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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >MOTEDAS: a new monthly temperature database for mainland Spain and the trend in temperature (1951-2010)
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MOTEDAS: a new monthly temperature database for mainland Spain and the trend in temperature (1951-2010)

机译:MOTEDAS:西班牙大陆的新月度温度数据库和温度趋势(1951-2010年)

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摘要

We have developed a new monthly temperature database for mainland Spain by using the complete holding of maximum and minimum monthly mean values stored at the Spanish National Meteorological Agency (AEMet). After an exhaustive quality control exercise, the data set includes 1358 complete series, and a high-resolution grid (0.1 degrees x0.1 degrees) was calculated to analyse monthly trends. There has been an uneven increase in the mean values of maximum and minimum temperatures in the Spanish mainland from 1951 to 2010. The maximum monthly mean temperature values have risen mostly in late winter/early spring and the summer, while the minimum monthly mean temperature values have increased in summer, spring and autumn in southern areas. The spatial pattern of the diurnal temperature range shows a clear north-south gradient in summer, with positive trends in the north and negative trends in the south; furthermore, a negative pattern has been detected in the south in spring and autumn. These areas, particularly the Mediterranean coastland, have been subject to dramatic urbanization and land use changes during the past 30 years that may have affected nocturnal temperatures, in particular. Thus, warming processes in the Iberian Peninsula appear to be influenced both by global factors and more local ones, and their effects should be differentiated spatially.
机译:我们使用西班牙国家气象局(AEMet)所存储的最大和最小每月平均值的完整存储,为西班牙大陆开发了一个新的每月温度数据库。经过详尽的质量控制工作后,该数据集包含1358个完整序列,并计算了高分辨率网格(0.1度x0.1度)以分析每月趋势。从1951年到2010年,西班牙大陆的最高和最低温度平均值出现了不均衡的增长。最大每月平均温度值大部分在冬末/初春和夏季上升,而最低每月平均温度值在南部地区的夏季,春季和秋季有所增加。昼夜温度范围的空间格局在夏季表现出明显的南北梯度,北部为正趋势,南部为负趋势。此外,在春季和秋季,在南部发现了一种消极模式。这些地区,特别是地中海沿岸地区,在过去30年中经历了剧烈的城市化进程和土地利用变化,这尤其可能影响了夜间温度。因此,伊比利亚半岛的变暖过程似乎既受全球因素的影响,又受更多局部因素的影响,其影响应在空间上区分开。

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