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No matter where you are on the planet - the day lengthens by four minutes each day, after the winter equinox, up to the summer solstice.
Depends on your latitude, but daylight gain is at a minimum after the winter solstice dwell point ( northern hemisphere) up to maximum daily gain at the spring equinox, gain per day then falls to 0 at the summer solstice dwell point, then this trend is reversed down to the winter solstice, completing the cycle. The graph of daylight hours in say england, resembles a sine curve.
There are 60 minutes in each hour. That 402 minutes (6 x 60 plus 42)
They are equal to each other.
There are 60 minute to each degree and 60 secons to each minute. 1 degree = 60 minutes 60 minutes = 3600 seconds