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the tropical pacific ocean
相关语句
  热带太平洋
    POP Analysis of Wind Stress Anomalies in the Tropical Pacific Ocean
    热带太平洋风应力距平场的主振荡型分析
短句来源
    Simulation of Seasonal Variations in the Tropical Pacific Ocean
    热带太平洋环流季节变化的数值模拟
短句来源
    SST anom- alies in different regions of the ocean influence the monsoon in different time: the indian Ocean is from April to June, South China Sea is May-June, while the influence of the tropical Pacific Ocean can per- sist from the last winter to this summer.
    不同区域海温对季风的影响有明显的季节差异,印度洋主要为晚春至初夏(4~6月),南海为5~6月,而热带太平洋从前冬一直持续到夏季。
短句来源
    A positive SSTA in the tropical Indian Ocean induces an easterly anomaly in the tropical Pacific Ocean, which results in a negative SSTA on both the interannual and interdecadal times cales in the tropical Pacific, and vice versa.
    热带印度洋SST暖(冷)异常导致热带太平洋上空东(西)风异常,该风应力异常在年际和年代际尺度上均导致热带太平洋SST冷(暖)异常,但年代际尺度上异常更明显.
短句来源
    Hindcast experiments of SAOMS shows it has a certain skill to predict the SST anomalies over the tropical Pacific Ocean, with the correlation coefficients considerably exceeding the persistence prediction at 6-12 lead months.
    SAOMS模式系统的回报试验表明 ,该系统对热带太平洋海表面温度距平有一定的预报能力 ,模式超前 6~ 12个月的回报与观测的相关系数明显高于持续预报。
短句来源
  热带太平洋
    POP Analysis of Wind Stress Anomalies in the Tropical Pacific Ocean
    热带太平洋风应力距平场的主振荡型分析
短句来源
    Simulation of Seasonal Variations in the Tropical Pacific Ocean
    热带太平洋环流季节变化的数值模拟
短句来源
    SST anom- alies in different regions of the ocean influence the monsoon in different time: the indian Ocean is from April to June, South China Sea is May-June, while the influence of the tropical Pacific Ocean can per- sist from the last winter to this summer.
    不同区域海温对季风的影响有明显的季节差异,印度洋主要为晚春至初夏(4~6月),南海为5~6月,而热带太平洋从前冬一直持续到夏季。
短句来源
    A positive SSTA in the tropical Indian Ocean induces an easterly anomaly in the tropical Pacific Ocean, which results in a negative SSTA on both the interannual and interdecadal times cales in the tropical Pacific, and vice versa.
    热带印度洋SST暖(冷)异常导致热带太平洋上空东(西)风异常,该风应力异常在年际和年代际尺度上均导致热带太平洋SST冷(暖)异常,但年代际尺度上异常更明显.
短句来源
    Hindcast experiments of SAOMS shows it has a certain skill to predict the SST anomalies over the tropical Pacific Ocean, with the correlation coefficients considerably exceeding the persistence prediction at 6-12 lead months.
    SAOMS模式系统的回报试验表明 ,该系统对热带太平洋海表面温度距平有一定的预报能力 ,模式超前 6~ 12个月的回报与观测的相关系数明显高于持续预报。
短句来源
  “the tropical pacific ocean”译为未确定词的双语例句
    A Coupled General Circulation Model for the Tropical Pacific Ocean and Global Atmosphere
    A Coupled General Circulation Model for the Tropical Pacific Ocean and Global Atmosphere
短句来源
    It is revealed that the mean meridional circulation in the tropical Pacific ocean has two different basic patterns: Hadley cell and Anti-Hadley cell.
    本文揭露,热带太平洋地区的平均经圈环流存在着两种最基本的类型:经典哈得来环流圈和哈得来反环流圈。
短句来源
    In January,Tropical high cloud and the corresponding upward regions are mainly located south of the equator,and exhibit zonal belt patterns with three distinct regions,including South Africa and the adjacent West Indian Ocean,the tropical Pacific Ocean and South America between equator and 30°S.
    热带1月份的云区和上升区集中在赤道以南,呈带状分布,其中南非及相邻的西印度洋、120°E~120°W的赤道太平洋、赤道与30°S之间的南美大陆为3个主要区域;
短句来源
    The third is from the tropical Pacific Ocean to the east of Philippines.
    第3股气流来自菲律宾以东的热带太平洋地区。
短句来源
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  the tropical pacific ocean
One of the major forcings for the interannual variability of the Asian Summer Monsoon is the Sea Surface Temperature (SST) distribution in the tropical Pacific Ocean.
      
Both signals shared a delayed action oscillator (DAO) similar to that shared by corresponding signals in the tropical Pacific Ocean (White et al., 2003), intensified in the South Indian Ocean.
      
The effects of intra-seasonal wind forcing on the mean field of the tropical Pacific Ocean has been studied using an ocean general circulation model (GCM).
      
Seasonal variation in the upper layer thickness of the tropical Pacific ocean model
      
Fluctuation of transports and Sea level in the western boundary region of the tropical Pacific Ocean
      
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It is revealed that the mean meridional circulation in the tropical Pacific ocean has two different basic patterns: Hadley cell and Anti-Hadley cell. The transformation of one type of the mean meridional circulation to the other not only has the seasonal variation but also the non-seasonal long-term variation. The intensity of meridional circulation has a long-term fluctuation with the period of 32-48 monthes.It is also found that the transformation of mean meridional circulation patterns is closely connected...

It is revealed that the mean meridional circulation in the tropical Pacific ocean has two different basic patterns: Hadley cell and Anti-Hadley cell. The transformation of one type of the mean meridional circulation to the other not only has the seasonal variation but also the non-seasonal long-term variation. The intensity of meridional circulation has a long-term fluctuation with the period of 32-48 monthes.It is also found that the transformation of mean meridional circulation patterns is closely connected with the variation of the vertical circulation on the vertical plane along the equator. There exists a low-frequency coupling oscillation between them. The transformation of atmospheric vertical circulations would have some importent influences on the long-range weather variation in this region.

本文揭露,热带太平洋地区的平均经圈环流存在着两种最基本的类型:经典哈得来环流圈和哈得来反环流圈。它们的出现,不仅具有明显的季节特点,而且还存在着一类值得重视的非季节性的长期变化。平均经圈环流强度,具有周期大约48个月的长期振荡。这一振荡与赤道纬圈平面上垂直环流的变化有密切关系,并能对该地区大气的水平环流产生重要的影响。

First, the differences between the propagating path and amplitude distribution 昽f quasi-stationary planetary waves forced by a forcing source over middle latitudes and those forced by a forcing source over low latitudes in a winter basic current are theoretically discussed. It is pointed out that the anomaly of heat source over low latitudes may largely influence the anomalies in the tropo-spheric circulations over middle and high latitudes, while the anomaly of heat source over middle latitudes may play an...

First, the differences between the propagating path and amplitude distribution 昽f quasi-stationary planetary waves forced by a forcing source over middle latitudes and those forced by a forcing source over low latitudes in a winter basic current are theoretically discussed. It is pointed out that the anomaly of heat source over low latitudes may largely influence the anomalies in the tropo-spheric circulations over middle and high latitudes, while the anomaly of heat source over middle latitudes may play an important role for the stratospheric circulation anomalies.A quasi-geostrophic, 34-level spherical coordinate model with Rayleigh friction, Newtonian cooling and horizontal eddy thermal diffusivity is used to compute the disturbance patterns responding to an anomaly of heat source over middle latitudes and over low latitudes, respectivily. The computed results show that the anomaly of heat source over low latitudes may largely influence on the winter circulation anomalies over middle and high latitudes, and the anomaly of heat source over the tropical Pacific Ocean may cause the PNA (the Pacific/ North America) pattern anomalies.

本文首先从理论上讨论了北半球冬季低纬度强迫源与中纬度强迫源强迫所产生的准定常行星波在实际基本气流中传播路径及其振幅分布的差异,指出冬季低纬度热源异常将对北半球中、高纬度对流层大气环流的异常起很大影响,而中纬度热源异常将对平流层环流异常起很大作用。 本文应用一个包括Rayleigh摩擦、Newton冷却及水平涡旋热力扩散准地转34层球坐标模式分别计算了冬季低纬度热源异常与中纬度热源异常所造成北半球扰动系统的异常情况,计算结果表明了冬季低纬度热源异常将对中、高纬度对流层大气环流异常起很大作用,热带太平洋上空热源异常将产生PNA型环流异常。

By using composite, correlate analysis and SVD (Singular Value Decomposition) technique, the relationships among the onset of the South China Sea Summer Monsoon (SCSM), its associ- ated circulation anomalies from April to June and SST anomalies in the tropical Indian-Pacific Ocean were investigated. The results indicate the impacts of SST anomalies in the tropical Indian -Pacific Ocean on the onset of SCSM and its associated monsoon circulation anomalies are significant....

By using composite, correlate analysis and SVD (Singular Value Decomposition) technique, the relationships among the onset of the South China Sea Summer Monsoon (SCSM), its associ- ated circulation anomalies from April to June and SST anomalies in the tropical Indian-Pacific Ocean were investigated. The results indicate the impacts of SST anomalies in the tropical Indian -Pacific Ocean on the onset of SCSM and its associated monsoon circulation anomalies are significant. The onset of SCSM is early (late) when SST anomalies in the tropical central-eastern Pacific Ocean, Indian Ocean (mainly in the southwestern region) and South China Sea are negative (positive), while SST anomalies in the western Pacific Ocean and Australia's adjacent seas are positive (negative). SST anom- alies in different regions of the ocean influence the monsoon in different time: the indian Ocean is from April to June, South China Sea is May-June, while the influence of the tropical Pacific Ocean can per- sist from the last winter to this summer. Different SST anomalies can induce different monsoon circulation regimes; circulation anomalies in early or late SCSM are basically reverse. A close relationship exists between SCSM and the activities of the western Pacific subtropical high in previous winter and spring: when the western Pacific subtropical high is weak (strong), the onset of SCSM is early (late). Monsoon circulation and Walker circulation anomalies induced by SST anomalies in the tropical Pacific-Indian Ocean maybe play an important role in influencing SCSM in terms of its onset time.

用合成和相关分析方法及SVD技术研究了南海夏季风爆发早、晚年份4~6月季风建立时期季风环流的异常及其与热带太平洋-印度洋海温的关系。结果表明,南海夏季风爆发与热带大气环流和海温变异密切相关。(1)当热带中、东太平洋-印度洋(主要在西南部)及南海海温低(高),西太平洋-澳洲邻近海域海温高(低)时,南海夏季风爆发早(晚)。不同区域海温对季风的影响有明显的季节差异,印度洋主要为晚春至初夏(4~6月),南海为5~6月,而热带太平洋从前冬一直持续到夏季。(2)不同的海温异常产生不同的季风环流型,南海夏季风爆发早、晚年大气环流的异常变化基本相反。南海夏季风的活动主要受印度季风环流变化的影响,与前期冬春季西太副高的强弱及位置变化密切相关。西太副高弱时,南海夏季风爆发早;反之,爆发晚。(3)热带太平洋-印度洋海温异常引起季风环流和Walker环流的异常变化可能是影响南海夏季风爆发早、晚的物理过程。

 
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