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Recent Variations in Temperature, Precipitation, and Streamflow in the Rio Grande and Pecos River Basins of New Mexico and Colorado

机译:新墨西哥州和科罗拉多州里奥格兰德河和佩科斯河流域温度,降水和水流的近期变化

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摘要

Trends in climatic and hydrologic data from the Rio Grande and Pecos River basin are analyzed over an approximately 40-year period (1960 to 2000). Mann-Whitney tests for changes between halves of the record and between more recent decades, and Mann-Kendall tests for trend over the 40 years of record, are applied to monthly averages from 35 temperature stations and 63 precipitation stations. Similarly, the 15 hydrometric stations meeting the criteria of the Hydro-Climatic Data Network are examined using Mann-Whitney and Mann-Kendall tests to 5-day averages of daily mean streamflow. To distinguish regions that exhibit similar patterns of climatic variation, temperature and precipitation results from the Mann-Kendall test are used as inputs to a cluster analysis. Climatic variations in the region are consistent neither through time nor across space. Some areas have demonstrated recent increases in temperature or precipitation while others have displayed decreases in these same elements. In addition, many areas reveal climatic shifts in specific periods of the year that are in marked contj-ast with the trends observed in other periods and other places. Hydrologic variations are also not spatially homogeneous, but generally indicate higher streamflow,earlier onset to freshet, and generally larger freshet volumes in more recent decades.
机译:在大约40年的时间段(1960年至2000年)中,分析了里奥格兰德河和佩科斯河流域的气候和水文数据趋势。对35个温度站和63个降水站的月平均值进行了Mann-Whitney检验,以记录的两半之间和最近几十年之间的变化,Mann-Kendall检验了记录的40年趋势。同样,使用Mann-Whitney和Mann-Kendall测试对满足水文气候数据网络标准的15个水文站进行了检查,得出每日平均流量的5天平均值。为了区分表现出类似气候变化模式的区域,Mann-Kendall试验的温度和降水结果被用作聚类分析的输入。该区域的气候变化既不随时间变化,也不跨空间变化。一些地区显示出近期温度或降水增加,而其他地区显示出这些相同元素的下降。此外,许多地区显示出一年中特定时期的气候变化与其他时期和其他地方的趋势明显不同。水文变化在空间上也不是均一的,但通常表明水流较高,较早地开始生水,并且在最近的几十年中通常较大的生水量。

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