Collaborative Research: Characterizing the Onset of Ice Stream Flow: A Ground Geophysical Field Program

0086297 Anandakrishnan该奖项支持一个为期四年的项目，旨在更好地了解罗斯海海湾(A-F)的冰流，这些冰流通过将大量冰快速移动到罗斯冰架的崩解前沿来排干西南极冰盖(WAIS)内部。该项目将研究这些冰流作为内部冰和漂浮冰架之间的缓冲的作用。它们快速流动的原因，控制它们当前接地线、边缘和头部位置的因素，对于任何对WAIS系统进行建模和预测冰盖未来的尝试都是至关重要的。对于六海岸的南极冰流，从无滑动(或全部内部变形)到以滑动为主的运动的转变被定义为“起始区”。为了充分理解WAIS(并充分模拟)WAIS，必须更好地了解这一起病区域。冰流的侧缘也是一种转变，需要更好的解释。关于起始区位置控制的假设范围从“纯粹的冰川学”到“纯粹的地质学”。因此，为了准确地模拟冰盖，需要基本的边界条件(粗糙度、湿度、耕作性质)和良好的冰下地质图，以显示沉积盆地的分布、厚度和性质。这些参数可以通过地震、雷达和其他地球物理方法进行估计。通过这次耦合地球物理实验，将详细研究冰流D的过渡区。此外，还将选择冰流C&A；D上的其他地点，以与冰流D上的主要地点进行比较和对比。主营地的选址将基于现有的雷达、GPS和卫星数据以及来自建模社区的输入。

0086297AnandakrishnanThis award supports a four year project to develop of better understanding the ice streams of the Ross Sea Embayment (A--F) which drain the interior West Antarctic Ice Sheet (WAIS) by rapidly moving vast quantities of ice to the calving front of the Ross Ice Shelf. The project will examine the role of these ice streams as buffers between the interior ice and the floating ice shelves. The reasons for their fast flow, the factors controlling their current grounding-line-, margin-, and head-positions are crucial to any attempt at modeling the WAIS system and predicting the future of the ice sheet. For the Antarctic ice streams of the Siple Coast, the transition from no-sliding (or all internal deformation) to motion dominated by sliding is defined as the "onset-region". To fully understand (and adequately model) the WAIS, this onset region must be better understood. The lateral margins of the ice streams are also a transition that need better explanation. Hypotheses on controls of the location of the onset region range from the "purely-glaciologic" to the "purely-geologic. Thus, to model the ice sheet accurately, the basal boundary conditions (roughness, wetness, till properties) and a good subglacial geologic map, showing the distribution, thickness, and properties of the sedimentary basins, are required. These parameters can be estimated from seismic, radar, and other geophysical methods. The transition region of ice stream D will be studied in detail with this coupled geophysical experiment. In addition, selected other locations on ice streams C & D will be made, to compare and contrast conditions with the main site on ice stream D. Site-selection for the main camp will be based on existing radar, GPS, and satellite data as well as input from the modeling community.