Air temperature at the summit of Mont Jacques-Cartier (Gaspé peninsula) 2012-2015
Abstract
The available dataset is the unique continuous measurement of the air temperature on the summit of Mont Jacques-Cartier (1263 m a.s.l.). This summit represents the highest peak of the Chic-Chocs Mountains in the Gaspé Peninsula. This unique site is characterised by typical periglacial landforms (e.g. sorted polygons, sorted stripes, blockfield), by a marginal alpine permafrost body and by a alpine tundra vegetation cover (Gray et al., 2017). Air temperature data are recorded every hour by a U22-001 datalogger (Hobo®; resolution of 0.2°C, accuracy of +/- 0.21°C), which is installed 1 m above the ground surface (GPS: 48°59,268 N; 65°56,937 W). The dataset covers the period 1/12/2012-23/09/2015. The data will be updated after each field trip.
Gray JT, Davesne G, Godin E, Fortier D. 2017. The Thermal Regime of Mountain Permafrost at the Summit of Mont Jacques-Cartier in the Gaspé Peninsula, Québec, Canada: A 37 Year Record of Fluctuations showing an Overall Warming Trend, Permafrost Periglacial Processes, 28, 266-274. DOI: 10.1002/ppp.1903.
Gray JT, Davesne G, Godin E, Fortier D. 2017. The Thermal Regime of Mountain Permafrost at the Summit of Mont Jacques-Cartier in the Gaspé Peninsula, Québec, Canada: A 37 Year Record of Fluctuations showing an Overall Warming Trend, Permafrost Periglacial Processes, 28, 266-274. DOI: 10.1002/ppp.1903.
Data citation
Fortier D., Davesne, G., Gray, J. 2017. Air temperature at the summit of Mont Jacques-Cartier (Gaspé peninsula) 2012-2015, v. 1.0. Nordicana D30, doi: 10.5885/45465CE-1CDBEA34D928494E.
Location map
Key references
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Gray J.T., Davesne G., Godin E., Fortier D. 2017. The Thermal Regime of Mountain Permafrost at the Summit of Mont Jacques-Cartier in the Gaspé Peninsula, Québec, Canada: A 37 Year Record of Fluctuations showing an Overall Warming Trend, Permafrost Periglacial Processes, 28, 266-274.
DOI: doi:10.1002/ppp.1903. -
Davesne G., Fortier D., Dominé F., Gray J.T. 2016. Wind driven snow conditions control the occurrence of contemporary marginal mountain permafrost in the Chic-Chocs Mountains, south-eastern Canada – a case study from Mont Jacques-Cartier, The Cryosphere.
DOI: doi:10.5194/tc-2016-211
Contributors
Godin , Étienne
Géocryolab, Département de Géographie, Université de Montréal
Acknowledgements
We thank the Parc National de la Gaspésie especially François Boulanger, Pascal Lévesque, and Claude Isabel for their assistance with logistical aspects of the research and for the use of facilities
Version history
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Version 1.0 (2012–2015)Updated May 25, 2017
You can request an older version by contacting nordicana@cen.ulaval.ca
Measurement sites
| Site | Latitude | Longitude | Altitude (m) | |
|---|---|---|---|---|
| Mont Jacques-Cartier | 48.986086 | -65.947858 | 1263 | More info |
Download
Data available for download are in ZIP format. Please properly cite the data when using it.
