TJ-Ⅱ型钻孔体应变仪数字化观测资料分析

对位于山东省不同地理、构造条件的4个TJ－Ⅱ型钻孔体应变仪数字化观测资料进行了分析，结果表明：4个台的体应变资料不同程度地受降雨、地下水位、气压、温度的影响，其完整性、稳定性和可靠性不同，记录地震波的能力也存在差异。     

BDS/GPS/GLONASS融合网格伪距差分定位性能分析

为了充分利用全球导航卫星系统资源,最大限度发挥北斗卫星导航系统的优势,向用户提供高精度、高可靠性和稳定性更好的服务,该文对BDS/GPS/GLONASS 3系统融合网格伪距差分定位性能进行了分析。运用该文阐述方法的原理进行实验分析,结果表明,3系统融合网格伪距差分定位较其他方案具有更高的定位精度、解算成功率,可见卫星数大幅度提高,可靠性和稳定性更优。     

无法到达区动态定位方法研究

研究了在动态条件下对人员无法到达区目标定位的方法,分别研制了GPS激光测距定位系统和GPS近景信息采集系统。设计了水上动态实验,分析了两套系统的定位精度,验证了两套系统在动态测量模式下的可用性,提出了对人员无法到达区目标定位的新手段。     

ENSO循环与太平洋-北美型遥相关事件的关系

利用1950~2009年的Nio3.4指数和冬季5个月逐日太平洋-北美型遥相关(PNA)指数,对ENSO冷、暖位相及中性年份冬季发生的PNA事件进行了统计分析,结果发现PNA事件个数有显著的差异。ENSO暖位相年份冬季的PNA+事件个数是PNA-事件个数的4.13倍,而冷位相年份的PNA-事件个数是PNA+事件个数的2.73倍。PNA事件指数和PNA事件对应的300 hPa流函数场合成分析结果显示ENSO暖(冷)位相年份的PNA+(PNA-)事件的强度较小,生命史较长,PNA-(PNA+)事件的强度较大生命史较短,位于北太平洋上空的南北向偶极子结构仅出现在PNA+事件过程的成熟阶段。同时,聚类分析也发现,ENSO暖(冷)位相年份的PNA+(PNA-)型的比例大于PNA-(PNA+)型,PNA+型波列结构中有太平洋区域的南北向偶极子结构,而PNA-波列结构中没有,与合成分析结果一致。通过计算北太平洋的300 hPa基本流发现,ENSO循环暖位相年份的副热带急流位置比ENSO循环冷位相年份的偏北,这解释了ENSO循环冷暖位相年份PNA+事件和PNA-事件发生频率的差异。由于中性年份也存在PNA事件,ENSO循环对PNA事件的强度与发生频率有一定的调制作用。     

野生对虾与养殖对虾脂肪酸组成和含量的比较

野生中国对虾(Penaeus chinensis)脂肪酸的组成类似于其他的海洋动物,即雌、雄虾的肝胰脏和肌肉中,棕榈酸(16:0)和n-3族高不饱和脂肪酸(如20:5n-3和22:6n-3)占优势。野生虾体内含有的脂肪酸种类,尤其是高不饱和脂肪酸的种类多于养殖虾。野生虾肝胰脏中主要脂肪酸为16:0(20.0～22.5%),18:0(2.5～2.9%),18:1 n-9(12.3～14.0%),18:2 n-6(2.4～2.6%),20:5 n-3(6.1～6.6%)和22:6 n-3(7.1～7.5%)。肌肉中的主要脂肪酸种类大致与肝胰脏中相同。养殖虾中除了18:2 n-6(6.3～13.0%)高于和16:l(3.6～4.2%)低于野生虾外,其余的基本类似。野生虾比养殖虾有较高水平的n-3族和较低水平的n-6族不饱和脂肪酸,且野生虾n-3/n-6族脂肪酸的比率同样大于养殖虾。     

饵料中的锌对中国对虾的影响

本文报道了中国对虾摄食补充锌饵料的实验结果。结果表明,饵料中加锌与不加锌,对对虾的增长、增重和成活率均无明显差异;各组对虾肝胰脏中羧肽酶A的比活性也无显著变化。我们认为,利用上述原料生产的对虾配合饵料,可以不加锌,即使饵料中含锌量较高,对对虾也没有什么危害。     

Interaction between a slowly moving planetary—scale dipole envelope rossby soliton and a wavenumber— two topography in a forced higher order nonlinear Schrödinger equation

A parametrically excited higher-order nonlinear Schr dinger (NLS) equation is derived to describe the interaction of a ,slowly moving planetary-scale envelope Rossby soliton for zonal wavenumber-two with a wavenumber-two topography under the LG-type dipole near-resonant condition. The numerical solution of this equation is made. It is found that in a weak background westerly wind satisfying the LG-type dipole near-resonance condition, when an incipient envelope Rossby soliton is located in the topographic trough and propagates slowly, it can be amplified through the near-resonant forcing of wavenumber-two topography and can exhibit an oscillation.However, this soliton can break up after a long time and excite a train of small amplitude waves that propagate westward. In addition, it is observed that in the soliton-topography interaction the topographically near-resonantly forced planetary-scale soliton has a slowly westward propagation, but a slowly eastward propagation after a certain time. The instantaneous total streamfunction fields of the topographically forced planetary-scale soliton are found to bear remarkable resemblance to the initiation, maintenance and decay of observed omega-type blocking high and dipole blocking. The soliton perturbation theory is used to examine the role of a wavenumber-two topography in near-resonantly forcing omega-type blocking high and dipole blocking. It can be shown that in the amplifying process of forced planetary-scale soliton, due to the inclusion of the higher order terms its group velocity gradually tends to be equal to its phase velocity so that the block envelope and carrier wave can be phase-locked at a certain time.This shows that the initiation of blocking is a transfer of amplified envelope soliton system from dispersion to nondispersion. However, there exists a reverse process during the decay of blocking. It appears that in the higher latitude regions, the planetary-scale envelope soliton-topography interaction could be regarded as a possible mechanism of the establishment of blocking.     

The Role of Topography and Diabatic Heating in the Formation of Dipole Blocking in the Atmosphere

In this paper, the nonlinear stationary waves forced by topography and diabatic heating are investigated. It is pointed out that (1) the nonlinear interaction of different stationary waves forced only by topography might form dipole blocking in the atmosphere, this might explain the dipole blocking appeared in the Pacific and Atlantic regions; (2) the dipole blocking could not be caused by the nonlinear interaction of the different stationary waves forced by the diabatic heating alone; (3) the nonlinear interaction of the diffferent stationary waves forced by both topography and diabatic heating could initiate dipole blocking in the atmosphere. In winter, the dipole blocking mainly occurs in the west regions of the Pacific and the Atlantic, and the heat source over the western part of the two oceans is advantageous to the formation of dipole blocking in the west of two oceans. However, in summer, the dipole blocking could be formed in the east part of the two oceans, and the heat source over the eastern     

大气中大尺度扰动超熵的产生和广义 Lyapunov稳定性及其应用

本文把大气中的大尺度扰动与背景场分开,由于扰动与背景场义有能量交换,因而扰动可作为一个开放系统,尔后将耗散结构理论应用于研究大气中大尺度扰动的特性,并指出:大气中大尺度扰动超熵的产生表征了大气中扰动有效位能的增减.在此基础上,得到了一个Lyapunov函数,而这个Lyapunov函数的时间导数表征了大尺度扰动总能量的增减,另外,还按Glandsdorff和Prigogine的工作引入了一个广义Lyapunov函数,这个函数的时间偏导可以与大尺度E—P通量联系起来,最后还用大尺度扰动超熵的产生讨论了阻塞形势的发展和衰减过程.     

背景西风对由局地天气尺度波所形成阻塞的影响

本文从理论上研究了在不同的背景西风条件下阻塞胚胎与局地天气尺度波之间的相互作用。结果发现合适的弱西风对阻塞的形成是至关重要的 ,较强的背景西风不利于阻塞的形成。同时局地天气尺度波的位置也起着重要作用。