Firn Temperatures from NW Greenland

Firn temperatures taken in the NW sector of the Greenland Ice Sheet in 2013. Temperatures were collected at locations where similar data was first observed by Carl Benson in 1952-55 (see Research Report 70 of the Snow Ice and Permafrost Research Establishment (SIPRE), Benson, 1962). These data show...

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Bibliographic Details
Main Author: Polashenski, Chris
Format: Dataset
Language:English
Published: NSF Arctic Data Center 2016
Subjects:
Firn
Ice sheet
temperature
Glacier Facies
Greenland
glacier
Ice
Ice Sheet
permafrost
Online Access:https://dx.doi.org/10.18739/a2bk16q0d
https://arcticdata.io/catalog/view/doi:10.18739/A2BK16Q0D
Description
Summary:Firn temperatures taken in the NW sector of the Greenland Ice Sheet in 2013. Temperatures were collected at locations where similar data was first observed by Carl Benson in 1952-55 (see Research Report 70 of the Snow Ice and Permafrost Research Establishment (SIPRE), Benson, 1962). These data show the long term change in firn temperature caused both by warming of mean annual temperatures, and an increase in percolation intensity. Data is used and further discussed in: Polashenski, C., Courville, Z., Benson, C., Wagner, A., Chen, J., Wong, G., ... & Hall, D. (2014). Observations of pronounced Greenland ice sheet firn warming and implications for runoff production. Geophysical Research Letters, 41(12), 4238-4246.

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