Research Article
Disturbances of Temperature-Depth Profiles by Surface Warming and Groundwater Flow Convection in Kumamoto Plain, Japan
Figure 9
2D diagrams showing (a) initial thermal distribution, (b) thermal distribution at tā=ā100 years with linearly increasing surface temperature, and (c) differences in thermal distributions between (b) and (a). The dashed lines with arrows represent the heat flow profile.