Differentiate \(L\left( t \right)\) with respect to \(t\) as follows:
\(\begin{aligned}L'\left( t \right) &= 0 + 2.8\cos \left( {\frac{{2\pi }}{{365}}\left( {t - 80} \right)} \right)\frac{d}{{dt}}\left( {\frac{{2\pi }}{{365}}\left( {t - 80} \right)} \right)\\ &= 2.8\cos \left( {\frac{{2\pi }}{{365}}\left( {t - 80} \right)} \right)\left( {\frac{{2\pi }}{{365}}} \right)\\ &= \frac{{5.6\pi }}{{365}}\cos \left( {\frac{{2\pi }}{{365}}\left( {t - 80} \right)} \right)\end{aligned}\)
At \(t = 80\), the rate of increase of the daylight can be obtained as follows:
\(\begin{aligned}L'\left( {80} \right) &= \frac{{5.6\pi }}{{365}}\cos \left( {\frac{{2\pi }}{{365}}\left( {80 - 80} \right)} \right)\\ &= \frac{{5.6\pi }}{{365}}\cos \left( 0 \right)\\ &= \frac{{5.6\pi }}{{365}}\left( 1 \right)\\ &\approx 0.0482\end{aligned}\)
Hence, the number of hours of daylight is increasing in Philadelphia on March 21 is \(0.0482\) hours per day.
At \(t = 141\), the rate of increase of the daylight can be obtained as follows:
\(\begin{aligned}L'\left( {141} \right) &= \frac{{5.6\pi }}{{365}}\cos \left( {\frac{{2\pi }}{{365}}\left( {141 - 80} \right)} \right)\\ &= \frac{{5.6\pi }}{{365}}\cos \left( {61} \right)\\ &= \frac{{5.6\pi }}{{365}}\left( {0.484} \right)\\ &\approx 0.02398\end{aligned}\)
Hence, the number of hours of daylight is increasing in Philadelphia on May 21 is \(0.02398\) hours per day.
The increase on May 21 is approximately half to that of March 21.