纬

基于MSP430的织物纬斜检测系统

Bias weft detection system of fabric based on MSP430

无纬绑扎带在复合外套MOA中的应用

Application of Weft Bandage Tape in MOA Polymeric Housing

利用天文时纬观测资料解算组合Love数

Determination of the love number a from astronomical time and latitude observations

西北太平洋137°E断面海流的纬向体积输送

Zonal volume transports at 137 ° e in the northwestern Pacific

当Kp在4和6之间时，随着Kp指数增大，Sq焦点向低纬方向移动；

When 4 low latitudes as K_pindex is increased ;

基于PLC的片梭织机自动混纬系统

The automatic mixed filling system of projectile loom based on the PLC

提出基于摄像检测的整纬系统，使用CCD摄像机取代传统光电式整纬机的光电探头。

, we propose a weft-straightening system based on camera detection .

低纬电离层闪烁与扩散F

Radio Wave Scintillations and Spread - F at Low-latitudes

低纬子午环配备科学CCD后的课题目标

The Research Goal with the Low Latitude Meridian Circle Attached the Scientific CCD Detector

低纬地磁Z分量的半年变化

Semiannual variation of geomagnetic Z component at low latitude

用时－空谱分析方法分析了32.5°N纬圈上的1980～1983年逐日大气折射指数N单位的变化。

The space - time spectral analysis is adopted to explore the variation in the 1980 ~ 1983 daily atmospheric refractive index N at 32.5 ° N.

南亚（50°&100°E）夏季风的撤退是造成这种纬向平均温度减小的重要原因。

The monsoon withdrawal from South Asia ( 50 ° - 100 ° E ) contributed the most to this rapid zonal mean temperature decrease .

热带大气环流对低纬太平洋SST暖异常的响应

Response of the tropical atmospheric circulation to the low & latitude Pacific SST warm anomaly

本文选取较真实的电离层模型参数，对130°E和114°E两个子午面内传播的低纬哨声进行了射线跟踪。

The most realistic ionospheric electron density models are selected to trace whistler rays of low latitudes in 130 ° E and 114 ° E meridian planes .

本文介绍了1980年冬和1981年冬在广东省湛江地区（磁纬9.8°N）观测哨声的结果。

Results from whistler observation over Zhanjiang Region ( Mag. Lat. 9.8 # N ), Kwang-tung , China , in winter , 1980 and in winter , 1981 are described .

切变基本纬向流中赤道Rossby包络孤立波

Equatorial Rossby Envelope Solitary Waves in a Mean Zonal Flow with Shear

旋转正压纬向流中的非线性Rossby波

Nonlinear Rossby wave in a rotating barotropic zonal current

卫星OLR资料在低纬风场分析中的应用

Application of OLR data to the wind analysis in the tropics

用经列和纬行造8k阶Franklin半幻方

Constructing 8k Orders Franklin Semi Magic Square by Using Warp Column and Weft Row

此外，利用Eu和Ev矢量讨论了高频波对纬向平均流和经向平均流的反馈强迫作用。

The forcing role of the band-pass eddies on the time-mean zonal and meridional flows is also examined by use of vectors Eu and Ev .

初步分析发现，在湛江附近（磁纬约10°N）存在一个比较稳定的哨声路径出口区，三台同时接收到的哨声大多从这同一出口区透射出来；

It was found that there is a stable exit region near Zhanjiang ( geomag . lat. 10 ° N ), from which most of the coincident whistlers received at the 3 stations originate .

论证了这些纬向带具有地球深部的背景。在它们与一些弧形构造和V形构造交会的部位易于发生8级大震。

As those zones have the background in deep of the earth , over 8 magnitude earthquakes are prone to take place in their intersection regions with arc and V type tectonics .

纬向平均副热带高压和Hadley环流下沉支的关系

Relation between the zonal mean subtropical anticyclone and the sinking arm of the Hadley cell

最后利用优化后的结果在ADAMS软件中构建六连杆打纬机构的虚拟样机模型，通过仿真得到期望的运动特性。

The virtual prototype model of 6-link beating mechanism is constructed in ADAMS with the optimal design , and an expected kinematical characteristic is achieved at last .

分析了赤道地区纬向风的年际变化特征，以及亚澳季风与ENSO在各个位相的联系。

The interannual variability of tropical zonal wind and the relationship between ENSO and the Asian / Australian monsoon in different phases are discussed .

另外，与气候平均比较，暖异常年纬向Walker环流上升支大幅西移，而冷异常年该环流上升支则东移。

In addition , the ascending branch of the Walker circulation moves westward largely in the warm abnormal years , but shift eastward in the cold abnormal years .

利用NCEP/NCAR40a再分析资料研究了赤道低平流层纬向风垂直切变与ENSO变率间的关系。

Based on the NCEP / NCAR 40-year reanalysis dataset , analysed is the relationship between vertical shear of zonal wind in equatorial lower stratosphere and ENSO variability .

中低纬Spread-F的数值模拟

Numerical simulation of Spread-F in low and mid-latitudes

当少台风活动时期，东亚为纬向环流，西南太平洋上赤道西风及ITCZ也弱。

During the inactive period , the circulation of East Asia is essentially zonal and the ITCZ over Southwest Pacific is weak .

ITF的年代际变化是：年代际信号取决于赤道太平洋纬向风应力的变化。

The decadal variation of ITF is that the decadal signal lies in the change of latitude-oriented wind stress in the Equator-Pacific region .