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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
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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...

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。

During 1990~1991,temperature and humidity in the natural braod-leaved avergreen forest were measured in the scenic spot of Hangzhou and were compared with the data in the same period from Hangzhou Meteorolo-gical Station.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...

During 1990~1991,temperature and humidity in the natural braod-leaved avergreen forest were measured in the scenic spot of Hangzhou and were compared with the data in the same period from Hangzhou Meteorolo-gical Station.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.Meanwhile,it increased the annual average minimum temperature and the annual average extreme minimum temperature of the ground surface by1.2~1.4℃ and 7.9~8.0℃.The daily range of the surface temperature inthe forest was lower than that in the urban district of Hangzhou.The foresthad a noticeable effect on the soil temperature below the ground surface,and it could lower the annual average temperature by 2.0~3.0℃.The mostobvious decrease of the surface temperature and the soil temperature appearedat 14: 00 in summer, and in winter, there was an increase of the temperaturein the forest to a certain extent. Air temperature changes in the forest hadthe same tendency with those of the soil temperature,but fluctuated withina narrow range. Annual average absolute humidity and relative humidity ofground layer in the forest were higher than those in the urban district ofHangzhou by 0.5~0. 6 hPa and 7%~8%,and the effect of increasing humidityoccurred most obviously at 14:00。

1990~1991年,观测了杭州风景区天然常绿阔叶林内的温度和湿度,并以此与杭州市气象台的同期气象资料进行对比分析。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℃;使年平均最低温度上升1.2~1.4℃,年极端最低温度上升7.9~8.0℃;使平均日较差下降13.3~14.6℃。对林内5~20cm深度地中温度的调节作用也甚为明显,可使年平均温度比市区下降2.0~3.0℃。对地表、地中温度的降温效应都以盛夏午后14:00前后最为显著,在严冬季节具有一定的增温效应。对林内近地层气温的调节趋势与地温基本一致,但调温幅度比地温小。可使林内近地层空气的年平均绝对湿度比市区提高0.5~0.6hPa,年平均相对湿度上升7%~8%,且都以午后14:00前后增湿最为明显。

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。

 
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