乌拉尔山的英文

• ural mountains

• "乌拉尔"英文翻译    Ural
• "北乌拉尔山" 英文翻译 :    severny ural
• "南乌拉尔山" 英文翻译 :    gora yuzhny ural; yuzhny ural gora
• "乌拉尔山脉" 英文翻译 :    the ural mountains; ural mts; uralskiy khr
• "中乌拉尔山" 英文翻译 :    sredniy ural
• "极圈乌拉尔山" 英文翻译 :    polyarny ural
• "乌拉尔山脉的" 英文翻译 :    ural
• "乌拉尔" 英文翻译 :    ural◇乌拉尔山 the ural mountains; the urals
• "拉尔山" 英文翻译 :    lar koh
• "乌拉卡尔山" 英文翻译 :    urracal mt
• "奥乌拉尔普" 英文翻译 :    oguralp
• "乌拉尔比" 英文翻译 :    oularbi
• "乌拉尔德" 英文翻译 :    uralde
• "乌拉尔甘草" 英文翻译 :    glycyrrhiza uralensis fisch
• "乌拉尔航空" 英文翻译 :    ural airlines
• "乌拉尔河" 英文翻译 :    ural river
• "乌拉尔季奇" 英文翻译 :    ulardzic
• "乌拉尔焦尔" 英文翻译 :    urar char
• "乌拉尔阶" 英文翻译 :    uralian stage
• "乌拉尔卡河" 英文翻译 :    uralka river
• "乌拉尔丽蝇" 英文翻译 :    calliphora uralensis
• "乌拉尔普" 英文翻译 :    uralp
• "乌拉尔契奇" 英文翻译 :    ularcic
• "乌拉尔沙蜥" 英文翻译 :    phrynocephalus guttatus
• "乌拉尔斯基" 英文翻译 :    uralski; uralsky

• Indeed , the individual aims of the leaders who gathered this month in central asia ? first for a summit in bishkek , and then to the ural mountains for the war games ? are much easier to discern than any common purposes
  事实上，本月在中亚聚会的领导人的个人目标? ?首先是在比什凯克举行峰会，继而前往乌拉尔山观摩军事演习? ?相比任何共同目的要更易于为人明悉。
• The interdecadal characteristics of correlation pattern of interannual relationship between winter sea - ice extent of davis strait and august 500hpa height of northern hemisphere is " + - + " pattern from ural mountains to north of sea of okhotsk which is strongly negatively correlated with the august rainfall of north china before 1974 , and it has not apparent correlation pattern in europe - asia continent after 1974
  1974年前，冬季戴维斯海峡海冰面积和北半球8月500hpa位势高度场的相关系数呈一个自乌拉尔山开始到鄂霍次克海以北分布的“ + - + ”型，该型和8月华北降水的反相关较好； 1974年后，相关在欧亚大陆地区变差，没有明显的相关型，冬季戴维斯海峡海冰面积和8月华北降水关系变差。
• Abstract : monthly rainfall data from 1951 to 1995 for june , july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months . serious flood mainly happened in july and august , and sevious drought mainly happened in august . there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china . meanwhile , the deeper trough which covered the regions from the ural mts . to the balkhash lake play an important role in serious rainstom in rainy season in the north china . there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ) , and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage
  文摘:利用华北平原地区的13个站点, 45年（ 1951 1995 )的降水资料,对夏季4个时段（ 6月、 7月、 8月、 6 8月）进行了z指数计算,确定了该地区各个时段的严重涝年和严重旱年.发现华北地区雨季的严重洪涝主要集中在7 , 8月,严重干旱则主要发生在8月,并可明显看出由50 60年代的多水期向70年代中期以后的少水期的转变,另外,乌拉尔山到巴尔喀什湖附近的低压槽加深和西北太平洋副热带高压的北抬,对华北地区雨季持续性暴雨的产生起着决定性的作用.严重洪涝年的夏季（ 6 8月） ,西北太平洋副热带高压偏西、偏北,赤道东太平洋海温多处于下降阶段;严重干旱年西北太平洋副高偏东、偏南,赤道东太平洋海温则处于上升阶段
• Firstly , subtropical high center lay to the north than usual , and forms a blocking high in combination with land high in eastern asia . secondly , on account of the strong southwest current which occurred at the west side of the subtropical high and dynamic effect of the typhoon itself , the landing northward tropical cyclone ( 9711 ) landed in liaoning again . thirdly , a trough with some weak air from ural mountain and the northeast cold air entering into the tropical cyclone showed that the systems in different latitudes had some effects each other
  模拟结果表明：此次热带风暴造成辽宁全省大暴雨的天气背景是：副热带高压偏北并与大陆高压叠加，构成了稳定的东亚阻塞形势； 9711台风减弱的热带风暴，在其自身内力和副高西侧的强盛偏南气流引导下，持续北上并在辽宁营口至盘锦之间登陆；从乌拉尔山冷堆分裂南下出的弱冷空气不断南下，与热带风暴在辽宁产生了相互作用，增强了上升运动，致使大暴雨出现。
• The most severely damaged will be the canadian low arctic tundra ; the wooded ural mountain taiga in russia ; the central andean dry puna in chile , argentina and bolivia ; the daurian steppe of mongolia ; the savannah of north - east india and nepal ; and the fynbos of southern africa
  受害最严重的将是加拿大的下北极苔原，俄罗斯树木繁茂的乌拉尔山针叶林，智利、阿根廷和玻利维亚安第斯山脉中部的干冷高原，蒙古的干草原，印度和尼泊尔两国东北部的热带稀树草原，非洲南部的高山硬叶灌木群落。
• This paper use the ncep / ncar day - to - day reanalysis data of 500hpa high field and so on , choose ural mountain , baikal , okhotsk as the key district , the mid - high latitude of eurasia circulation courses that have long duration ( scale of time is middle , namely during 10 - 30 day ) , maybe continue continuously after being intermittence of 1 - 2 days in middle , appear repeatedly is for research object , define an index " i " of the circulation pattern over mid - high latitude of eurasia . a method is proposed to identify the summer typical persistent circulation pattern at 500hpa levels over eurasia mid - high latitude . the climate characteristics of those typical persistent circulation patterns are studied
  本文利用ncep / ncar再分析逐日500hpa高度场等资料，选择乌拉尔山、贝加尔湖、鄂霍次克海这三个地方作为关键区，以夏季欧亚中高纬度持续时间长(时间尺度属于中间时间尺度，即10 ? 30天之间) 、中间可能会间歇1 、 2天然后又继续持续、反复出现的环流过程为研究对象，定义了一个夏季欧亚中高纬流型指数，在此基础上提出了一种对夏季欧亚中高纬500hpa典型持续流型的界定方法，研究了典型持续流型的气候特征，分析了流型指数的年代际变化，以及对应不同阶段、不同流型的降水场、加热场、海温场等的主要特征。
• The analysis on the spatial distribution feature of rainfall trend for global land seasonal and monthly rainfall points out that the mainly regions of increasing precipitation are north of canada , east of greenland , southeast of south america , mid - west of australia , from newland to north of siberian in northern ural and west of europe
  分析了全球陆地3 - 5月及逐月降水量的空间分布特征。指出全球陆地3 - 5月降水正趋势明显的区域有，加拿大北部、格陵兰岛东部、南美东南部、澳大利亚中西部、乌拉尔山以北新地岛至北西伯利亚和西欧。
• ( 2 ) sxsp anomaly is closely related to the abnormity of 500hpa geopotential height field over the east of ural and yakutsk area , western ridge point and area of subtropical high , the cold air abnormity from north of china and the position of upper level westerly jet over east asia
  ( 2 )三峡库区夏季降水异常与大气环流异常密切相关：与500hpa乌拉尔山以东高度场异常、雅库茨克以东高度场异常、副热带高压面积及西伸脊点、北方冷空气异常、 200hpa东亚高空西风急流位置异常偏南(偏北)密切相关。
• Monthly rainfall data from 1951 to 1995 for june , july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months . serious flood mainly happened in july and august , and sevious drought mainly happened in august . there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china . meanwhile , the deeper trough which covered the regions from the ural mts . to the balkhash lake play an important role in serious rainstom in rainy season in the north china . there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ) , and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage
  利用华北平原地区的13个站点, 45年（ 1951 1995 )的降水资料,对夏季4个时段（ 6月、 7月、 8月、 6 8月）进行了z指数计算,确定了该地区各个时段的严重涝年和严重旱年.发现华北地区雨季的严重洪涝主要集中在7 , 8月,严重干旱则主要发生在8月,并可明显看出由50 60年代的多水期向70年代中期以后的少水期的转变,另外,乌拉尔山到巴尔喀什湖附近的低压槽加深和西北太平洋副热带高压的北抬,对华北地区雨季持续性暴雨的产生起着决定性的作用.严重洪涝年的夏季（ 6 8月） ,西北太平洋副热带高压偏西、偏北,赤道东太平洋海温多处于下降阶段;严重干旱年西北太平洋副高偏东、偏南,赤道东太平洋海温则处于上升阶段