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

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2018/8451276/figures/8451276.fig.005a.svgz" name="8451276.fig.005a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Recharge type</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2018/8451276/figures/8451276.fig.005b.svgz" name="8451276.fig.005b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Intermediate type</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/geofluids/volume-2018/8451276/figures/8451276.fig.005c.svgz" name="8451276.fig.005c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Discharge type</td></tr></table>

<div>Classification of the observed temperature-depth profiles around 2012 (showing high similarity with the observed data around 2000 by Taniguchi et al. [<a href="/journals/geofluids/2018/8451276/#B17">17</a>]).</div>

Geofluids

fig5

Figure 5

Figure 5: Disturbances of Temperature-Depth Profiles by Surface Warming and Groundwater Flow Convection in Kumamoto Plain, Japan 