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Snowmelt Monitoring. Snowmelt was monitored at a site c. 3km North-East of the Polar Continental Shelf Project (PCSP) base (74 o 43’07” N, 94 o 59’19”

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Presentation on theme: "Snowmelt Monitoring. Snowmelt was monitored at a site c. 3km North-East of the Polar Continental Shelf Project (PCSP) base (74 o 43’07” N, 94 o 59’19”"— Presentation transcript:

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2 Snowmelt Monitoring. Snowmelt was monitored at a site c. 3km North-East of the Polar Continental Shelf Project (PCSP) base (74 o 43’07” N, 94 o 59’19” W), near Resolute, Cornwallis Island, in the Canadian High Arctic. The region is well within the zone of continuous permafrost, and the mean annual air temperature (1947-1990) is -16.4 o C, reaching a monthly high in July of 4.2 o C. Winter endures for 8-9 months of the year, usually from mid-September to early-June, with the main snowmelt season beginning in mid-June and lasting for as little as one week or up to 3-4 weeks. A meteorological tower was set-up on June 1 st at a FLAT site and recorded a range of atmospheric and radiation data throughout the melt season. The 2000 spring snowmelt at Resolute was fairly typical, with temperatures rising above freezing from June 7 th and sustained melt occurring after June 15 th with warmer air temperatures. Various snow data were also acquired, such as a vertical temperature profile of the snow pack; snow ablation was monitored using a snow line above the snow (to measure surface changes) and surface density measurements taken, to yield a snow ablation curve for the site. Snowmelt took approximately 29 days to complete, from the first day of above 0 o C temperatures until snow cover was completely eliminated from the FLAT site and it’s immediate vicinity (c. 1 km 2 ).

3 Location of Cornwallis Island in the Canadian High Arctic Location of Flat Site Cornwallis Island N N

4 The Flat Site, Pre-Melt.

5 Flat Site, Mid-melt

6 Flat Site, Post/Late-melt.

7 Snow Ablation Curve at the FLAT site, Spring 2000, Resolute.

8 Contributors… David Jones, Graduate Student,York University, Toronto, Canada Dr. Kathy Young, York University, Toronto, Canada The authors wish to gratefully acknowledge the following for financial and logistical support: Polar Continental Shelf Project (PCSP), Natural Sciences Engineering & Research Council (NSERC), The Arctic Institute of North America (AINA). Prof. Ming-ko Woo, MacMaster University, Hamilton, Canada.


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