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Abstract The thermal field within the firn layer on the Greenland Ice Sheet (GrIS) governs meltwater retention processes, firn densification with surface elevation change, and heat transfer from the surface boundary to deep ice. However, there are few observational data to constrain these processes with only sparse in situ temperature time series that do not extend through the full firn depth. Here, we quantify the thermal structure of Western Greenland’s firn column using instrumentation installed in an elevation transect of boreholes extending to 30 and 96 m depths. During the high‐melt summer of 2019, heat gain in the firn layer showed strong elevation dependency, with greater uptake and deeper penetration of heat at lower elevations. The bulk thermal conductivity increased by 15% per 100 m elevation loss due to higher density related to ice layers. Nevertheless, the conductive heat gain remained relatively constant along the transect due to stronger temperature gradients in the near surface firn at higher elevations. The primary driver of heat gain during this high melt summer was latent heat transfer, which increased up to ten‐fold over the transect, growing by 34 MJ m−2per 100 m elevation loss. The deep‐firn temperature gradient beneath the seasonally active layer doubled over a 270‐m elevation drop across the study transect, increasing heat flux from the firn layer into deep ice at lower elevations. Our in situ firn temperature time series offers observational constraints for modeling studies and insights into the future evolution of the percolation zone in a warmer climate.
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Firn temperature time series to 100 m depth at two sites along the west Expéditions Glaciologiques Internationales au Groenland (EGIG) line, Greenland 2019-2021
This archive contains firn temperature data collected at two sites in the western Greenland Ice Sheet percolation zone. The sites, T3 and Crawford Point (CP), are located along the Expéditions Glaciologiques Internationales au Groenland (EGIG) line. The data are time series of firn temperature measured in boreholes drilled to 100 m depth. The boreholes were drilled by hot water methods. The CP measurements span the period June to August, 2019. This borehole was drilled in 2018, so the temperature profile had fully recovered from the drilling thermal disturbance by the start of the time series. The T3 data span the period June 2019 to September 2021. This borehole was drilled in June 2019, so the time series of measurements includes the thermal recovery from drilling (several months) and two subsequent years. The dataset was collected as part of projects funded by the U.S. National Science Foundation. These measurements are associated with additional datasets collected as part of a NSF Arctic Observing Network project, and include measurements at multiple sites on the EGIG line of firn temperature and firn density/ice content.
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- Award ID(s):
- 1717939
- PAR ID:
- 10447793
- Publisher / Repository:
- NSF Arctic Data Center
- Date Published:
- Subject(s) / Keyword(s):
- Firn Temperature Percolation zone
- Format(s):
- Medium: X Other: text/xml
- Sponsoring Org:
- National Science Foundation
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