Postdoctoral Researcher at Stanford University
(Now an Assistant Professor at Georgia Insitute of Technology)
I am a geophysicist who studies ice sheets and their interrelation with our climate system. I synthesize radar sounding technique and numerical ice-sheet modeling to understand what "mechanisms" cause a glacier to accelerate. From satellite measurements of ice velocity, we know that different glaciers do not accelerate in the same way as one another under similar climate forcings. The core of my research is to better understand how glacial dynamics respond to a varying climate. I specifically focus on ice-sheet hydrology, as it is one of the most critical processes influencing glacier dynamic behavior. You can learn more about my work in the research section below.
Ice sheets have three hydrological systems: at the top, within the ice, and at the bottom. The interaction between these systems governs the ice-sheet water budget and controls the amount of water flushed into the oceans along the edges. Quantifying and monitoring water storage within these systems is critical to assessing how ice sheets are adjusting to climate changes and predicting their future stability. I develop and apply geophysical techniques, such as ice-penetrating radar sounding, to constrain an ice sheet's top-to-bottom water budget. One of my primary goals is to understand what controls water storage on both ice sheet and ice shelf environments in Greenland and Antarctica.
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On a seasonal scale, the presence of water at the ice-sheet bed can temporarily cause glacier velocity to speed-up; however, the ice sheet can experience vastly different responses to similar meltwater forcing, with one glacier showing massive speed-up while its neighbor barely notices the presence of water at its bed. I am fascinated by the complexity of how meltwater can interact with glacier motions and have made it a central focus of my research. I investigate this phenomenon by combining hydrological modeling and radar sounding to examine how meltwater drainage within an ice sheet evolves through time. Analysis of these results in the context of seasonal velocity observations from satellites will provide a clearer picture of what governs the response of individual glaciers to changes in meltwater.
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Water at the ice bed interacts with the ice-sheet thermal regime to create a complex ice flow structure. Changes in melting and freezing of water at the bed of the ice-sheet interior can cause glaciers to slow-down, and in dramatic cases, large ice streams to completely shut-down. Also at the bed, ice in contact with this water can soften and deform basal ice. This interaction of water and heat with basal ice makes it very challenging to apply traditional geophysical methods to constrain the basal condition, but by combining ice-sheet thermomechanical models with these observations, I can estimate these thermal effects to overcome this barrier and enable more robust constraints on the basal thermal conditions from geophysical data.
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In order to produce policy-relevant sea-level projections, ice-sheet modelers require real-world observations. Radar data is an excellent source of real-world observations, but the majority of models only use radar-derived measurements of ice thickness. This is limiting for predictive models because there is significantly more information that radar sounding can provide like bed-echo-strengths and internal ice layer properties. Bed-echo-strength radar values represent information about basal sliding and internal ice layer properties illustrate past glacier flow and the thermal structure of an ice sheet. I am actively engaged in developing new algorithms for assimilating all radar sounding data in ice-sheet models, which will aid in improving our understanding of glacier dynamics and sea-level prediction.
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