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Trend Analysis In Icelandic Discharge, Temperature And Precipitation Series By Parametric Methods

机译:用参数法对冰岛排放量,温度和降水序列的趋势分析

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This paper presents results of analyses by parametric methods of annual means of temperature, precipitation and discharge, and of seasonal maximum precipitation at 17, 28 and 10 Icelandic stations, respectively, for the period 1961-2000. Trends in mean seasonal temperature and precipitation are in broad agreement with results found by other authors using other methods. A positive trend appears in both mean annual temperature and mean temperatures in most seasons. Annual mean precipitation trends are positive in most seasons except for negative trends in the September-November season in the south. Additionally, positive trends appear in maximum one-, three- and five-day precipitation, both during the spring and autumn, except at a group of stations in central Iceland. Some of the positive trends in mean annual and seasonal precipitation may, however, be attributed to the positive trend in temperature which may have influenced gauge catch. Trends in mean annual and seasonal discharge are small and statistically insignificant; the trends found in temperature and precipitation do not all relate directly to trends in discharge but suggest hypotheses for further study of the relationships between them.
机译:本文介绍了通过参数方法对1961-2000年期间分别在17、28和10个冰岛气象站进行的年度温度,降水和流量平均值以及季节性最大降水量分析的结果。平均季节温度和降水的趋势与其他作者使用其他方法得出的结果大致吻合。年平均温度和大多数季节的平均温度均呈正趋势。在大多数季节,年平均降水量趋势为正,但南部的9-11月季节为负趋势。此外,春季和秋季,除了冰岛中部的一组气象站外,最大的一日,三日和五日降水出现积极趋势。但是,平均年降水量和季节降水量的某些积极趋势可能归因于温度的积极趋势,而温度的积极趋势可能已经影响了仪表的捕获。年均和季节性排放量的趋势很小,在统计上微不足道;温度和降水的趋势并非都与排放趋势直接相关,但提出了进一步研究两者之间关系的假设。

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