震破坏和地震动特征相应于已发生地震的极震区。近期国内外诸多强烈地震的实际资料和相关研究成果表明 ,直下型地震不仅地震峰值加速度大 ,且竖向和水平峰值加速度比值也有别于远场地震的统计关系。文中从极震区岩土体破坏、地震动特点及地震地质灾害等方面对潜在震源区内的重大工程问题进行了探讨  相似文献   

Curvature ductility of columns and structural displacement ductility in RC frame structures subjected to ground motions     

《Soil Dynamics and Earthquake Engineering》2014

This paper examined the statistical relationship between the curvature ductility demands of columns and the global displacement ductility demands of reinforced concrete (RC) frame structures when subjected to earthquakes. Elements with a designated moment–curvature relationship were adopted for both beam and column elements, and five-story and ten-story RC frame numerical structures were established. Using pushover analysis and earthquake nonlinear dynamic time-history analysis, the maximum global displacement ductility demands of the structure and the maximum curvature ductility demands of the columns were determined. The effects of the spectral acceleration and the strong column factor on ductility demands were analyzed, and the quantitative relationship between the curvature ductility demands of columns and the global displacement ductility demands of frame structures were established. Moreover, the validity of the established relationship was further tested and verified through a real-world application. The results show that the maximum curvature ductility demands of the columns and the maximum displacement ductility demands of the structure were positively associated with the spectral acceleration and negatively associated with the strong column factor. A proposed first-degree linear relationship between curvature ductility of columns and structural displacement ductility in RC frame structures with two parameters was obtained by curve fitting, while considering the effect of the strong column factor. The model was highly correlated with the sampling analysis data. Applying the empirical model established in this study is a simple and effective means to guide the design of ductility and the assessment of RC frame columns.  相似文献   

Influences of Indian Ocean interannual variability on different stages of El Nio: A FOAM1.5 model approach     

XiaoYuan Hong  HaiBo Hu  XiuQun Yang  Yuan Zhang  GuoQiang Liu  Wei Liu 《中国科学:地球科学(英文版)》2014,57(11):2616-2627

Both the tropical Indian and tropical Pacific Oceans are active atmosphere-ocean interactive regions with robust interannual variability, which also constitutes a linkage between the two basins in the mode of variability. Using a global atmosphereocean coupled model, we conducted two experiments(CTRL and PC) to explore the contributions of Indian Ocean interannual sea surface temperature(SST) modes to the occurrence of El Ni?o events. The results show that interannual variability of the SST in the Indian Ocean induces a rapid growth of El Ni?o events during the boreal autumn in an El Ni?o developing year. However, it weakens El Ni?o events or even promotes cold phase conversions in an El Ni?o decaying year. Therefore, the entire period of the El Ni?o is shortened by the interannual variations of the Indian Ocean SST. Specifically, during the El Ni?o developing years, the positive Indian Ocean Dipole(IOD) events force an anomalous Walker circulation, which then enhances the existing westerly wind anomalies over the west Pacific. This will cause a warmer El Ni?o event, with some modulations by ocean advection and oceanic Rossby and Kelvin waves. However, with the onset of the South Asian monsoon, the Indian Ocean Basin(IOB) warming SST anomalies excite low level easterly wind anomalies over the west tropical Pacific during the El Ni?o decaying years. As a result, the El Ni?o event is prompted to change from a warm phase to a cold phase. At the same time, an associated atmospheric anticyclone anomaly appears and leads to a decreasing precipitation anomaly over the northwest Pacific. In summary, with remote forcing in the atmospheric circulation, the IOD mode usually affects the El Ni?o during the developing years, whereas the IOB mode affects the El Ni?o during the decaying years.  相似文献