负异常的英文

• negative anomaly

• "负"英文翻译    burden; load
• "异常"英文翻译    unusual; abnormal; anomalous ...
• "负异常带" 英文翻译 :    negative belt
• "负异常区" 英文翻译 :    negative area
• "系统负异常" 英文翻译 :    systematic negative anomaly
• "负相区 负异常区 凹下部分" 英文翻译 :    negativearea
• "负异促反应" 英文翻译 :    negative heterotropic reaction
• "负异固缩" 英文翻译 :    negative heteropycnosis
• "负异性石" 英文翻译 :    eucolite; eukolite
• "负异钠花岗岩" 英文翻译 :    fasibitikite
• "异常" 英文翻译 :    1.(不同于寻常) unusual; abnormal; anomalous; singular 异常现象 abnormal phenomena; 神色异常 not be one's usual self2.(非常) extremely; exceedingly; extraordinarily; particularly 异常丰富 exceedingly rich; 异常需要 particularly necessary; 异常危险 extremely dangerous; 异常迫切 extremely anxious; 这种鱼的肉异常鲜美。 the flesh of this kind of fish has exceptional delicacy.3.(反常) anomaly 气候异常 climatic anomaly
• "负异钠闪花岗岩" 英文翻译 :    fasibitikite
• "eeg异常" 英文翻译 :    eeg abnormality
• "poland异常" 英文翻译 :    poland anomaly
• "rieger异常" 英文翻译 :    rieger's anomaly
• "壁异常" 英文翻译 :    change in wall
• "磁异常" 英文翻译 :    magnetic anomaly
• "电异常" 英文翻译 :    electrical anomaly
• "反常，异常" 英文翻译 :    abnormal; anomaly; anormal
• "古异常" 英文翻译 :    fossil anomaly
• "氦异常" 英文翻译 :    helium anomaly
• "核异常" 英文翻译 :    dyskarosis
• "假异常" 英文翻译 :    false anomaly; spurious anomaly; tramp
• "矿异常" 英文翻译 :    anomalies related to mineral deposits; ore anomaly
• "例外；异常" 英文翻译 :    exception

• Cu - ni sulfided mine complex locate in baimazai of jinping county is sub alkali iron - super iron , it ' s zoning is clear and it ' s ni - cu - co melting first and enrichment , its rare earth is rich in right lean light rare earth , but eu in olive rock is serious to be bad , gd - tb is tittles negative abnormity . above - mentioned show that the mineral is cone from mantle , and didn " t mix with crustal substance , and continent tholeiite magma turning into continent tholeiite emplacement after by surging
  金平白马寨铜镍硫化矿床杂岩体分带明显、属亚碱性铁质-超铁质岩、具ni - cu - co三元素先熔离，后富集的规律、稀土配分为右倾斜轻稀土富集型，但橄榄岩铕亏损显著， gd - tb微小负异常，显示成矿物质来源地幔，与地壳物质无混染和大陆拉斑玄武岩浆上涌后变为大洋拉斑玄武岩浆侵位特点。
• In heavy snow years , there are marked anomaly of atmospheric circulation : on 500 height field trough of east asia is heavier , north - west flow after height trough is striver , so that cold air of eastern region is stronger following " cold winter ' . spring rain answering to eurasia winter snow anomaly is notable , in heavy snow years , yangtse - river has negative rain anomaly
  在欧亚冬季积雪异常偏重的年份，大气环流出现显著异常： 500hpa位势高度场上径向气流占优势，东亚大槽偏强，高度场槽后西北气流偏强，造成影响我国东部地区的冷空气偏强，出现“冷冬天气” 。我国春季降水对欧亚冬季积雪异常的响应最为显著，重雪年春季我国长江流域以南大部地区出现明显的降水负异常。
• There is a north - north - east negative anomaly belt of aerial magnetism in the middle - east part of the basin , which could be displayed by the aerial magnetism of commutative field , upwardly continuation , lvt in earthquakes , the experimentation of granite liquation ( demagnetization ) , the distribution of neozoic era volcanic rock , earthquake , hot spring and ground feature . the anomaly shows the blocking in east - west direction , and it is also associated with intense activity of deep heat interaction and the development of the crust - mantle mixed layer in the north qiangtang
  从区域航磁、向上延拓、地震低速层、花岗岩熔融(退磁)实验、新生代火山岩的分布、地震、温泉、地貌等发现，盆地中东部存在一北北东向航磁负异常带，既显示出东西分块，也与北羌塘深部热力作用强烈活动、发育“壳幔混合层”有联系。
• The research showed that : from january to march , the acreage average ozone gross gathered , which was synchronized with the increase of the frequency of strong ssw event . furthermore , the change tendency of ozone gross in the atmosphere break forward and backward 1990 . after the1990s , ozone gross in the atmosphere appeared negative anomaly in the mid and high latitude of north hemisphere from january to march , which was consistent with the obvious descent of appearance frequency of strong ssw event after the 1990s
  分析表明： 1至3月，臭氧总量的面积平均逐渐增高，这与强ssw事件频数1至3月增高同步；此外，大气臭氧总量趋势变化以1990年前后存在明显的突变， 90年代以后，北半球中高纬1 ? 3月间大气臭氧总量处于负异常阶段，这和90年代以来强ssw事件发生频数明显下降相吻合。
• On the paas - normalized plots , the parent granite and the granite weathering crust are enriched in lree without ce anomaly . while the groundwaters are also enriched in lree , they display significant negative ce anomaly , indicating the fractionation of ce during water - rock interaction . based on the study of two profiles of granitoid weathering crust , we concluded that ree concentrations in the groundwaters from the granitoid weathering crust are likely related to the continued chemical weathering , as well as the ree concentrations in the crust near the water table , clay concentration and the wate r ph values
  地下水与母岩、风化壳稀土的paas标准化分布模式基本相似，呈lree富集型，母岩中无ce异常，而水样中有ce负异常，表明ce在水岩作用过程中发生明显的分异；通过研究两个典型花岗岩风化壳剖面发现，地下水的稀土含量与连续的化学风化，以及水位附近剖面上的稀土含量、粘土矿物含量以及水的ph值等有关。
• ( 4 ) in summer , tropic west pacific ssta decadal change infect precipitation decadal change in south and north of changjiang river maybe by : positive ssta in tropic west pacific weaken the summer monsoon circulation , lead more precipitation in south of changjiang river and less precipitation in north of it , vice versa ; middle north pacific ssta decadal change infect precipitation decadal change in mid - down valley of changjiang river maybe by : when ssta is negative in middle north pacific , the height field in tropic rises obviously , the subtropical high strengthens and extends westward , the northern limit retreats southward , leads upper trough retreats northward and move eastward , meiyu front moves northward , then leads more precipitation in mid - down valley of changjiang river , vice versa ; middle northwest pacific - low latitude mid - east pacific infects precipitation in north china possibly by change the activity of northeast china cyclone
  （ 4 ）热带西太平洋ssta年代际变化影响夏季中国长江南北降水年代际变化的可能机制是热带西太平洋海表温度正（负）异常减弱（加强）东亚夏季风环流，从而使江南降水增加（减少） ，江北降水减少（增加） ；夏季中部北太平洋ssta年代际变化影响中国长江中下游地区夏季降水年代际变化的可能机制是中部北太平洋海表温度负异常，将导致热带地区高度场普遍增高，副高加强西伸，副高北界南退，致使高空槽北缩东移，梅雨锋西移北进，中国长江游中游、中卜游降水增多，反之亦反；夏季中高纬西北太平洋一低纬中东太平洋反向距平分布结构影响中国东北降水的可能机制是低纬中东太平洋海表温为负异常。
• On base of results above , composite model of ssta in pacific and circulation anomaly are constructed for analysis their evolution . during mature phase of el nino usually in winter , positive ssta dominates in tropical eastern ocean and negative ssta dominates in west wind drift district in mid - latitude ocean , correspondingly the pna index of 500 hpa geopotential height is positive which means the aleutian low gets strong , and the situation is somewhat inversely during la nina phase of ssta
  合成位相反映了太平洋ssta演变特征，以及相对应的大气环流异常特征：当西风漂流区处于暖态而热带中东太平洋海温偏低时，合成大气模型当中阿留申低压减弱， 500hpapna指数为负异常；当西风漂流区处于冷态，热带中东太平洋处于暖态( elnino峰值?成熟期ssta典型分布) ，合成大气模型中阿留申低压加强， 500hpapna指数为正异常。
• Among the felsic rocks , samples from the zhangjiakou formation ( fm . ) are characterized by moderately to strongly eu anomalies , and variable negative anomaly of sr , ti and p , whereas samples from the donglingtai fm . exhibit enriched lree and flat hree patterns with nb / ta fractionation and high zr / sm ratios
  在中酸性火山岩系列中，张家口组火山岩表现出中等-强烈的eu负异常和不同程度的sr 、 ti 、 p负异常；东岭台组火山岩表现出富集lree和平坦的hree的稀土配分模式， nb ta分馏，高zr sm比值。