McCormick R A, Ludwig J H
Science. 1967 Jun 9;156(3780):1358-9. doi: 10.1126/science.156.3780.1358.
Theoretical considerations and empirical evidence indicate that atmospheric turbidity, a function of aerosol loading, is an important factor in the heat balance of the earth-atmosphere system. Turbidity increase over the past few decades may be primarily responsible for the decrease in worldwide air temperatures since the 1940's.
理论思考和实证证据表明，大气浑浊度作为气溶胶负荷的一个函数，是地球 - 大气系统热平衡中的一个重要因素。过去几十年间浑浊度的增加可能是自20世纪40年代以来全球气温下降的主要原因。
