Figure 3
From: High geothermal heat flux in close proximity to the Northeast Greenland Ice Stream
“Dybet” section temperature anomalies. (a) Potential temperature difference (°C) averaged in the period between 2005 and 2015. The annual potential temperature difference is defined by the difference between in situ potential temperature and the average value between 260 and 280 m, i.e. the depth interval of the deep temperature minimum. (b) Box model of the deepest part of the “Dybet” section.
