Chinese translation for "intraseasonal"

季内

Related Translations:

intraseasonal oscillation:  季内振荡

intraseasonal time scale:  季内时间尺度

Example Sentences:

	1.	The relationship between the intraseasonal oscillations in the northern hemisphere during the boreal winter in the stratosphere and troposphere 平均环流场的气候特征及其与我国夏季降水关系的初步分析
	2.	( 4 ) the epwp climatologic sst has a clear intraseasonal variability , which is very similar to el nino growth process , i . e . , occurring in spring , developing in summer , maturing in autumn and decaying in winter 进一步分析表明，东太平洋暖池及异常经向风仅对日nino （ lanina ）事件发生、发展起促进（抑制）作用而不起决定作用。
	3.	5 intraseasonal discrepancy exists in the extremely temperature decrease corresponding with the four type of spring temperature . the cold wave incidence of the heilongjiang type tend to be more in may , while the others in april 5 、春季气温4种空间分布型态极端降温过程的分布存在月际差异，黑龙江地区多出现在5月份，其它地区多出现在4月份。
	4.	2 the intraseasonal variation features of summer precipitation in northeast china are that the 24 percent of summer precipitation concentrate on late - july and first dek of august , i . e . the 12th , 13th and 14th pen of summertime 2东北地区夏季降水的季内演变特征为：东北地区夏季降水量的近24集中在7月末期到8月上旬即主要集中在夏季第12 、 13 、 14候。
	5.	6 , the intraseasonal discrepancy exists in the temporal distribution of extreme rainfall in northeast china . while extreme rainfall appears in august in the east of liaoning and the northeast of heilongjiang , so does june in other three areas 6东北地区不同区域极端降水的时间分布存在月季差异，辽宁东部和黑龙江东北部地区主要出现在8月份，其它3个地区则出现在6月份。
	6.	Furthermore , the zonal propagation of the intraseasonal oscillation ( iso ) of the sh subtropical high is also documented . results show that the australia high ( ah ) is influenced by the mascarene high ( mh ) through the eastward propa gation of the quasi - biweekly oscillation 另外还分析了南半球副热带高压低频振荡的纬向传播，指出马斯克林高压(马高)对澳大利亚高压(澳高)的影响主要通过准双周低频振荡的东传得以实现。
	7.	In contrast , the out - of - phase vacillation in summertime ao covers the arctic region and mid - latitude asian continent . though the summertime ao exists on intraseasonal as well as interannual time scale , its asian active center abates on the intraseasonal pattern , thus awarding it more conspicuous zonal symmetric structure . interannually , summertime ao exhibits the zonal asymmetric and baroclinic features , and its seesaw mode is significant only in the lower troposphere 在年际时间尺度上，夏季北极涛动表现出比冬季北极涛动更强的纬向非对称性和对流层高、低层位相不一致的斜压性，其极地中心和亚洲中心的反位相涛动关系在对流层低层比较显著，向上逐渐减弱，到对流层高层不能表现明显的亚洲中心。
	8.	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。
	9.	Based on the ncep / ncar reanalysis products , the sea ice concentration data and the observation rainfall data in china , the seasonal , intraseasonal and interannual variations of the atmospheric circulation in the southern hemisphere ( sh ) are systematically analyzed together with their influences on east asian summer monsoon ( easm ) . the major conclusions are summarized as follows : ( 1 ) in the lower level of the troposphere , the semi - annual oscillation ( sao ) is most active along 40 s and 65 s in the extratropics of the sh . over these latitudes , the variance percentages of sao exceed 70 % , and the anti - phase variation of the sea level pressure ( slp ) between the two latitudes is primarily caused by their sao components 利用ncep ncar再分析资料、南半球海冰密度资料及中国台站降水资料，本文系统分析了南半球大气环流的季节、季节内和年际变化特征及其对东亚夏季风的影响，主要结论归纳如下： ( 1 )对南半球热带外大气环流而言， 40 s和65 s是低层大气准半年振荡最为显著的两个纬带，在这两个纬带上，半年波的贡献都超过了70 ，二者季节变化的反位相主要体现为半年波分量的反位相。
	10.	To diagnose the climate changes and anomalies on different time scales ( intraseasonal , seasonal , interannual , decadal and interdecadal ) in climate system , to investigate the formation mechanisms of the climate changes and climate anomalies from the point of view of land - sea - atmosphere interactions in climate system , and to understand the dynamical processes in the climate changes and climate anomalies 通过动力学诊断方法揭示大气中时间尺度为一周以上的各种异常气象现象及其变化，从气候系统各子系统之间相互作用的角度研究异常气候的产生机制，增加对气象异常现象形成的动力学过程的认识。

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