助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   tropical india ocean 的翻译结果: 查询用时:0.179秒
图标索引 在分类学科中查询
所有学科
海洋学
更多类别查询

图标索引 历史查询
 

tropical india ocean
相关语句
  热带印度洋
     With to the 5 ×5 sea surface temperature anomaly data about the tropical India Ocean and the tropical Pacific(22.5 S~22.5 N,42.5 E~77.5 W)from 1951 to 1995, the average power spectral was first analyzed for the sea surface temperature anomaly data. The results show that there are quasi-12-yr. and quasi-4-yr.
     根据热带印度洋和热带太平洋(22.5 S~22.5 N,42.5 E~77.5 W )1951~1995年逐月5 ×5 的海面温度距平资料,首先进行了海面温度距平的平均功率谱分析,获取赤道印度洋和赤道太平洋海面平均温度距平存在准12年和准4年的周期变化;
短句来源
     THE OSCILLATION LAW FOR THE SEA SURFACE TEMPERATURE OF THE TROPICAL INDIA OCEAN AND TROPICAL PACIFIC
     热带印度洋和热带太平洋海温振荡规律的研究
短句来源
     It was found that the "key regions" from which moisture transports influenced Shandong summer rainfall lies in tropical India Ocean, South China Sea to tropical west Pacific, China mainland to Japan Sea and the upstream area in westerly belt by analysis of SVD method on water vapor transport.
     7月虽然来自热带印度洋季风区的水汽输送通量达到最大值,但7~8月它们对山东夏季降水异常的贡献并不显著,相反来自南海-西太平洋、中国大陆-日本海的水汽输送以及西风带天气系统对山东夏季降水异常的贡献较显著。
短句来源
     The results of these experiments show that: (1) The SST anomalies in tropical eastern Pacific can modify the distribution of LFO variance. When the positive center of ΔSST is at the middle of tropical eastern Pacific, the value of LFO variance center in tropical eastern Pacific is larger than that in tropical western Pacific and tropical India Ocean.
     结果表明:赤道东太平洋冬半年的海温异常增暖可改变低频振荡方差贡献的地理分布,其中当正的ΔSST中心位于赤道东太平洋的东部时,热带印度洋和西太平洋地区的低频振荡的方差贡献较为显著,而热带东太平洋的低频振荡较为不活跃;
短句来源
  相似匹配句对
     INDIA
     神佑印度
短句来源
     Journey to India
     印度之旅
短句来源
     THE OSCILLATION LAW FOR THE SEA SURFACE TEMPERATURE OF THE TROPICAL INDIA OCEAN AND TROPICAL PACIFIC
     热带印度洋和热带太平洋海温振荡规律的研究
短句来源
     Tropical cooking film
     高温蒸煮膜
短句来源
     Tropical Botanical Garden
     热带之梦中心
短句来源
查询“tropical india ocean”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
没有找到相关例句


To investigate the effect of SST anomalies on the characters of low frequency oscillation(LFO), two sets of numerical experiment have been performed with the 2 layer OSUGCM. One uses monthly climatic data of SST and the other includs two tests in which the artificial centers of SST anomalies(ΔSST) are assumed in the eastern and the middle of tropical eastern Pacific, respectively. The results of these experiments show that: (1) The SST anomalies in tropical eastern Pacific can modify the distribution...

To investigate the effect of SST anomalies on the characters of low frequency oscillation(LFO), two sets of numerical experiment have been performed with the 2 layer OSUGCM. One uses monthly climatic data of SST and the other includs two tests in which the artificial centers of SST anomalies(ΔSST) are assumed in the eastern and the middle of tropical eastern Pacific, respectively. The results of these experiments show that: (1) The SST anomalies in tropical eastern Pacific can modify the distribution of LFO variance. When the positive center of ΔSST is at the middle of tropical eastern Pacific, the value of LFO variance center in tropical eastern Pacific is larger than that in tropical western Pacific and tropical India Ocean. The contrast is true, when the positive center of ΔSST is in the eastem part of tropical eastern Pacific. (2) The response of propagation characters of LFO to the geographic location of ΔSST center is sensitive considerably, that is, the propagation direction and phase velocity of LFO in the two sensitive tests are different considerably.

为研究海温的异常增暖对30-60天低频振荡的影响,利用OSU两层大气环流模式作了两组试验:一组使用气候平均海温,另一组包括两个试验,它们分别设正的海温距平(ΔSST)中心位于赤道东太平洋的东部(100°W)和中部(145°W)。结果表明:赤道东太平洋冬半年的海温异常增暖可改变低频振荡方差贡献的地理分布,其中当正的ΔSST中心位于赤道东太平洋的东部时,热带印度洋和西太平洋地区的低频振荡的方差贡献较为显著,而热带东太平洋的低频振荡较为不活跃;当正的ΔSST中心位于赤道东太平洋的中部时,情形则相反,即热带东太平洋的低频振荡的方差贡献较显著,而西太平洋地区的则不活跃。在赤道东太平洋海温异常增暖过程中,低频振荡的传播特性对ΔSST中心位置的响应是敏感的,即当正的ΔSST中心位置偏于该海区的东部或中部时,低频振荡的传播方向和传播速度有明显的差异

With to the 5 ×5 sea surface temperature anomaly data about the tropical India Ocean and the tropical Pacific(22.5 S~22.5 N,42.5 E~77.5 W)from 1951 to 1995, the average power spectral was first analyzed for the sea surface temperature anomaly data. The results show that there are quasi-12-yr. and quasi-4-yr. oscillation periods for the sea surface temperature anomaly data about the tropical India Ocean and the tropical Pacific. Thereafter, the covariant spectral and time-lag spectral...

With to the 5 ×5 sea surface temperature anomaly data about the tropical India Ocean and the tropical Pacific(22.5 S~22.5 N,42.5 E~77.5 W)from 1951 to 1995, the average power spectral was first analyzed for the sea surface temperature anomaly data. The results show that there are quasi-12-yr. and quasi-4-yr. oscillation periods for the sea surface temperature anomaly data about the tropical India Ocean and the tropical Pacific. Thereafter, the covariant spectral and time-lag spectral in the 12-yr. and 4-yr. oscillation periods are further analyzed with the cross power spectral analysis for multiple dimension time series. Some significant results are obtained.

根据热带印度洋和热带太平洋(22.5 S~22.5 N,42.5 E~77.5 W )1951~1995年逐月5 ×5 的海面温度距平资料,首先进行了海面温度距平的平均功率谱分析,获取赤道印度洋和赤道太平洋海面平均温度距平存在准12年和准4年的周期变化;然后,利用多维时间序列的交叉谱分析,进一步分别分析了赤道印度洋和赤道太平洋各格点上海面温度距平在准12年和准4年演变周期各格点之间的演变位相及演变落后时间,获得一些有意义的结论。

Using the monthly mean reanalysis data of height, wind and vertical velocity of NCEP/NCAR from 1958 to 2003, the characteristics of 500hPa height anomalies in the Northern Hemisphere, convergence and divergence on the levels of 200hPa and 925hPa and vertical stream over the Shandong province were studied and compared with that over North China. The study shows that the teleconnection pattern called East Asia-Pacific pattern (EAP) plays important roles in the summer rainfall of Shandong. Weaker Okhotsk sea high,...

Using the monthly mean reanalysis data of height, wind and vertical velocity of NCEP/NCAR from 1958 to 2003, the characteristics of 500hPa height anomalies in the Northern Hemisphere, convergence and divergence on the levels of 200hPa and 925hPa and vertical stream over the Shandong province were studied and compared with that over North China. The study shows that the teleconnection pattern called East Asia-Pacific pattern (EAP) plays important roles in the summer rainfall of Shandong. Weaker Okhotsk sea high, stronger upward stream over tropical areas and Shandong and northward location of subtropical high and stronger Indian low, are likely to lead to more rain in Shandong province in summer, but there are some flood (drought) years in which these characteristics such as the location and intensity of subtropical high change with the least extent. The difference between Shandong and North China in 500hPa height is that there is a teleconnection pattern called Europe / Asia pattern in North China, while there is a negative East Asia Pattern in Shandong during drought years. There is a teleconnection relation between Shandong summer rainfall and convective activities happening in tropical areas in spring and summer accomplished by the Rossby waves. During the flood years in Shandong, the convective activities happening in tropical India Ocean and tropical west Pacific and Walker circulation are much stronger than that during the drought years, but the convective activities happening in tropical east Pacific are weaker than those during the drought years.

利用1958~2003年NCEP/NCAR再分析资料,对山东旱涝年500hPa高度距平、高(200hPa)低(925hPa)层散度距平、OLR距平分布以及115~123°E山东东西边界范围内的平均垂直速度进行合成分析,并与华北旱涝年大气环流的分布特征进行了对比。结果发现:(1)北半球500hPa夏季存在的东亚-太平洋遥相关型(EAP)对山东夏季降水产生重要影响,山东涝年夏季500hPa呈现出EAP型,旱年呈负EAP型。(2)山东涝年,鄂霍茨克海高压春季偏强、夏季偏弱,山东上游易维持低压槽区,副高偏北,热带地区对流活动加强,Hadley和Walker环流加强,山东上空盛行上升运动。旱年与涝年的特征基本相反,只是鄂霍茨克海高压在春季和夏季均较常年偏强。(3)不同旱年(涝年)的500hPa特征与旱年(涝年)平均情况相似,只是有时距平中心位置和强度不同。特别是涝年,冷空气强度、入侵路径以及副高的位置均有差别。(4)华北旱涝年500hPa高度距平与山东不同。华北旱年500hPa欧亚大陆中高纬度呈现出EU遥相关分布,且华北涝年夏季鄂霍茨克海和朝鲜-日本地区位势高度变化不显著。(5)影响山东夏季降水的热带强迫源区主要位于热...

利用1958~2003年NCEP/NCAR再分析资料,对山东旱涝年500hPa高度距平、高(200hPa)低(925hPa)层散度距平、OLR距平分布以及115~123°E山东东西边界范围内的平均垂直速度进行合成分析,并与华北旱涝年大气环流的分布特征进行了对比。结果发现:(1)北半球500hPa夏季存在的东亚-太平洋遥相关型(EAP)对山东夏季降水产生重要影响,山东涝年夏季500hPa呈现出EAP型,旱年呈负EAP型。(2)山东涝年,鄂霍茨克海高压春季偏强、夏季偏弱,山东上游易维持低压槽区,副高偏北,热带地区对流活动加强,Hadley和Walker环流加强,山东上空盛行上升运动。旱年与涝年的特征基本相反,只是鄂霍茨克海高压在春季和夏季均较常年偏强。(3)不同旱年(涝年)的500hPa特征与旱年(涝年)平均情况相似,只是有时距平中心位置和强度不同。特别是涝年,冷空气强度、入侵路径以及副高的位置均有差别。(4)华北旱涝年500hPa高度距平与山东不同。华北旱年500hPa欧亚大陆中高纬度呈现出EU遥相关分布,且华北涝年夏季鄂霍茨克海和朝鲜-日本地区位势高度变化不显著。(5)影响山东夏季降水的热带强迫源区主要位于热带印度洋、南海-热带西太平洋,两者实现遥相关的可能机制是热带强迫所激发的大尺度准定常Rossby波列的传播。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关tropical india ocean的内容
在知识搜索中查有关tropical india ocean的内容
在数字搜索中查有关tropical india ocean的内容
在概念知识元中查有关tropical india ocean的内容
在学术趋势中查有关tropical india ocean的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社