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OUTLINES AND DYNAMICS OF EURARCTIC ICE CAPS IN ANOMALOUS GRAVITY FIELDS

机译:重力场中南极冰盖的轮廓和动力学

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The present investigation was aimed at studying spatialrnvariability and directional dynamics of inland ice/snowrnfields in relation to lateral variations of surface gravityrnat the sub-regional scale of tens to hundreds ofrnkilometres. The main goal was to evidence, bothrntheoretically and empirically, the existence andrnsignificance of gravitational impacts and associatedrnatmospheric effects on the status and fluctuations ofrnEurasia’s northernmost insular ice caps using spacebornernradar altimetry and interferometry data from thernEarth Explorers and Sentinel missions in conjunctionrnwith GOCE satellite gradiometry, ground-basedrnmeteorological time series and glaciologicalrnobservations. EO-based geodetic and cryosphericrnmodels describing the amount of solid precipitation,rnsnow drift and accumulation, glacier elevation changernand ice flow pattern were generated, homogenized andrncombined in the terrain-following reference frame. Thernmodels were then verified and applied to the diagnosisrnof glacioclimatic differences in arctic lowlands withrnstrong gravity anomalies. It was ascertained that surfacerngravity gradients modulate the atmospheric circulationrnand stability thereby influencing the intensity of localrnprecipitation and glacier growth and flow patterns in arncascade fashion.
机译:本研究旨在研究内陆冰雪域的空间变率和方向动力学,其与子重力在几十到几百千米的次区域尺度上的横向变化有关。主要目的是从理论上和经验上证明重力影响和相关的大气影响对欧亚大陆最北端的岛状冰盖的状态和波动的影响和意义,方法是使用太空出生的雷达测高仪和来自地球探索者和前哨任务的测距数据,结合GOCE卫星g,基于气象时间序列和冰川冰冻观测。基于EO的大地模型和冰冻圈模型描述了固体降水量,雪漂移和积聚,冰川高度变化和冰流模式,并在地形参考框架中进行了均化和组合。然后验证了这些模型,并将其应用于诊断重力异常强的北极低地的冰川气候差异。可以确定地表重力梯度调节了大气环流和稳定性,从而以级联的方式影响了局部降水的强度和冰川的生长和流动模式。

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