巴尔喀什湖的英文
发音:
"巴尔喀什湖"怎么读"巴尔喀什湖"的汉语解释用"巴尔喀什湖"造句
英文翻译手机版
- balkhash lake
- balkash
- balkhash oz
- lake balkhash
- "巴尔喀什" 英文翻译 : balkhash
- "巴尔喀什山" 英文翻译 : gora balkhash
- "喀什湖" 英文翻译 : balkhash lake
- "喀什" 英文翻译 : cascar/qäshqär; kashgar; kashi; kaxgar; kaxqar; khg
- "布尔喀" 英文翻译 : buruke
- "喀尔喀" 英文翻译 : khalkha
- "廓尔喀" 英文翻译 : gkh gorkha; gurkha
- "比什湖" 英文翻译 : biche l. la
- "菲什湖" 英文翻译 : fish lake
- "喀什河" 英文翻译 : kax he
- "喀什市" 英文翻译 : kashgar; kashi shi
- "喀什玉" 英文翻译 : kashgar jade; nbsp
- "库什湖" 英文翻译 : kus golu
- "洛什湖" 英文翻译 : loche la; loche, la
- "马什湖" 英文翻译 : marsh l
- "纳什湖" 英文翻译 : nash lake
- "托什湖" 英文翻译 : torsvatn
- "耶什湖" 英文翻译 : jiesjavrre
- "因什湖" 英文翻译 : insh lake
- "阿尔喀山" 英文翻译 : arka shan
- "丹珠尔喀泽" 英文翻译 : tengyur
- "喀尔喀蒙古" 英文翻译 : khalkha
- "柯尔喀塔" 英文翻译 : kolkata
- "科尔喀斯" 英文翻译 : colchis
- "巴尔卡" 英文翻译 : balca; balka; barcat; barkat; parca; varca
- "巴尔聚尔" 英文翻译 : bardhyl
例句与用法
- According to the " tahcheng protocol on the delimitation of the sino - russian border " 1864 , china was compelled to cede 440 , 000 km
根据1864年在塔城签订的中俄勘分西北界约记又称塔城条约,中国割让巴尔喀什湖以东以南, 44万km - According to the " tahcheng protocol on the delimitation of the sino - russian border " ( 1864 ) , china was compelled to cede 440 , 000 km
根据1864年在塔城签订的中俄勘分西北界约记(又称塔城条约) ,中国割让巴尔喀什湖以东、以南, 44万km - 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 - 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
其他语种
百科解释
巴尔喀什湖(,)古称夷播海,是位于中亚哈萨克斯坦共和国东部的一个内流湖,在19世纪属于大清国,隶属伊犁将军辖区。沙俄势力扩张到此之后,清政府被迫于1864年与沙俄签定不平等条约《中俄勘分西北界约记》,巴尔喀什湖移交沙俄。。
详细百科解释
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