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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Spatial and temporal rainfall changes in the Jucar and Segura basins (1955-2016): Fine-scale trends
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Spatial and temporal rainfall changes in the Jucar and Segura basins (1955-2016): Fine-scale trends

机译:Jucar和Segura盆地的空间和时间降雨变化(1955-2016):细尺趋势

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A daily rainfall database covering the Jucar and Segura river basin authorities (east Iberian Peninsula, Spain) with high spatial density without gaps (890 series) has been created for the complete period 1955-2016. This has allowed a trend analysis of precipitation and dry/wet spells with a better spatial detail and coverage of key headwaters sectors than previous studies in this area. Results show significant negative trends for precipitation prevailing in Jucar area (an annual average loss of 51mm), especially towards its north interior headwaters. For this last one the annual loss exceeds 200mm (20% of precipitation). By contrast, certain pre-littoral sectors and most of the Segura area are remaining out of these negative trends (some local positive trends). However, the dry spells length and the number of dry days have increased in a generalized way (Jucar and Segura basins) with rainfall concentration in time and space. The decrease of moderate rainfall with greater precipitation effectiveness and weight in the key interior headwaters is the most significant. On the contrary, there has been an increase in extreme torrential rainfall (with poor effectiveness and high risk) at points on the coast and pre-littoral towards south of the region. These results are linked to a change in the frequency of three basic synoptic types identified in the region as rainfall origin.
机译:每天降雨量数据库覆盖Jucar和Segura River Basin Authoritues(East Iberian半岛,西班牙),在1955 - 2016年的完整期间已经创建了没有差距的高空间密度(890系列)。这允许对沉淀和干/湿法法术进行趋势分析,具有更好的空间细节和关键地面领域的覆盖范围,而不是此领域的先前研究。结果表明,JUCAR地区(年平均损失51mm)的降水普遍存在的显着消极趋势,尤其是朝北内部返波。对于这一持续年度损失超过200毫米(降水量的20%)。相比之下,某些预沿沿海地区和大多数Segura地区都留有这些负趋势(一些局部积极趋势)。然而,干法术长度和干燥的日子的数量以一般而言的方式(Jucar和Segura盆地)增加了时间和空间的降雨浓度。在关键的内部脑脊中具有更高降水量和重量的温度降雨量最为显着。相反,在海岸上的点和地区南部的北部地区的极端暴雨(有效性和高风险差)增加。这些结果与该区域中鉴定为降雨来源的三种基本概要类型的频率的变化相关联。

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