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

Table 5

Sensitivity coefficients of subsurface temperature at x = 1000 m, 15,000 m, and 29,000 m to aquifer thermal diffusivity () and hydraulic conductivity ().

Parameter	Sensitivity coefficient (dimensionless) at x=			Global sensitivity coefficient
	1000 m	15,000 m	29,000 m
	1.388	0.464	0.981	0.944
	0.318	0.265	0.733	0.439