开启世界尽头的气象观测:十九世纪末二十世纪初巴塔哥尼亚南部月平均气温气候学

Climate Pub Date : 2024-04-09 DOI:10.3390/cli12040051
P. Canziani, S. G. Lakkis, A. Yuchechen, Oscar Bonfilli
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引用次数: 0

摘要

对十九世纪末和二十世纪初巴塔哥尼亚南部的月平均气温进行了气候分析,这是国际数据拯救地球大气环流重建(ACRE)计划在阿根廷的合作伙伴关系的一部分,同时还分析了具有区域和全球记录的其他数据源。结合这些不同来源的数据,对巴塔哥尼亚沿海地区(包括火地岛)南纬 42 度至 55 度之间的 11 个地点进行了研究。此外,还使用了 1880-1920 年期间的 HadSST 月/季场数据。既考虑了月平均温度值和季节温度值,也考虑了时间序列的变化。他们的分析表明,与南半球的平均结果相比,研究区域内的表现是一致的,其特点是十九世纪晚期偏暖,二十世纪早期偏冷。这也与巴塔哥尼亚沿岸的海温变化和半球记录相一致。在有观测资料的情况下,与现今观测资料进行比较,也得出了一致的结论。研究期间的低频变率,即周期超过 3 年的变率,与目前的变率一致。对 1901-2020 年期间特雷利乌和里奥加耶戈斯的趋势估计显示出显著的趋势,与这两个纬度的半球变暖相一致。
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Unlocking Weather Observations at the End of the World: Late-XIX and Early-XX Century Monthly Mean Temperature Climatology for Southern Patagonia
A climate analysis of the monthly mean temperatures of Southern Patagonia during the late-XIXth and early-XXth centuries was carried out as part of the international data rescue Atmospheric Circulation Reconstructions over the Earth (ACRE) program partnership in Argentina, together with other data sources with regional and global records. The data from these diverse sources were combined to carry out a study in the coastal region of Patagonia, including Tierra del Fuego, between 42° S and 55° S for 11 locations. Furthermore, HadSST monthly/seasonal fields during the period 1880–1920 were also used. Both mean monthly and seasonal temperature values and timeseries variability were considered. Their analysis shows consistent behavior within the study region and compared to Southern Hemisphere mean results, which are characterized by a warm late-XIX century and a cooler early-XX century. This is also in agreement with SST variability along the coasts of Patagonia and hemispheric records. A comparison with present-day observations, where available, also yields consistent behavior. Low-frequency variability, i.e., in periods longer than 3 years, during the study period is consistent with present variability. Trend estimates at Trelew and Rio Gallegos for the period 1901–2020 yield significant trends, consistent with hemispheric warming at their latitudes.
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