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A Study of Spatial and Temporal Distribution Law about Temperature and Precipitation in the Northeast of China

机译:东北地区温度和降水的时空分布规律研究

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This paper chooses precipitation and temperature data from 106 stations in the Northeast of China from 1951 to 2007.By using time series analysis Kriging analysis and other mathematical methods, combined with geographic information system technology, we analyzed precipitation and temperature change on a time and space of this region during nearly 60 years. The results show that the average temperature in the northeastern region exhibits an increasing tendency during nearly 60 years. The average temperature has stage characteristics. Temperature fluctuation was greater between 1951 and 1970. The temperature was mainly on the rise between 1971 and 1988 but the change range was relatively small. Since 1989, there appeared significant warming process and the trend was obvious. On the precipitation change, precipitation was decreasing tendency on this area and had bigger fluctuation. The period (1951-1970) is rainy period. The period (1971-1988) is less rain period and annual fluctuation range of precipitation is not big. Since 1989, annual fluctuation range of precipitation was relatively large. The period since 2000 was obvious less rain period. In the spatial distribution, the temperature change range was gradually strengthened from the southwest to the northeast between prophase and middle. Changes of precipitation have different degree decrease in most northeast area except northern mountain area. The temperature change range was gradually strengthened from the southeast to the northwest between middle and late. Precipitation changes range in the northern mountain of the area is smaller, while the western and south-western plain areas have larger precipitation change range.
机译:本文选取1951年至2007年东北地区106个站点的降水和温度数据,结合时间序列分析Kriging分析和其他数学方法,结合地理信息系统技术,分析了随时间和空间的降水和温度变化。该地区近60年的发展。结果表明,东北地区的平均温度在近60年中呈上升趋势。平均温度具有阶段特性。 1951年至1970年间温度波动较大。1971年至1988年间温度主要呈上升趋势,但变化幅度较小。自1989年以来,出现了明显的变暖过程,并且趋势很明显。从降水变化看,该地区降水呈下降趋势,波动较大。时期(1951-1970)是阴雨期。 1971-1988年为少雨期,年降水量波动幅度不大。自1989年以来,年降水量的波动幅度比较大。自2000年以来的时期明显少雨。在空间分布上,温度变化范围从前期到中期从西南向东北逐渐增强。除北部山区外,大多数东北地区的降水变化均有不同程度的下降。从中后期到东南部到西北部,温度变化范围逐渐增大。该地区北部山区的降水变化范围较小,而西部和西南平原地区的降水变化范围较大。

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