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Cluster analysis for validated climatology stations using precipitation in Mexico

机译:使用墨西哥的降水对经过验证的气候站进行聚类分析

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Annual average of daily precipitation was used to group climatological stations into clusters using the k-means procedure and principal component analysis with varimax rotation. After a careful selection of the stations deployed in Mexico since 1950, we selected 349 characterized by having 35 to 40 complete years of observations. The clustering of stations was performed three times: firstly according to the amount of precipitation; secondly according to their anomalies from the mean, resulting in their standard deviations grouping; and thirdly using the standardized anomalies, which resulted in a clustering according to the features of the trend and the structural changes of the series over the observing period. We identified two clusters that occupy northwestern and north-central Mexico; another at the center of the territory, between Sierra Madre Oriental and Sierra Madre Occidental; the following over the Sierra Madre Oriental; and a last one in the southeast of the territory, the southern coast of the Pacific Ocean and the Yucatán Peninsula, that overlaps with Sierra Madre Oriental group. Some stations of Yucatán Peninsula show similar characteristics to the northwestern cluster. The groupings were compared with the results of previous studies. The comparison indicates that regions are invariant in time and space and independent of the method of agregation and the stations sampled.
机译:日平均降水量的年平均值用于通过k均值程序和具有最大极大值旋转的主成分分析将气候站分组。在仔细选择自1950年以来在墨西哥部署的站点之后,我们选择了349个具有35至40个完整观测年的特征。站的聚类进行了三次:首先根据降水量;其次根据它们与平均值的异常,将它们的标准差分组。第三,利用标准化异常,根据趋势特征和观测期间序列的结构变化进行聚类。我们确定了两个集群,分别占据了墨西哥西北部和中北部。另一个位于领土中心,在东方马德雷山脉和西方马德雷山脉之间;以下是关于东方马德雷山脉的信息;最后一块是该领土的东南部,即太平洋南部海岸和尤卡坦半岛,与塞拉·马德雷东方集团重合。尤卡坦半岛的某些站点表现出与西北集群相似的特征。将这些分组与以前的研究结果进行比较。比较表明,区域在时间和空间上是不变的,并且与聚集方法和采样站无关。

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