季内振荡 meaning in English
intraseasonal oscillation
Examples
- 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。