助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   极端最高温度 在 气象学 分类中 的翻译结果: 查询用时:0.04秒
图标索引 在分类学科中查询
所有学科
气象学
建筑科学与工程
生物学
林业
更多类别查询

图标索引 历史查询
 

极端最高温度
相关语句
  extreme maximum temperature
    Slight change was detected in density and frequency of diurnal extreme maximum temperature annually in 1955~2004a. But there was apparent difference in two periods: 1955~1982a、 1976~2004a.
    日间极端最高温度和频数虽然在整个研究时段内变化较小,但在1955~1987a、1984~2004a两个时间段内有明显的差异。
短句来源
    The results showed that this kind forest had the most remark-able effect on the ground surface temperature within the forest. The forest decreased the annual everage temperature,the annual average maximum temperature and the annual average extreme maximum temperature of theground surface by 2.6~3.3℃,12.1~13.2℃,and 25.3~29.4℃ respectively.
    其结果表明:天然常绿阔叶林对林内地表温度的调节效应最为显著,林内年平均温度比市区下降2.6~3.3℃,年平均最高温度下降12.1~13.2℃,年极端最高温度下降25.3~29.4℃;
短句来源
  extreme maximum temperature
    Slight change was detected in density and frequency of diurnal extreme maximum temperature annually in 1955~2004a. But there was apparent difference in two periods: 1955~1982a、 1976~2004a.
    日间极端最高温度和频数虽然在整个研究时段内变化较小,但在1955~1987a、1984~2004a两个时间段内有明显的差异。
短句来源
    The results showed that this kind forest had the most remark-able effect on the ground surface temperature within the forest. The forest decreased the annual everage temperature,the annual average maximum temperature and the annual average extreme maximum temperature of theground surface by 2.6~3.3℃,12.1~13.2℃,and 25.3~29.4℃ respectively.
    其结果表明:天然常绿阔叶林对林内地表温度的调节效应最为显著,林内年平均温度比市区下降2.6~3.3℃,年平均最高温度下降12.1~13.2℃,年极端最高温度下降25.3~29.4℃;
短句来源
  extremely highest temperature
    The results indicate that the evergreen and deciduous broadleaf mixed forest is the optimal living vegetation community for Guizhou golden Monkey, and the suitable annual temperature is 8-15 C, the extremely lowest temperature is 2.5 C, the extremely highest temperature is 25 C, and the optimal living altitude is 1500-1700 m.
    结果表明常绿针阔混交林是黔金丝猴的最佳生存的植被群落,其最适宜的年均温度为8~15C,极端最低温度为-2.5C,极端最高温度为25C,最适宜生存的海拔高度为1500~1700m。
短句来源
  “极端最高温度”译为未确定词的双语例句
    The results showed that compared with control,the average temperature of daytime,maximum temperature and temperature difference in the canopy in the shading treatments decreased by 1.47~4.42℃,3.95~7.26℃ and 3.33~8.44℃ respectively,relative humidity of daytime and the daily minimum relative humidity in the canopy were respectively increased by 4.31%~12.31% and 3.27%~12.62%.
    结果表明:与不遮荫的对照处理相比,遮荫后,(1)树冠层的白昼平均温度、日极端最高温度和温度日较差分别下降了1.47~4.29℃、3.95~7.26℃和3.33~8.44℃;
短句来源
    So the change of minimum and maximal temperature are dissymmetrical.
    极端最高温度在东部普遍下降,最低最高温度变化具有不对称性。
短句来源
    Fine meteorological factors of 15 counties in the major bamboo producer areas of Guangxi Province were analyzed by principal component analysis and by means of the multivariate regression analysis of a multiple statistic method. The results indicated that the most important meteorological factors affecting bamboo, distribution and growth were the year's average temperature, ≥10℃, accumulated temperature, the highest annual temperature of many years, relative humidity, rainfall amount in the bamboo-shoot sprouting period, and yearly rainfall.
    本文对广西毛竹两个主产区(桂林地区、柳州地区)15个县的9项气象因子,应用多元统计分析中的主成分分析法、逐步回归分析法进行分析,结果表明:影响广西毛竹分布、毛竹生长的气象因子主要是年均温、≥10℃积温、年极端最高温度、相对湿度、发笋期雨量、年雨量。
短句来源
    The daily mean air temperature of 20 cm height,daily change of air temperature and daily maximum temperature in the areas without intercropping were higher or larger than those with intercropping of rye grass;
    结果表明,在热状况下,自然裸露区域桃园的空气温度日较差、日极端最高温度和20 cm 高度处的空气平均温度均高于黑麦草套种区,空气湿度则黑麦草套种区明显大于自然裸露区。
短句来源
    In addition, we found that the regional warming in northern China is closely related to reduction of minimum temperature days, and increase of maximum temperature days has intensified regional warming since 1990.
    另外,通过分析北方地区极端温度发生的频率及年极端温度和区域增暖的关系发现,当前的增温趋势与极端最低温度发生频率的减少和年最低温度的升高密切相关,近10年极端最高温度的增加加剧了增温的幅度。
短句来源
更多       
查询“极端最高温度”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
没有找到相关例句


Based on China′s extreme temperature data during 1951~1990, after minimizing the possible biases caused by station moving and urban heat island effect, and performing quality control procedure, this paper mainly studies the spatial and temporal distribution of variability and trends for extreme temperatures The results show that the variability of extreme minimum temperatures in most part of China in spring and autumn is greater than those in other seasons, especially in the northern China Variability of...

Based on China′s extreme temperature data during 1951~1990, after minimizing the possible biases caused by station moving and urban heat island effect, and performing quality control procedure, this paper mainly studies the spatial and temporal distribution of variability and trends for extreme temperatures The results show that the variability of extreme minimum temperatures in most part of China in spring and autumn is greater than those in other seasons, especially in the northern China Variability of extreme minimum temperatures in summer, however, is the smallest in most part of China There exist clear temporal (seasonal) differences in trends of China′s extreme temperatures The increasing trends of China′s extreme minimum temperatures in winter and autumn are both significant at the statistical t -test level of 99% and 97% respectively, while decreasing trend of all-China mean extreme maximum temperature is significant only in autumn at the statistical t -test level of 90% There also exist obvious regional differences in trends of extreme temperature in China Increasing trends of extreme minimum temperatures are obvious in all seasons in Northeast China, northern North China, central-eastern Inner Mongolia and the Sichuan-Tibet adjoining region, while decreasing trends of extreme maximum temperatures are obvious in the Yangtze River valley in autumn and winter, and in the lower reaches of the Yellow River in spring and summer

利用中国1951~1990年极端温度资料,在消除台站迁移和城市热岛效应的影响,并经过资料质量控制的基础上,对我国极端温度的变率和变化趋势的区域分布以及季节变化特征进行了分析研究。结果发现,近40年中国季极端最低温度的变率以春、秋两季为最大,大变率区域主要集中在北方;夏季是极端最低温度变率最小的季节。我国季极端温度的变化趋势存在较大的季节性差异;极端最低温度在冬、秋季增温趋势分别具有99%、97%的显著水平;极端最高温度只有在秋季,其降温趋势具有90%的显著水平。极端温度的变化趋势还存在明显的地域性差异;东北、华北北部、内蒙古中东部和川藏交界等地极端最低温度在各季表现出明显的增温趋势;长江流域地区极端最高温度在秋、冬季具有较为明显的降温趋势,黄河下游地区则在春、夏季表现出降温趋势。

Based on daily mean surface temperature of 110 stations over China from 1951 to 2000, trends of days and intensity of extreme temperature over arid and semi-arid area of China have been analyzed, and the trend of annual extreme temperature and differences among regions were shown; also temporal and spatial characteristics of extreme temperature and its relationship to regional warming have been discussed finally. The results show that there is a remarkable decreasing trend of days of minimum temperature over...

Based on daily mean surface temperature of 110 stations over China from 1951 to 2000, trends of days and intensity of extreme temperature over arid and semi-arid area of China have been analyzed, and the trend of annual extreme temperature and differences among regions were shown; also temporal and spatial characteristics of extreme temperature and its relationship to regional warming have been discussed finally. The results show that there is a remarkable decreasing trend of days of minimum temperature over arid and semi-arid areas during the period, and the beginning date of trend is different in different regions. Compared with the trend of minimum temperature, there is no obvious trend of maximum temperature days before the 1990s, but there is a remarkable increasing trend in maximum temperature days since 1990. Except days of extreme temperature, there is decrease trend of annual minimum temperature. The results have also shown the trend of zero temperature(under 0 o C), i.e., there is reduction trend of zero temperature days, and its beginning date delays, and ending date is earlier. In addition, we found that the regional warming in northern China is closely related to reduction of minimum temperature days, and increase of maximum temperature days has intensified regional warming since 1990.

建立在全国110站的日平均表面温度资料的基础上,着重分析了北方干旱和半干旱地区1951~2000年极端温度发生频率和强度的变化趋势,同时给出了年极端温度变化的变化趋势及区域差异;最后讨论了极端温度的时空特征和区域增暖的相互联系。结果指出:从1951到2000年,在北方干旱和半干旱地区,最低温度发生的频率显著减小,只是趋势开始的时间存在区域差异;与之不同的是,20世纪90年代以前,绝大多数地区最高温度发生的频率没有明显的变化趋势,但近10年却有一个明显的增加趋势;年极端日平均温度强度的分析结果表明:北方地区年最低温度存在显著的减小趋势。从各个分区零温度以下天数的统计结果来看,北方地区近50年来零温度的天数正在减少,且零温度的开始时间推后,结束时间提前。另外,通过分析北方地区极端温度发生的频率及年极端温度和区域增暖的关系发现,当前的增温趋势与极端最低温度发生频率的减少和年最低温度的升高密切相关,近10年极端最高温度的增加加剧了增温的幅度。

Shenyang locates in the sensitive region of global change. In past one hundred years, Shenyang temperature kept rising gradually by 1.7 Celsius degrees. This trend is more obvious in winter than in summer. Annual average temperature of Shenyang has a 12-years cycle, and temperature basically presents ladder form rise in every cycle. The cycle average temperature in winter of the end of 20th century rose about 2.8 Celsius degrees than that of the beginning of the century. According to variation tendency of the...

Shenyang locates in the sensitive region of global change. In past one hundred years, Shenyang temperature kept rising gradually by 1.7 Celsius degrees. This trend is more obvious in winter than in summer. Annual average temperature of Shenyang has a 12-years cycle, and temperature basically presents ladder form rise in every cycle. The cycle average temperature in winter of the end of 20th century rose about 2.8 Celsius degrees than that of the beginning of the century. According to variation tendency of the extreme temperature of the past 50 years, the minimum extreme temperature obviously rose; the maximum extreme temperature has not risen, but slightly dropped, so that the temperature difference reduced between winter and summer. The fact, the lowest average temperature and the highest average temperature of Shenyang both rise gradually with time, proves that not only the rise of minimum temperature leads to the increasing warm of Shenyang, but also the rise of maximum temperature is also important. Analysis of the winter circulation situation shows that: East Asia Trough, the weak ridge behind it, and Mongolian Ground High subsided obviously after the 80s of last century, and the cold air current passed Shenyang from the north is weakened consequently. This is one of reasons why Shenyang temperature is obviously increasing in winter.

沈阳地处全球温度变化的敏感带 ,在近百年的温度观测记录中 ,沈阳的温度变化呈逐渐上升之势 ,近百年增高约 1.7℃ ,这种上升趋势在冬季远比夏季明显。沈阳的年平均温度变化有一个 12a的周期 ,各周期温度基本呈阶梯状上升 ,2 0世纪末的周期冬季平均温度比世纪初的周期升温 2 .8℃左右。从近 5 0a的极端温度的变化趋势来看 ,极端最低温度明显升高 ,而极端最高温度并没有上升 ,变化趋势甚至略下降 ,以致冬、夏两季温差缩小。从沈阳的最低平均温度和最高平均温度变化来看 ,两者均随时间逐渐升高 ,说明沈阳市的增温不仅是最低温度升高造成的 ,最高温度的增温作用亦十分重要。从冬季环流形势分析来看 ,东亚大槽及其后弱脊和地面蒙古高压在上世纪 80年代、90年代明显减弱 ,使得冷空气向南侵袭的径向气流减弱 ,是导致位于冷空气通道中的沈阳冬季增温明显的原因之一

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关极端最高温度的内容
在知识搜索中查有关极端最高温度的内容
在数字搜索中查有关极端最高温度的内容
在概念知识元中查有关极端最高温度的内容
在学术趋势中查有关极端最高温度的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社