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Dynamics of Rift-opening calving dominant ice shelves and the analysis of its influencing factors

机译:裂口开放式占领冰货架的动态及其影响因素分析

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Landsat imagery of TM, ETM+ and L8 were taken as data source and the partial least-squares regression was conducted to investigate the response of dynamics of Ross Ice Shelf and Ronne-Flchner Ice Shelf belonging to rift-opening calving dominant ice shelves to the natural environmental factors. The results show that, these two ice shelves have been extending to the ocean at nearly uniform speed along each coastline. The factors influence the dynamics of ice shelves via affecting the glacier movement. Surface air temperature and surface wind velocity facilitate the extension of ice shelves. Sea surface temperature, near-surface current velocity and atmospheric precipitable water are negatively correlated with the areal changes of ice shelves along each coastline. Salinity of the ocean is influenced by the ice shelves, and is positively correlated to the areal changes.
机译:TM,ETM +和L8的Landsat图像被视为数据源,并进行了部分最小二乘回归,以调查罗斯冰货架和罗恩 - 佛罗特冰货架的响应,属于裂口开口的碎冰冰货架到自然 环境因素。 结果表明,这两种冰架一直沿着每个海岸线的几乎均匀的速度延伸到海洋。 这些因素通过影响冰川运动来影响冰架的动态。 表面空气温度和表面风速有助于冰架的延伸。 海表面温度,近表面电流速度和大气沉淀水与每个海岸线的冰架的面积变化负相关。 海洋的盐度受到冰架的影响,与面积变化呈正相关。

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