Support The more sunlight our planet reflects back into space, the cooler the global atmosphere tends to become. ββββ βββ βββ βββββββ ββββ ββββ ββββββββ ββββ ββββ βββββ ββββ ββ βββββ βββββ ββ ββββ βββββββ ββββ ββββββ ββββββββββ βββ βββββββ βββ ββββ ββ βββββββ βββββββ ββββ ββ βββββββ ββββ ββββ βββ ββββ βββ βββββββ ββ ββββββββ βββ ββββββ ββββββββββ ββ ββββββ ββ βββββββ
The author concludes that if more of Earthβs surface area is covered with snow and ice, the global atmosphere will probably become cooler. This is supported by the observations that snow and ice reflect more sunlight into space than ocean or land, and the atmosphere becomes cooler when more sunlight is reflected into space.
The author assumes that increased snow and ice coverage on Earth will not have other effects that counteract the cooling caused by greater sunlight reflection.
Analysis by AlexandraNash
Which one of the following, ββ βββββ βββββ ββββ ββββββββββ βββ βββββββββ
Low atmospheric temperatures βββ ββββββββ βββ βββ βββββββββ ββ ββββββ ββββ ββββββ ββ βββββ
Other factors besides βββ ββββββββββββ ββ βββ βββ ββββ ββββββ βββ βββββββ ββ βββββββ βββββββββββ
Ocean water and ββββ ββββββ ββ ββββββββ ββ ββββ ββββ βββββββ βββββββββββ
The atmosphere derives ββββ ββ βββ ββββ ββββ βββ βββββββ ββ ββββββββ βββββββ βββ
Lighter-colored soil reflects ββββ ββββββββ ββββ ββββ βββββ ββββ ββββ ββββββββββββββ βββββ