%0 Journal Article %J Journal of Glaciology %D 2019 %T Non-linear glacier response to calving events, Jakobshavn Isbræ, Greenland %A Cassotto, Ryan %A Fahnestock, Mark %A Amundson, Jason M. %A Truffer, Martin %A Boettcher, Margaret S. %A De La Peña, Santiago %A Howat, Ian %K calving %K dynamic thinning %K Jakobshavn Isbræ %K terrestrial radar interferometry %K tidewater glaciers %X Jakobshavn Isbræ, a tidewater glacier that produces some of Greenland's largest icebergs and highest speeds, reached record-high flow rates in 2012 (Joughin and others, 2014). We use terrestrial radar interferometric observations from August 2012 to characterize the events that led to record-high flow. We find that the highest speeds occurred in response to a small calving retreat, while several larger calving events produced negligible changes in glacier speed. This non-linear response to calving events suggests the terminus was close to flotation and therefore highly sensitive to terminus position. Our observations indicate that a glacier's response to calving is a consequence of two competing feedbacks: (1) an increase in strain rates that leads to dynamic thinning and faster flow, thereby promoting destabilization, and (2) an increase in flow rates that advects thick ice toward the terminus and promotes restabilization. The competition between these feedbacks depends on temporal and spatial variations in the glacier's proximity to flotation. This study highlights the importance of dynamic thinning and advective processes on tidewater glacier stability, and further suggests the latter may be limiting the current retreat due to the thick ice that occupies Jakobshavn Isbræ's retrograde bed. %B Journal of Glaciology %V 65 %P 39–54 %G eng %R 10.1017/jog.2018.90 %0 Journal Article %J Journal of Glaciology %D 2017 %T Acquisition of a 3 min, two-dimensional glacier velocity field with terrestrial radar interferometry %A Voytenko, Denis %A Dixon, Timothy H. %A Holland, David M. %A Cassotto, Ryan %A Howat, Ian M. %A Fahnestock, Mark A. %A Truffer, Martin %A De La Peña, Santiago %K glacier flow %K glacier geophysics %K glaciological instruments and methods %X {\textless}p{\textgreater}Outlet glaciers undergo rapid spatial and temporal changes in flow velocity during calving events. Observing such changes requires both high temporal and high spatial resolution methods, something now possible with terrestrial radar interferometry. While a single such radar provides line-of-sight velocity, two radars define both components of the horizontal flow field. To assess the feasibility of obtaining the two-dimensional (2-D) flow field, we deployed two terrestrial radar interferometers at Jakobshavn Isbrae, a major outlet glacier on Greenland's west coast, in the summer of 2012. Here, we develop and demonstrate a method to combine the line-of-sight velocity data from two synchronized radars to produce a 2-D velocity field from a single (3 min) interferogram. Results are compared with the more traditional feature-tracking data obtained from the same radar, averaged over a longer period. We demonstrate the potential and limitations of this new dual-radar approach for obtaining high spatial and temporal resolution 2-D velocity fields at outlet glaciers.{\textless}/p{\textgreater} %B Journal of Glaciology %P 1–8 %G eng %U https://www.cambridge.org/core/product/identifier/S0022143017000284/type/journal{\_}article %R 10.1017/jog.2017.28