季内振荡的英文

• intraseasonal oscillation

• "季"英文翻译    season
• "内"英文翻译    inner; inside; within
• "振荡"英文翻译    generation; oscillating; osc ...
• "内振荡器" 英文翻译 :    internal oscillator
• "季内" 英文翻译 :    intraseasonal; season in
• "内振动" 英文翻译 :    internal vibration
• "季内克" 英文翻译 :    tynek
• "带内振铃" 英文翻译 :    signaling in band
• "面内振动" 英文翻译 :    in plane vibration; in-plane vibration
• "带内振铃设备" 英文翻译 :    inband signalling equipment
• "贝季内茨" 英文翻译 :    betinec
• "法尔季内克" 英文翻译 :    faltynek
• "福尔季内克" 英文翻译 :    foltynek
• "哈别季内克" 英文翻译 :    habetinek
• "季内伊纳湾" 英文翻译 :    gnejna bay
• "杰维亚季内" 英文翻译 :    devyatiny
• "科季内克" 英文翻译 :    kotynek
• "科斯季内茨" 英文翻译 :    kostinec
• "科斯季内克" 英文翻译 :    kostinek
• "利亚季内" 英文翻译 :    lyadiny
• "林季内罗娃" 英文翻译 :    lintinerova
• "卢什季内茨" 英文翻译 :    lustinec
• "马拉季内茨" 英文翻译 :    malatinec
• "乌季内克" 英文翻译 :    utinek
• "振荡" 英文翻译 :    generation; oscillating; oscillation; vibration 本机振荡 local oscillation; 寄生振荡 parasitic oscillation; 振荡变压器 oscillation transformer; 振荡波 wave of oscillation; 振荡次数 number of oscillation; 振荡电路 oscillating circuit; oscillatory circuit; oscilation circuit; 振荡功率 hunting power; 振荡管 oscillating tube; oscillating valve; 振荡离心机 [机械工程] vibratory centrifuge; 振荡指示器 [电学] cymoscope

• The spread features of sst mjo are not clearly
  55了季内振荡沿上述路径的传播方向不清晰。
• 5 ) the features of the olr and velocity potential ( x ) mjo spreading eastward , northeastward ( wnp ) and southeastward ( wsp ) are researched on the climatic and interannual scale
  5 )用改进了的复经验正交函数( ceof )方法分析了从赤道印度洋到西太平洋然后向正东、东北、东南三条路经上的olr及速度势x的季内振荡传播特征。
• 2 ) the olr mjo intensity anomaly for the four key areas of the pacific , namely , the tropical western pacific , the middle and eastern pacific , the northwest pacific and the southwest pacific , is significantly and positively related to the local ssta
  2 )太平洋四关键区(热带西太平洋、热带东中太平洋、西北太平洋、西南太平洋)的olr季内振荡强度与sst异常呈显著局地同时性正相关关系。
• The tropical eastern pacific ( for the whole year ) , northwest pacific ( for the boreal spring , summer and autumn ) and southwest pacific ( for the austral summer around ) are the strong mjo regions of sst with the conditions of shallow climatic mixed layer depth
  Sst季内振荡高强度区存在于热带东太平洋(终年存在) ，西北太平洋(北半球春夏秋季存在、夏季最强)和西南太平洋(南半球夏季前后存在) ；气候薄混合层( mld )是其存在条件。
• During the el nino ( la nina ) events , the negative ( positive ) sst anomaly occurs and the corresponding the olr mjo intensity weakens ( enhances ) in the tropical western pacific ; at the same time , the positive ( negative ) surface westerly anomaly leads to positive ( negative ) mld anomaly , and the corresponding sst mjo intensity weakens ( enhances ) in the equatorial eastern pacific , 4 ) the interdecadal variation of the atmospheric mjo intensity took place distinctly in 1970s in the tropical western , northwest and eastern pacific , with the stronger intensity in the former than the back stage , and the interdacadal variation of sst is its cause
  Elnino ( lanina )事件中热带两太平洋sst出现负(正)异常， olr季内振荡强度出现减弱(增强)的变化。 elnino ( lanina )事件中，赤道太平洋出现地面信风西风分量正(负)异常，并引起热带东太平洋mld出现正(负)异常，造成热带东太平洋sst季内振荡强度出现减弱(增强)的变化。 4 )热带印度洋、热带西太平洋和热带东太平洋季内振荡强度在上世纪70年代发生了明显的年代际变化，均为前弱、后强， sst本身的年代际变化是其原因。
• 1 ) the centers of the strong olr mjo as found in the tropical indian ocean and the western pacific warm pool are observed in any one of the four seasons ; the mjo are stronger in the boreal winter and spring than in the boreal summer and autumn and move southward and northward with season ; high climatic sst is the conditions for strong olr mjo
  得到如下主要结论： 1 )热带印度洋和热带西太平洋暖池区域是olr季内振荡高强度区；它们终年存在，北半球冬春季强、夏秋季弱，且随季节更替作南北向移动；气候高sst区是其存在条件。
• In terms of diagnostic analysis chiefly , including of lanczos filter , single value decomposition ( svd ) , ceof , composite and correlation analysis etc . , and numerical modeling , the temporal and spatial characteristics of the intraseasonal oscillation ( mjo ) of the air - sea system and the causes are investigated in this paper
  本文对海气系统季内振荡的时空特征及其成因作了气候学研究。主要采用诊断方法( lanczos滤波、奇异值分解、复自然正交函数分析、合成分析及相关分析等) ，并结合数值模拟。
• It is shown that olr spread eastward more clearly in the eastern hemisphere , and the x is persistently spread eastward in both hemisphere ; the interannual variability of the spread of mjo is evident , with the intensity weakening during el nino events and sometimes spreading westward in individual years
  气候上，在沿赤道的传播中， olr东半球较西半球明显， x东、西半球无显著差别；两种要素季内振荡沿向东南路径的传播较向东北路径的传播特征明显。异常表现为季内振荡强度在elnin 。
• With the exception of the tropical western pacific of large mld . there is negative correlation relationships between the anomaly of the sst mjo intensity and that of the mld in the other three regions in the seasons of the climatic small mld thus the causes of climatic and anomalous characteristics of atmospheric mjo are related to sst identically , and the corresponding features of sst mjo are related to mld , 3 ) enso is the strongest sign and can lead to the distinct sst and mld anomaly , hence the intensity anomaly of the air - sea system inevitably takes place during the enso
  Sst季内振荡强度与mld异常的局地同时性相关结果是，热带西太平洋无显著相关(气候mld较大) ，其余三关键区气候mld小的季节均存在sst季内振荡强度与mld异常的负相关联系。因此大气季内振荡气候及异常特征直接成因一致地与sst 、有关；海洋季内振荡相应特征则直接与mld有关。 3 ) enso是海气系统中最强异常信号，在海洋中它引起了sst 、 mld的明显异常，因此，伴随enso必然发生海气系统季内振荡强度的异常。
• 6 ) the correlation relationships of the mjo of daily 10m - wind ( v ) fields with that of sst fields are investigated by time - lagged svd method in the north pacific , south pacific and the tropical eastern pacific , and the basal process of v and sst mjo obtained in the three areas , which is a negative feedback process drived by drift and sensible heat under the conditions of shallow mld , is probably the maintaining mechanism
  6 )用时滞svd方法分析了北太平洋、南太平洋、热带东太平洋区域10米高处逐日风(夕)场与sst场季内振荡的相关联系，得到了三区夕、 sst场季内振荡的基本过程，它们是由漂流和感热输送推动的一个负反馈过程，它以薄mld为存在条件，可能是sst季内振荡的维持机制。