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the tropical indian ocean
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  热带印度洋
     A Diagnosis of Interactions between the Tropical Indian Ocean and Pacific Ocean Air-Sea Systems in the Past 20 Years
     近20年来热带印度洋与热带太平洋海气系统相互作用特征的诊断研究
短句来源
     The Study of the Occurrence and Evolution Mechanism of the Tropical Indian Ocean Dipole
     热带印度洋偶极子发生和演变机制的数值研究
短句来源
     Based on the thermal equation and model output data, the variation mechanism of SST and heat budget are investigated in the tropical Indian Ocean;
     基于热力学方程和海洋环流模式输出结果,探讨了热带印度洋SST和北印度洋热量收支的季节和年际变化机制,进一步揭示了海洋动力过程在北印度洋热平衡中的重要作用;
短句来源
     Study on the Heat Budget and Meridional Circulation in the Tropical Indian Ocean
     热带印度洋热收支与经向环流的研究
短句来源
     The relationships between autumn sea surface temperature(SST) anomalies in the tropical Indian Ocean and the strength of the East Asian winter and summer monsoons are investigated by analyzing Reynolds monthly SST dataset and NCEP/NCAR atmospheric reanalysis data.
     利用多年的Reynolds月平均海表温度资料和NCEP/NCAR全球大气再分析资料,分析了热带印度洋秋季海表温度距平(SSTA)与后期东亚冬夏季风强度变化的关系。
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  “the tropical indian ocean”译为未确定词的双语例句
     Using the monthly mean data from SODA, GISST 2.3b, NCEP/NCAR reanalysis, CMAP and Willmott precipitation datasets, we have investigated the relationships between the summer rainfall in southern part of China and the SSTA of the tropical Indian Ocean along with the South China Sea.
     利用CMAP和WiUmott降水、SODA和GISST 2.3b海洋变量以及NCEP/NCAR再分析月平均资料,研究了中国南方夏季降水与印度洋偶极型海温异常及南海海温异常的关系,结果表明:
短句来源
     The period analysis also finds that the dipole like a precipitation pattern in the tropical Indian Ocean has dominant periods of not ony 1.5 years but also 4 years.
     另外对偶极子型降水主要模态的周期分析表明,偶极子型降水距平还存在1.5 a和4 a左右的变化周期。
短句来源
     The results are summarized as follows:(1) The dipole pattern is observed in the sea surface height and the depth of 20℃ when a dipole event occurs in the tropical Indian Ocean as observed in SSTA.
     (1)当热带西印度洋海温偏高(低)、东印度洋海温偏低(高)时,西印度洋海表高度变高(低)、20℃等温线深度变深(浅),东印度洋海表高度变低(高)、20℃等温线深度变浅(深),赤道中印度洋出现纬向东(西)风异常。
短句来源
     The same-signed SSTA in SCS has positive (negative) correlation with both the tropical southeast (southwest) Pacific SSTA and the tropical Indian Ocean.
     与同期热带东南太平洋存在大范围正相关,与同期西南太平洋则成负相关;
短句来源
     The left component of SVD1 shows a mono-polar mode in the tropical Indian Ocean, whereas the right component (for geopotential height) of SVD1 displays a PNA-like pattern over Pacific-North America regions, indicating the close relations of Indian Ocean SSTA with the ENSO.
     SVD分析结果显示:SVD1左场是印度洋地区海温一致的单极型模态,而右场出现了类似PNA遥相关型波列,说明ENSO对中高纬度大气环流的强迫影响在IOD发生之前就已存在。
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  相似匹配句对
     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
     REVIEW ON THE ARCHITECTURE OF TROPICAL TREES
     热带树木构筑学研究概述
短句来源
     THE CHARACTERISTICS OF THE MOTION IN THE TROPICAL ATMOSPHERE
     热带大气运动的特征
短句来源
     ASYMMETRY OF UNSTABLE WAVES IN THE TROPICAL OCEAN
     热带海洋中非稳定波的不对称现象(英文)
短句来源
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  the tropical indian ocean
The interannual variability of sea surface temperature (SST) anomalies in the tropical Indian Ocean is dominated mainly by a basin-scale mode (BM) and partly by an east-west contrast mode (zonal mode, ZM).
      
A dynamic link between the basin-scale and zonal modes in the Tropical Indian Ocean
      
The air-sea interaction processes over the tropical Indian Ocean region are studied using sea surface temperature data from the Advanced Very High Resolution Radiometer sensor onboard the NOAA series of satellites.
      
Sea surface temperature anomalies to the west of New Zealand and in the tropical Indian Ocean are also useful, especially for seasonal predictions.
      
We address the various roles played by the net surface heat flux and the local and remote ocean dynamics for the seasonal variation of near-surface heat budget in the Tropical Indian Ocean.
      
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By using a five-layer primitive equation model with P-sigma coordinates, the effect of convective heating source with the oscillation of a dipole pattern over the tropical Indian Ocean- western Pacific on Asian summer monsoon is inver-stigated. The results from simulations show that the oscillatory heating source may cause oscillations in east-west zonal circulation at the quator, in cross-equatorial flow, in meridional monsoon circulation and in the phase of high-low level circulation over Asia, with...

By using a five-layer primitive equation model with P-sigma coordinates, the effect of convective heating source with the oscillation of a dipole pattern over the tropical Indian Ocean- western Pacific on Asian summer monsoon is inver-stigated. The results from simulations show that the oscillatory heating source may cause oscillations in east-west zonal circulation at the quator, in cross-equatorial flow, in meridional monsoon circulation and in the phase of high-low level circulation over Asia, with same period as that of the oscillating heat source. Furthermore, the influence mechanism of the tropical heating source associated with oscillations on Asian summer monsoon circulation is also studied. It is clearly shown that the westward propagation of thermally-forced Rossdy waves to the west of the oscillatory heating source and the northward propagation of disturbances can give rise to oscillations of the equatorial east-west zonal circulation and monsoonal meridional circulation, Finally, the oscillation of all the Asian summer monsoon circulation is formed.

本文利用p—σ混合坐标系的五层原始方程模式,研究了印度洋—西太平洋热带偶极子型振荡对流加热源对亚洲夏季环流的影响。试验结果表明印度洋—西太平洋热带振荡源可以引起赤道东—西纬向环流、越赤道气流、季风经向环流以及亚洲夏季高、低层环流的位相振荡,其振荡周期与振荡热源的振荡周期一致。本文还进一步研究了热带振荡源影响亚洲夏季风环流的机制,研究表明振荡热源西侧激发的Rossby波的西传和扰动的北传、引起赤道东—西纬向环流和季风经向环流的振荡,从而最终导致整个亚洲夏季风环流振荡的机制。

In this paper, annual and seasonal features of the distribution of SST signal areas and air-sea energy transport are studied and general ways discussed in which air-sea interaction takes place in the tropical Indian Ocean. Three SST signal areas are identified and separate maximum zonal areas for the transport of energy between the air and sea are located near 20°S and 10°N (in the Arabian Sea), showing significant seasonal variations. In the area of the Indian Ocean, the Arabian Sea and eastern...

In this paper, annual and seasonal features of the distribution of SST signal areas and air-sea energy transport are studied and general ways discussed in which air-sea interaction takes place in the tropical Indian Ocean. Three SST signal areas are identified and separate maximum zonal areas for the transport of energy between the air and sea are located near 20°S and 10°N (in the Arabian Sea), showing significant seasonal variations. In the area of the Indian Ocean, the Arabian Sea and eastern equatorial Indian Ocean are two key areas, for they not only depict the basic characteristics of the conditions of maritime heat of the ocean, but act as key regions where the air-sea interaction takes place.

本文分别研究了印度洋海温信息区和海-气能量输送的年、季分布特征,讨论了印度洋热带地区海-气相互作用的一般形态。得出,印度洋海温可划出三个信息区,在20°s附近和阿拉伯海10°N附近各有—个东西向的最大海-气能量输送区。它们都有明显的季节变化,印度洋重要海区是阿拉伯海和东赤道印度洋,因为该两个海区不仅能表征印度洋海洋热状况的基本性质,而且是印度洋海-气相互作用过程的关键海区。

Based on the ECMWF global objective analysis of 7-level mean geopotential height anomaly, a study is made of the simultaneous correlations of the corresponding points of these level with the sea surface level as the base for December, January and February (DJF) and June, July and August (JJA), respectively. Results show that the barotropy and baroclinity change greatly geographically, as shown in the height departures, with remarkable seasonality: the DJF lower troposphere anomaly is marked by higher (poor)...

Based on the ECMWF global objective analysis of 7-level mean geopotential height anomaly, a study is made of the simultaneous correlations of the corresponding points of these level with the sea surface level as the base for December, January and February (DJF) and June, July and August (JJA), respectively. Results show that the barotropy and baroclinity change greatly geographically, as shown in the height departures, with remarkable seasonality: the DJF lower troposphere anomaly is marked by higher (poor) equivalent barotropy over the oceans (continent); the upper troposhere circulation anomaly is illustrated by a high-value region of correlation coefficient around the equator and a low area dominating subtropics; the correlation pattern between the circulation departure fields of the low and upper troposphere indicates that a high region is not always over the waters and a strongest negative correlation center arises in the tropical eastern Pacific. Its comparison to the JJA pattern reveals that a particular significant seasonality occurs in Africa and the tropical Indian Ocean with a DJF vigorous barotropic sector and a JJA baroclinic one, respectively.

利用欧洲中心全球客观分析的7层月平均位势高度距平资料,分别计算了相同格点上12—2月和6—8月各层高度距平之间的同时相关分布。结果表明:全球月平均位势高度距平场的正压、斜压性随地理区域变化很大,并有较明显的季节变化。其中12—2月对流层下部大气环流距平场在海洋上空有较好的相当正压性,在大陆上空正压性较差;对流层上部大气环流异常的正、斜压性分布与下部不同,赤道附近地区是相关系数的高值区,副热带地区主要是低值区;在对流层下部与上部大气环流距平场的相关系数分布图上,海洋上空并不总是高值区,在热带东太平洋区域就出现最强的负相关中心。与6—8月的相关系数分布型比较发现:特别明显的季节变化在非洲大陆和热带印度洋区域,12—2月为强正压区,6—8月为强斜压区。

 
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