Disturbances of Temperature-Depth Profiles by Surface Warming and Groundwater Flow Convection in Kumamoto Plain, Japan

Figure 10

Surface warming-forced temperature-depth profile variation at t = 0, 25, 50, 75, and 100 years under various water flow conditions: (a) only heat conduction, (b) x = 1000 m (recharge), (c) x = 15,000 m (intermediate), and (d) x = 29,000 m (discharge).

(a)

(b)

(c)

(d)