Dear Cryolist,
Since we are in the final throes of AGU abstract submission, please consider submitting an abstract to our AGU Fall meeting session C006: Arctic and Antarctic subglacial environments: Bridging the gap between modern observations and paleoclimate records. We encourage abstracts that highlight how modern observational and modeling efforts and paleoclimate records can be united to generate a more holistic understanding of ice sheet processes.
Since we are in the final throes of AGU abstract submission, please consider submitting an abstract to our AGU Fall meeting session C006: Arctic and Antarctic subglacial environments: Bridging the gap between modern observations and paleoclimate records. We encourage abstracts that highlight how modern observational and modeling efforts and paleoclimate records can be united to generate a more holistic understanding of ice sheet processes.
We are particularly excited about our invited talks from two dynamic early-career researchers, Emily Stevenson (University of Cambridge) and Benjamin Keisling (University of Massachusetts-Amherst).
Thank you,
Ryan Venturelli, University of South Florida
Chloe Gustafson, Lamont-Doherty Earth Observatory
Alex Michaud, Bigelow Laboratory for Ocean Sciences
Matt Siegfried, Colorado School of Mines
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Session ID: 77589
Section: Cryosphere
Description: Interconnected physical and geobiological systems in the subglacial environment modulate modern ice-sheet processes and leave an imprint on the sedimentary archive of paleo-ice-sheet behavior. A holistic view of the extent, magnitude, and timescale of glaciological, geochemical, geomorphic, hydrological, and geobiological processes can help refine our quantification of past, present, and future ice-sheet state. This session aims to bring together studies from a variety of fields to explore how modern observations and models of sub-ice systems can improve our interpretation of paleoclimate records and how inferences from paleoclimate records can help contextualize the relevance and magnitude of modern sub-ice processes. We encourage contributions that cover a wide-range of methods, including direct borehole sampling, in situ and remote geophysical observation, laboratory experiments, sedimentological analysis, biogeochemical studies, geochronological surveys, and modeling studies, in order to improve our collective process-to-paleo perspective.
Thank you,
Ryan Venturelli, University of South Florida
Chloe Gustafson, Lamont-Doherty Earth Observatory
Alex Michaud, Bigelow Laboratory for Ocean Sciences
Matt Siegfried, Colorado School of Mines
---
Session ID: 77589
Section: Cryosphere
Description: Interconnected physical and geobiological systems in the subglacial environment modulate modern ice-sheet processes and leave an imprint on the sedimentary archive of paleo-ice-sheet behavior. A holistic view of the extent, magnitude, and timescale of glaciological, geochemical, geomorphic, hydrological, and geobiological processes can help refine our quantification of past, present, and future ice-sheet state. This session aims to bring together studies from a variety of fields to explore how modern observations and models of sub-ice systems can improve our interpretation of paleoclimate records and how inferences from paleoclimate records can help contextualize the relevance and magnitude of modern sub-ice processes. We encourage contributions that cover a wide-range of methods, including direct borehole sampling, in situ and remote geophysical observation, laboratory experiments, sedimentological analysis, biogeochemical studies, geochronological surveys, and modeling studies, in order to improve our collective process-to-paleo perspective.
Ryan Venturelli (she, her, hers)
PhD Candidate
University of South Florida
College of Marine Science
www.marine.usf.edu
PhD Candidate
University of South Florida
College of Marine Science
www.marine.usf.edu
