- Mon Sep 11, 2017 5:43 pm
#39589
"sheds light"
If we assume that (C) is talking about ocean water and snow-covered land, I agree that it would have to be true that snow-covered land would be heated less than non-snow-covered land given the same sun. And I agree that that's compatible with (C): water and snow-covered land could still heat the atmosphere, just by not as much as water and non-snow-covered land would.
But I still don't see how (C) would *strengthen* that reasoning. I read the argument (and your explanation) as being about what warms the atmosphere *more or less* than normal conditions. We know that everything warms the atmosphere: sun being reflected on land, ocean, ice, and snow; AND sun being absorbed by land, ocean, ice, and snow. The mere fact that the sun reaches earth warms the atmosphere; if there were no sun, it would not be warmed; even if Earth were all ice, the atmosphere would still be warmed more than if there were no sun at all. The argument is saying that the more reflection there is, the less warming there will be. Showing that "the less reflection (=more absorption) there is, the more warming there will be" would strengthen the argument, because it would show that relationship goes dynamically in both directions.
But (C) doesn't say that "the less reflection (=more absorption) there is, the more warming there will be." It simply repeated the premise: everything warms the atmosphere. No information about more or less. Thus no strengthening effect, imo.
Anyway, I agree that (C) is the best of bad answers if you give it as much help as I do many of my wrong answers!
If we assume that (C) is talking about ocean water and snow-covered land, I agree that it would have to be true that snow-covered land would be heated less than non-snow-covered land given the same sun. And I agree that that's compatible with (C): water and snow-covered land could still heat the atmosphere, just by not as much as water and non-snow-covered land would.
But I still don't see how (C) would *strengthen* that reasoning. I read the argument (and your explanation) as being about what warms the atmosphere *more or less* than normal conditions. We know that everything warms the atmosphere: sun being reflected on land, ocean, ice, and snow; AND sun being absorbed by land, ocean, ice, and snow. The mere fact that the sun reaches earth warms the atmosphere; if there were no sun, it would not be warmed; even if Earth were all ice, the atmosphere would still be warmed more than if there were no sun at all. The argument is saying that the more reflection there is, the less warming there will be. Showing that "the less reflection (=more absorption) there is, the more warming there will be" would strengthen the argument, because it would show that relationship goes dynamically in both directions.
But (C) doesn't say that "the less reflection (=more absorption) there is, the more warming there will be." It simply repeated the premise: everything warms the atmosphere. No information about more or less. Thus no strengthening effect, imo.
Anyway, I agree that (C) is the best of bad answers if you give it as much help as I do many of my wrong answers!