14.4
Imagine measuring snowfall in centimeters across Colorado over a 2-day period, with different regions receiving varying amounts. A contour map represents this variation across the state, showing lines of equal snowfall.
To find the average snow depth, we need to calculate the average value of the variable snowfall function over a rectangular region.
The total snowfall over the region can be expressed as a double integral. To estimate this integral using the midpoint rule, the region is divided into smaller equal sub-rectangles. Each sub-rectangle represents an equal portion of the total area.
Within each sub-rectangle, a midpoint is identified. These points serve as representative locations for each section.
The snowfall is evaluated at each midpoint, providing an approximate value for each subregion. For each sub-rectangle, a contribution is obtained by multiplying its area by the corresponding snowfall value.
The contributions from all sub-rectangles are then summed to obtain an approximation of the total snowfall over the region. Finally, dividing this total by the area of the region gives the average snowfall.
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