1. Constraints on the Cryohydrological Warming of Firn and Ice in Greenland From Rayleigh Wave Ellipticity Data.
- Author
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Jones, G. A., Ferreira, A. M. G., Kulessa, B., Schimmel, M., Berbellini, A., and Morelli, A.
- Subjects
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GREENLAND ice , *RAYLEIGH waves , *MELTWATER , *ICE mechanics , *ICE sheets , *ANTARCTIC ice - Abstract
Rayleigh wave ellipticity measurements from seismic ambient noise recorded on the Greenland Ice Sheet (GrIS) show complex and anomalous behavior at wave periods sensitive to ice (T < 3–4 s). To understand these complex observations, we compare them with synthetic ellipticity measurements obtained from synthetic ambient noise computed for various seismic velocity and attenuation models, including surface wave overtone effects. We find that in dry snow conditions within the interior of the GrIS, to first order the anomalous ellipticity observations can be explained by ice models associated with the accumulation and densification of snow into firn. We also show that the distribution of ellipticity measurements is strongly sensitive to seismic attenuation and the thermal structure of the ice. Our results suggest that Rayleigh wave ellipticity is well suited for monitoring changes in firn properties and thermal composition of the Greenland and Antarctic ice sheets in a changing climate. Plain Language Summary: Surface meltwater is increasingly being routed and distributed through the Greenland Ice Sheet (GrIS) changing the mechanical and thermal properties of the ice and resulting in accelerated ice flow. Here we observe complex and anomalous Rayleigh wave ellipticity measurements at periods sensitive to the ice structure. We compare our observations with ellipticity measurements made on simulated seismic noise for various seismic velocity and attenuation models. We demonstrate that in the interior of the GrIS the ellipticity is sensitive to the accumulation and densification of snow as it compacts into glacier ice. The variation in the measurements is strongly sensitive to the thermal structure of the ice sheet which we estimate to be warmer than about −10°. These results demonstrate that Rayleigh wave ellipticity is well suited for monitoring changes in firn properties and thermal composition of the Greenland and Antarctic ice sheets in a changing climate. Key Points: Densification of snow into firn has a first order effect on ellipticity measurements at periods sensitive to the iceThe distribution of ellipticity measurements is sensitive to the thermal composition of the iceEllipticity is a promising method for long term monitoring of ice properties and thickness beneath the seismic station [ABSTRACT FROM AUTHOR]
- Published
- 2023
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