To find the approximate base of cumulus clouds, you need to calculate the difference between the air temperature and dewpoint at 1,000 feet MSL. In this case, the difference is 22 F (70 F - 48 F). For every 4.4 F drop in temperature per 1,000 feet, a cumulus cloud forms. So, you need to divide the temperature difference by 4.4 to find the altitude where the temperature reaches dewpoint, which gives you 5 (22 F / 4.4 = 5). Multiply this by 1,000 feet to get the approximate base of the cumulus clouds, which is 5,000 feet. Adding the initial altitude of 1,000 feet gives a total of 6,000 feet MSL as the correct answer.