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An analysis of precipitation data from the Antarctic base Faraday/Vernadsky

机译:南极基地法拉第/韦尔纳斯基的降水数据分析

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A recent study on cloud observations reports an increase in total cloud cover at Faraday/Vernadsky since 1960 in the annual and wintertime data. The aim of this present study is to investigate whether this increase in total cloud cover has influenced the precipitation in this region. For this purpose, precipitation observations at the Antarctic base Faraday/Vernadsky between 1960 and 1999 were analysed. A positive trend, significant at the 5% level, was found in the number of precipitation events recorded during winter, showing an increase of 13 events per decade. The annual number of precipitation days has increased by 5.7 per decade during the period of investigation, with highest increase rates being observed in winter and autumn. The characteristics of these findings confirm that results previously published though trends presented here are ~50% smaller due to a more thorough data quality control of the observational data. These results indicate that an increase in total cloud cover at Faraday/Vernadsky observed since 1960 in the annual and wintertime data is reflected in higher numbers of precipitation events and days. Analyses of the precipitation type found an increase in the proportion of events of non-frozen precipitation, which is significant (1% level) on an annual basis as well as in spring and autumn (both significant at 5% level). This is a clear manifestation of the year round temperature increase observed over the Antarctic Peninsula. The increase in non-frozen precipitation will have reduced the albedo in the region and will thus have contributed to the temperature-albedo feedback. To refreeze rain that is draining through glaciers energy is extracted from the surrounding ice, thereby physically corroding the ice. This will have contributed to the observed retreat of glaciers around the Antarctic Peninsula. As non-frozen precipitation falling on frozen ground cannot be stored but instead runs off, less water will be available for the ecosystem.
机译:最近一项有关云观测的研究报告称,自1960年以来,法拉第/韦尔纳斯基的年和冬季数据总云量有所增加。本研究的目的是调查总云量的增加是否影响了该地区的降水。为此,分析了南极基地法拉第/维纳斯基在1960年至1999年之间的降水观测结果。在冬季记录的降水事件数量中发现了一个积极的趋势,在5%的水平上很显着,显示每十年增加13个事件。在调查期间,每年的降水日数每十年增加了5.7天,而冬季和秋季的增长率最高。这些发现的特征证实,由于对观测数据进行了更彻底的数据质量控制,因此尽管此处呈现的趋势以前公布的结果也要小50%。这些结果表明,自1960年以来在年度和冬季数据中观测到的法拉第/韦纳斯基的总云量增加反映在降水事件和天数的增加上。对降水类型的分析发现,非冻结降水事件的比例有所增加,这在年度以及春季和秋季均显着(1%水平),在春季和秋季均显着(均为5%水平)。这是南极半岛全年温度升高的明显表现。非冻结降水的增加将减少该地区的反照率,从而有助于温度-反照率的反馈。为了重新冻结通过冰川排出的雨水,需要从周围的冰中提取能量,从而对冰进行物理腐蚀。这将有助于观测到的南极半岛冰川退缩。由于无法存储落在冻结地面上的非冻结降水,而是流失,因此生态系统的可用水将减少。

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