Figure $2.$ Changes in modeled drawdown $($at observation well$)$ versus time for each multiplier of specific storage

$($indicated by the different colored curves, where $1$ is the calibrated value$).$

While answering these discussion questions, think about both the physical interpretation and the

mathematical representation of how groundwater flow relates to the parameter being varied.

Sensitivity to storage:

A: Using Figure $2,$ discuss how the aquifer is sensitive to changes in the specific storage value; e$.$g$.$

what behavior $($in the time$-$drawdown curves$)$ do you note over the range of $S0$ factors and how

does that behavior relate to what you know about specific storage or storativity? $2$ pts

B: Why might the drawdown stabilize $($just above $88m)$ for the lower specific storage values $(0\mathrm{.}01$

and $0\mathrm{.}1$ factors$)?$