Mass: Quebec

 

The Quebec 1 and 2 mass balance sites were adjacent to one another. Quebec 1 was undeformed ice with an initial thickness of 0.85 m. Quebec 2 was thicker ice, a slight hummock. There were four thickness gauges at Quebec 1 (24, 56, 49, 321) and four gauges at Quebec 2 (12, 48, 99, 320). In addition, three gauges (139, 202, 203) were installed in first-year ice that started growing in January when a lead opened near Quebec. There is a record of Quebec 1 temperature and Quebec 2 temperature. Quebec 2 also had an above ice acoustic sensor that monitored changes in the position of the surface and a pressure sensor that measured changes in the overall mass balance of the floe. During the winter, a crack formed within a meter of the Quebec 1 thermistor string. Early in the summer this crack melted open. In early August 1998, Quebec broke away from the rest of the floe, ultimately drifting more than 3 km from the ship. 

 

Quebec 2 during installation in October 1997. The orange box contains a data logger.

Quebec 1 (left) and Quebec 2 (right) on July 1. Ponds were starting. Note the crack by the Quebec 1 thermistor string.

Frozen, snow-covered crack near Quebec 1 thermistor string before the onset of melt.

Photo from 25 July showing the same crack completely melted open. The many frozen cracks of winter transformed into nascent leads in summer.

Quebec 1 and 2 from the air on 16 July 1998 . The crack near the Quebec 1 thermistor string is melting open. 

ec Quebec 1 and 2 from the air on 5 August 1998 . After the divergence event of 2 August, Quebec became an island. 

 

 

 
                                          

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