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高压活动
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  high activities
     An inverse correlation between the isotope time series of peat cellulose from Jinchuan and Hongyuan has been used for indicating the subtropical high activities of the Western Pacific Ocean.
     文章以金川和红原两组泥炭纤维素Δδ1 3C时间序列值的反向变化来指示西太平洋副热带高压活动变化。
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  “高压活动”译为未确定词的双语例句
     In this paper, the observations of the blocking high over the mid-high latitudes in east Asia (45-75°N, 80-120°E) are analysed.
     本文对1966—1989年6—8月亚洲东部中高纬(45—75°N,80—120°E)阻塞高压活动进行了研究。
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     The Characteristic Analysis of the Continuity rainstorm and South Asia High Activity in July
     7月份连续性暴雨与南亚高压活动特征分析
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     In this paper, a multiple-grid aia-sea coupled stochastic dynamic model whose main variables are height field and sea temperature field is designed and deduced according to the principles of dynamics and thermeodynamics of the atmosphere, moreover, and used for forecasting experiments on 500hPa height field.
     本文从大气热力学与动力学原理出发,设计并推导了一个以高度场和海温场为主要变量的多网格点的海气耦合随机动力模式,用此模式作500hPa平均高度场的预报试验。 预报以春季月份(2月)为初始场,取西太平洋副热带高压活动地区(10°N-40°N,110°E-170°W)6月500hPa高度场作为预报场。
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     A DIAGNOSTIC ANALYSIS OF ACTIVITIES OF THE WESTERN PACIFIC SUBTROPICAL HIGH DURING THE SECOND MEIYU PERIOD IN 1998
     1998年二度梅雨期西太平洋副热带高压活动的诊断分析
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     THE LOW-FREQUENCY OSCILLATION OVER THE QINGHAI-XIZANG PLATEAU AND THE ACTIVITIES OF THE SOUTH ASIA HIGH DURING THE SUMMER HALF YEAR IN 1981 AND 1982
     1981和1982年夏半年高原地区低频振荡与南亚高压活动
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     Activities
     活动
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     AN OBSERVATIONAL STUDY ON THE BEHAVIOR OF THE SUBTROPICAL HIGH OVER THE WEST PACIFICIN SUMMER
     夏季北太平洋副热带高压系统的活动
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     The Method And Application For Quantitatively Analyzing Subtropical High Activity By Using Satellite Cloud Images
     利用卫星云图定量分析副热带高压活动的方法及应用
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     Activity Show
     活动展示
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     HIGH PRESSURE HEAT EXCHANGER
     高压换热器
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  high activities
The objective of this study was to prepare a new photocatalyst with high activities for degradation of organic pollutants.
      
It was demonstrated that high activities of endogenous enzymes (nucleases and proteases) in milts of hydrobionts correlated with the degree of hydrolysis of their nucleic acids.
      
Preparations aGA, AG20X, and VR, characterized by high activities of pectinase and α-galactosidase, as well as laboratory preparation B2000Mix with a high activity of α-galactosidase, provided the highest yield of sugars from soybean flour.
      
In most newborns very high activities were recorded, which exceeded the activities in adults at rest 7-8-fold or 3-fold according to the conventional calculation, or more than 30-and 6-fold according to our more precise calculation.
      
On the contrary, high activities of liver transaminases are suggestive to be a result of some regulation mechanisms between the enzyme protein and its coenzyme.
      
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In this paper, an analysis is made on two main distinct flow patterns over the tropical and subtropical area in Asia and on its adjacent water. They occur respectively in the periods of July 8-18, 1958 and July 21-30, 1957. It is found that during these two periods there is marked difference in the characteristics of the tropospheric circulations. The position of zonal wind belt over the northern hemisphere, the distribution of long wave patterns, the activity of subtropical highs, and the distribution of the...

In this paper, an analysis is made on two main distinct flow patterns over the tropical and subtropical area in Asia and on its adjacent water. They occur respectively in the periods of July 8-18, 1958 and July 21-30, 1957. It is found that during these two periods there is marked difference in the characteristics of the tropospheric circulations. The position of zonal wind belt over the northern hemisphere, the distribution of long wave patterns, the activity of subtropical highs, and the distribution of the intertropical convergence zone are all quite different. At the same time, the activity of typhoons and other synoptic processes over the continent are also different.In addition, we found that there are some interactions between the northern and the . southern hemisphere. When low index circulation prevails over subtropics and tropics in Eastern Asia, there is meridional circulation in the southern hemisphere (especially in Australia), and there is a mass transport from the southern to northern hemisphere. While high index circulation prevails over northern hemisphere, zonal flow pattern prevails in the southern hemisphere.

根据1958年7月8—18日和1957年7月21—30日东亚低纬度的两个悬殊的环流型,分析了在这两个时期内东亚低纬度环流的各种特征。结果得出,在经向和纬向环流期间,无论北半球纬向风带的位置,长波系统的配置,副热带高压活动的情况以及赤道辐合区的分布都有着很大的不同。此外,台风活动的次数也表现有很大悬殊。其所以有如此悬殊,可以从该两时期低纬度流场的特点来说明原因。在中国大陆上,在这两个时期的天气过程也很不同,在经向环流期间,大陆上的主要雨带成东北—西南向的,而在纬向环流期间,雨带便成东西向分布,并集中在江淮流域之间。 另外,我们又研究了在这两个时期内南北半球间环流关系,从手头所掌握的资料分析结果看,两者关系相当密切。在东亚低纬度经向环流期间,南半球(特别在澳洲)也盛行经向环流,并且在澳洲附近从南半球向北半球的质量输送也最强烈;而在东亚低纬度纬向环流期间,南半球也盛行纬向环流,澳洲附近的冷空气活动不显著,越过赤道向北的质量输送也比较弱。

In this Paper, we had computed the geopotential anomaly field and the latitude geostrophic wind velocity of north hemispher 100 mb level. It was discussed that the activity of polar vortex and southasia high has a connection with the summer low temperature of Chinese Northeast Region. Following conclusions were obtained:1.The anomaly cold summer of Chinese Northeast Region is becomed by the weak suthasia high and the usual activity of polar cold air in middle latitude.2.Winter (Nov.-Feb.) 100mb level pacific...

In this Paper, we had computed the geopotential anomaly field and the latitude geostrophic wind velocity of north hemispher 100 mb level. It was discussed that the activity of polar vortex and southasia high has a connection with the summer low temperature of Chinese Northeast Region. Following conclusions were obtained:1.The anomaly cold summer of Chinese Northeast Region is becomed by the weak suthasia high and the usual activity of polar cold air in middle latitude.2.Winter (Nov.-Feb.) 100mb level pacific high has a connection with summer southasia high. The correlation coefficient of them is 0.62.3.It is show that there are three kinds of frequency graphs of five months (Jan.-May.) 100mb level polar vortex: a) When the arctic vortex is always activity in the north polar region, the summer temperature of Chinese Northeast Region is warm, b) When the arctic vortex is always activity in Eurasia, the summer temperature of Chinese Northeast Region is cold irrespective of intensity or weak the southasia high, c) When there are two frequency centres of frequency graph of five months (Jan.-May.) arctic vortex located specifically at Eurasia and north America, the summer temperature of Chinese Northeast Region is determined by high or low of southasia high. They are correlation to each other.4.The summer temperature of northeast region has a connection with winter snow-cover Eurasia area and sonwfall of Chinghai-Tibet plateau. They are anti-correlations each other.

本文利用10O毫巴面资料,计算了位势距平场及纬向地转风速,讨论了极涡、南亚高压的活动与我国东北区夏季低温的关系,得出如下结论: 1.中国东北区夏季异常低温的形成,是南亚高压弱、极地冷空气经常在中纬度活动的结果; 2.冬季(11—2月)100毫巴太平洋副热带高压与夏季的南亚高压有关系,他们的相关系数等于0.62; 3.1—5月 100毫巴面极涡的频数分布有三种类型:a·当极涡经常在极区活动时,则东北区夏季气温偏暖;b‘当极涡持续偏心在欧亚大陆活动时,则东北区夏季气温偏冷3c·如果极涡的频数分布有两个高频数中心分别在欧亚及北美,则东北区夏季气温的偏暖或偏冷决定于南亚高压的偏高或偏低,他们彼此成正相关; 4.东北区夏季气温与欧亚大陆冬季的雪盖面积和青藏高原的降雪量成反相关。

According to the analysis of 13 years data, it is shown that there are close relations between the ridge and center positions of Qinghai-Xizang high pressure on 100mb surface and the large scale distribution of floods and droughts in East China in summer.

通过分析13年资料后,指出夏季100毫巴青藏高压脊线及高压中心的位置与我国东部大范围旱涝分布的关系密切。 1.夏季100毫巴青藏高压脊线的位置,尤其是120°E处脊线位置,与长江中、下游梅雨期及伏旱期有密切的关系,梅雨期120°E脊线位于26°—32°N之间,伏旱期在33°N以北。 2.夏季100毫巴青藏高压中心经常出现在高原上空,这可能与高原夏季加热作用有关。100毫巴青藏高压中心、脊线位置及90°—120°E脊线的走向与我国东部地区旱涝有较密切的关系。 3.把100毫巴青藏高压的活动划分成东部型、带状型及西部型三类天气过程。在东部型和带状型过程中,长江中、下游、川东及贵州少雨(旱),而川西及华北多雨(涝);相反在西部型过程中,长江中、下游、川东及贵州多雨(涝);而川西少雨(旱),华北多雨(涝)。

 
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