1) NW Pacific subtropical high
西北太平洋副高
1.
By using a global spectral AGCM, a numerical experiment is performed on study of the influence of the anomalies of equatorial Pacific SST, arctic sea ice and Tibetan snow cover in July on the NW Pacific subtropical high and the precipitation over China.
本文利用一个全球大气环流谱模式，对七月份赤道太平洋海温异常、北极海冰异常及高原积雪对西北太平洋副高和我国降水的影响进行数值试验，得出一些很有意义的结果。
2) the western Pacific subtropical high
西太平洋副高
1.
The multi-threshold model of multidimensional time series andits application to prediction of the western Pacific subtropical high;
高维多门限时间序列模型在西太平洋副高预报中的应用
2.
The background large-scale circulation changes include the intensification of the western Pacific subtropical high(WPSH) and the southwest shift of the East Asian jet stream(EAJS).
第一模态中,降水大值区位于华南沿海,伴随西太平洋副高的加强以及东亚西风急流的西南向移动,水汽主要来源于菲律宾和中国南海地区;第二模态中,降水大值区位于长江中下游地区,西太平洋副高及东亚西风急流均较气候平均位置偏北,水汽主要来源于赤道西太平洋,同时赤道印度洋的西风水汽输送也为降水提供了部分水汽;第三模态中,降水中心位于黄淮流域,500 hPa高压异常中心北移至日本海附近,同时东亚西风急流大大减弱,水汽源地位于中纬度西北太平洋。
3) western pacific subtropical high
西太平洋副高
1.
In terms of the NCEP/NCAR daily reanalysis data,an index based on the vorticity value in the key area is defined to describe the longitudinal position of the western Pacific subtropical high(SH).
采用NCEP/NCAR再分析逐日资料,根据特定区域涡度值,定义描述西太平洋副高东西位置的指标,并利用该指标研究了6月副高东西位置变动特征。
2.
Simultaneous relationship between Western Pacific subtropical high and the rainfall over North China, wet/dry circulation anomaly patterns and precipitable water are discussed in terms of monthly rainfall, geopotential height, precipitable water and related indices of the high.
运用月降水量、月平均高度场、西太平洋副高指数和月可降水量资料,用相关及合成分析方法分析了西太平洋副高与华北降水、旱涝环流及可降水量的关系。
3.
WT5BZ]Based on the daily reanalysis data from May to August in 1998,it is found that the transient and quasi permanent structures are different from each other for western Pacific subtropical high(WPSTH).
通过分析 1 998- 0 5～ 1 998- 0 8再分析资料 ,得知夏季西太平洋副高的准定常结构和瞬变结构有着显著的不同。
4) West Pacific subtropical high
西太平洋副高
1.
Methods of wavelet decomposition, correlation analysis, analytic variance and phase contrast were used to discuss the structural features of and relationship between near-equatorial SST and the west Pacific subtropical high.
利用小波分解、相关分析、解释方差及位相对比方法,分析讨论了近赤道海温与西太平洋副高在不同时间尺度上的结构特征与对应关系。
2.
By using the SVD (Singular Value Decomposition), the seasonal coupling relationship between the transitions of East Asian summer monsoon (EASM) rainband and the west Pacific subtropical High (WPSH) was investigated.
利用NCEP/NCAR数据集中1950～1999年4～9月500 hPa位势高度和逐日降水率(PRATE)资料,通过奇异值分解,主要探讨了东亚夏季风雨带与西太平洋副高季节移动的耦合关系。
3.
The North Africa subtropical high shows distinct seasonal changes in its intensity and location,with two obvious northward jumps in late May and late June,about two to three pentads earlier than the West Pacific subtropical high.
以北非高压的 5个指数为基础 ,分析了北非高压的气候特征 :北非高压强度越强 ,范围越广 ,东伸越明显且脊线偏南 ,反之偏西偏北 ;北非高压的强弱趋势、南北位置和东西位置具有显著的季节变化 ,其中 5月下旬和 6月下旬有两次明显的跳跃 ,在时间上比西太平洋副高两次北跳提前 2～ 3候。
5) WPSH
西太平洋副高
1.
Defined is a new east Asian monsoon index , which can perfectly describe the seasonal and interannual change of the wester n Pacific subtropical high (WPSH).
定义了新的东亚季风指数 ,分析表明该季风指数能够更好地反映西太平洋副高的季节变化和年际变化。
补充资料：太平洋地区标准会议标准(见太平洋地区标准会议)
太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC
Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条