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Baseline characteristics of climate, permafrost and land cover from a new permafrost observatory in the Lena River Delta, Siberia (1998–2011)

机译:西伯利亚利纳河三角洲新建的多年冻土观测站的气候,多年冻土和土地覆盖的基线特征(1998年至2011年)

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Samoylov Island is centrally located within the Lena River Delta at72° N, 126° E and lies within the Siberian zone ofcontinuous permafrost. The landscape on Samoylov Island consists mainly oflate Holocene river terraces with polygonal tundra, ponds and lakes, and anactive floodplain. The island has been the focus of numerousmultidisciplinary studies since 1993, which have focused on climate, landcover, ecology, hydrology, permafrost and limnology. This paper aims toprovide a framework for future studies by describing the characteristics ofthe island's meteorological parameters (temperature, radiation and snowcover), soil temperature, and soil moisture. The land surface characteristicshave been described using high resolution aerial images in combination withdata from ground-based observations. Of note is that deeper permafrosttemperatures have increased between 0.3 to 1.3 °C over the last fiveyears. However, no clear warming of air and active layer temperatures isdetected since 1998, though winter air temperatures during recent years havenot been as cold as in earlier years.Data related to this article are archived under: href="http://doi.pangaea.de/10.1594/PANGAEA.806233"target="_blank">http://doi.pangaea.de/10.1594/PANGAEA.806233 .
机译:萨摩洛夫岛位于利纳河三角洲以南72°,东经126°,位于西伯利亚连续多年冻土带内。萨摩洛夫岛上的景观主要包括全新世河阶地,多边形苔原,池塘和湖泊以及活跃的洪泛区。自1993年以来,该岛一直是众多多学科研究的重点,这些研究集中在气候,土地覆盖,生态学,水文学,多年冻土和森林学。本文旨在通过描述该岛的气象参数(温度,辐射和积雪),土壤温度和土壤湿度的特征,为今后的研究提供一个框架。已经使用高分辨率航拍图像结合来自地面观测的数据描述了地表特征。值得注意的是,在过去五年中,更深的永冻土温度在0.3至1.3°C之间升高。但是,自1998年以来,没有发现明显的空气变暖和活性层温度升高的趋势,尽管近年来的冬季气温没有以前几年的寒冷。 与本文相关的数据归类于:href = “ http://doi.pangaea.de/10.1594/PANGAEA.806233"target="_blank">http://doi.pangaea.de/10.1594/PANGAEA.806233 。

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