首页> 外文OA文献 >Monitoring Inter- and Intra-Seasonal Dynamics of Rapidly Degrading Ice-Rich Permafrost Riverbanks in the Lena Delta with TerraSAR-X Time Series
【2h】

Monitoring Inter- and Intra-Seasonal Dynamics of Rapidly Degrading Ice-Rich Permafrost Riverbanks in the Lena Delta with TerraSAR-X Time Series

机译:使用TerraSAR-X时间序列监测莉娜三角洲快速退化的富冰多年冻土河岸的季节间和季节内动态

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Arctic warming is leading to substantial changes to permafrost including rapid Degradation of ice and ice-rich coasts and riverbanks. In this study, we present and evaluate a high spatiotemporal resolution three-year time series of X-Band microwave satellite data from the TerraSAR-X (TSX) satellite to quantify cliff-top erosion (CTE) of an ice-rich permafrost riverbank in the central Lena Delta. We apply a threshold on TSX backscatter images and automatically extract cliff-top lines to derive intra- and inter-annual CTE. In order to examine the drivers of erosion we statistically compare CTE with climatic baseline data using linear mixed models and analysis of variance (ANOVA). Our evaluation of TSX-derived CTE against annual optical-derived CTE and seasonal in situ measurements showed good agreement between all three datasets. We observed continuousuderosion from June to September in 2014 and 2015 with no significant seasonality across the thawing season. We found the highest net annual cliff-top erosion of 6.9 m in 2014, in accordance with above-average mean temperatures and thawing degree days as well as low precipitation. We found high net annual erosion and erosion variability in 2015 associated with moderate mean temperatures but above average precipitation. According to linear mixed models, climate parameters alone could not explain intra-seasonal erosional patterns and additional factors such as ground ice content likely drive the observed erosion. Finally, mean backscatter intensity on the cliff surface decreased from -5.29 to -6.69 dB from 2013 to 2015, respectively, likely resulting from changes in surface geometry and properties that could be connected to partial slope stabilization. Overall, we conclude that X-Band backscatter time series can successfully be used to complement optical remote sensing and in situ monitoring of rapid tundra permafrost erosion at riverbanks and coasts by reliably providing information about intra-seasonal dynamics.
机译:北极变暖正导致永久冻土发生重大变化,包括冰层迅速退化以及冰层丰富的海岸和河岸。在这项研究中,我们提出并评估了TerraSAR-X(TSX)卫星的X波段微波卫星数据的高时空分辨率三年时间序列,以量化富冰冻土河岸的悬崖顶蚀(CTE)。中央莉娜三角洲。我们对TSX背向散射图像应用阈值,并自动提取悬崖顶线以得出年度内和年度CTE。为了检查侵蚀的驱动因素,我们使用线性混合模型和方差分析(ANOVA)对CTE与气候基线数据进行了统计比较。我们对TSX衍生的CTE与年度光学衍生的CTE和季节性原位测量的评估表明,这三个数据集之间都具有良好的一致性。我们观察到2014年和2015年6月至9月连续退缩,整个融化季节没有明显的季节性变化。根据高于平均水平的平均气温和融化天数以及低降水量,我们发现2014年的最高悬崖峭壁年净侵蚀量为6.9 m。我们发现2015年的年净侵蚀量和侵蚀量变异性较高,平均气温适中,但降水量高于平均水平。根据线性混合模型,仅凭气候参数无法解释季节内的侵蚀模式,而诸如地面冰含量等其他因素则可能导致观测到的侵蚀。最后,从2013年到2015年,悬崖表面的平均背向散射强度分别从-5.29 dB下降至-6.69 dB,这可能是由于表面几何形状和特性的变化(可能与部分边坡稳定有关)引起的。总的来说,我们得出的结论是,X波段反向散射时间序列可以可靠地提供有关季节内动态的信息,从而可以成功地用于补充光学遥感和对河岸和海岸快速冻原永久冻土侵蚀的现场监测。

著录项

相似文献

  • 外文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号