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1)  sluice contruction for drought irsigation and flood drainage
建闸灌旱排涝
2)  combat a drought and drain waterlogged fields
抗旱排涝
3)  tide-resistance and drainage sluice
挡潮排涝闸
1.
Liangduohenan Sluice is one of the four tide-resistance and drainage sluices operated in the Dongtai City at present.
梁垛河南闸是东台市目前仍在运行的四座挡潮排涝闸之一。
4)  flood and drought
旱涝
1.
This paper conducts the computation classification for the spring flood and drought situation in He Zhou by using the spring precipitation data in four weather stations of He Zhou during 1965-2004,and the z index,and the index of regional flood and drought.
利用贺州市四站1965~2004年春季降水资料,运用z指数和区域旱涝指数对贺州地区春季旱涝情况进行计算分类,并对重旱涝典型年份500hPa环流特征量和4月平均环流场展开分析,发现:贺州地区春季极易发生局部旱涝灾情,90年代以来重旱涝年份出现频率明显增大;在重旱年副高强度强,西伸脊点明显偏西,南支槽偏西偏弱,极涡中心偏东,亚洲中高纬高度偏低,在重涝年则相反。
2.
The variabilities of the summertime flood and drought events over the lower reach of the Yangtze River Valley (YRV) are examined in this paper by employing monthly mean observation data from 1958 to 1999.
作者统计分析了 1 95 8~ 1 999年 42年长江中下游地区夏季 5~ 8月旱涝事件的分布特征。
5)  drought and flood
旱涝
1.
Regional features of summer drought and flood in Northeast China and corresponding abnormal water-vapor transportation;
东北地区夏季旱涝的区域特征及水汽异常输送
2.
By using monthly averaged NCEP/NCAR reanalysis data of the atmospheric circulation and the data of summer precipitation in 40 meteorological stations in Shandong province from 1961 to 1998,the climate characteristics of precipitation in the summer of Shandong are analyzed,and the atmospheric circulation anomalies of drought and flood have been compared and analyzed.
应用1961~1998年的山东省40个代表站夏季降水资料及NCAR/NCEP再分析月平均资料,分析了山东夏季降水的气候特征,并对旱涝年的大气环流异常进行了合成对比分析。
3.
Based on grade data of drought and flood of Anhui in recent 554 years, variable regular are given by calculation method of departure coefficient, kurtosis coefficient, number of appearance, accumulative anomaly and so on.
基于安徽省近554年的旱涝等级资料,首先利用偏度系数、峰度系数、频次、累积距平等计算公式和方法进行旱涝变化规律的分析,结果表明:安徽省旱涝等级序列具有不对称分布即涝明显多于旱的非正态分布特征,呈现干燥期、湿润期的阶段性变化特征,以旱为主和以涝为主的现象间隔出现。
6)  flood/drought
旱涝
1.
Research on climate features of summer s flood/drought in Northwest China;
我国西北地区夏季旱涝气候特征研究
2.
Based on the fact that the predictor and predictand will change when some variateschange ahruptly in the climatic system, a multivariate threshold regression model for sum-mer flood/drought in the Lower ChangJiang valley is developed.
考虑了气候系统中一些变量突变时对预测关系的改变作用,用多元门限回归模型的建模方法建立长江下游地区夏季旱涝趋势预测模型。
3.
Experimental research has been made into short-term climate prediction of flood/drought in spring,monsoon and typhoon seasons and autumn and winter seasons.
利用最优子集、神经网络、EOF-CCA和均生函数4种常用统计方法,对福建春季、前汛期、后汛期和秋冬季进行年度、季度旱涝的短期气候预测试验,采用统一的评分标准评定。
补充资料:帛尸梨密多罗(晋建康建初寺)《高僧传》卷一
【帛尸梨密多罗(晋建康建初寺)《高僧传》卷一】
帛尸梨密多罗。此云吉友。西域人。时人呼为高座。传云。国王之子当承继世。而以国让弟。闇轨太伯。既而悟心天启。遂为沙门。密天姿高朗风神超迈。直尔对之。便卓出于物。晋永嘉中。始到中国。值乱仍过江止建初寺。丞相王导一见而奇之。以为吾之徒也。由是名显。太尉庾元规光禄周伯仁太常谢幼与廷尉桓茂伦。皆一代名士。见之终日累叹。披衿致契。导尝诣密。密解带偃伏悟言神解。时尚书令卞望之亦与密致善。须臾望之至。密乃敛衿饰容。端坐对之。有问其故。密曰。王公风道期人。卞令轨度格物。故其然耳。诸公于是叹其精神洒厉皆得其所。桓廷尉尝欲为密作目。久之未得。有云。尸梨密可谓卓朗。于是桓乃咨嗟绝叹。以为标题之极。太将军王处仲在南夏。闻王周诸公皆器重密。疑以为失。及见密乃欣振奔。至一面尽虔。周顗为仆射。领选临入过造密。乃叹曰。若使太平之世尽得选此贤。真令人无恨也。俄而顗遇害。密往省其孤。对坐作胡呗三契。梵响凌云。次诵咒数千言。声音高畅颜容不变。既而挥涕收泪。神气自若。其哀乐废兴皆此类也。王公尝谓密曰。外国有君一人而已。密笑曰。若使我如诸君。今日岂得在此。当时为佳言。密性高简不学晋语。诸公与之语言。密虽因传译。而神领意得顿尽言前。莫不叹其自然天拔悟得非常。密善持咒术所向皆验。初江东未有咒法。密译出孔雀王经明诸神咒。又授弟子觅历高声梵呗传响于今。晋咸康中卒。春秋八十余。诸公闻之痛惜流涕。桓宣武每云少见高座称其精神著出当年。琅玡王玟师事于密。乃为之序曰。春秋吴楚称子。传者以为先中国而后四夷岂不以三代之胤行乎殊俗之礼。以戎狄贪婪无仁让之性乎。然而卓世之秀。时生于彼。逸群之才。或侔乎兹。故知天授英伟。岂俟于华戒。自此以来唯汉世有金日磾。然日磾之贤尽于仁孝忠诚德信纯至。非为明达足论。高座心造峰极。交俊以神。风领朗越过之远矣。密常在石子冈东行头陀。既卒因葬于此。成帝怀其风为树刹冢所。后有关右沙门来游京师。乃于冢处起寺。陈郡谢琨赞成其业。追旌往事。仍曰高座寺也。
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