Answer:
sulfur dioxide and drops of sulfuric acid
Explanation:
Answer: D
Explanation:
They bought war bonds (sold by the
United States government) to fund the war effort. When the war was over, they had savings
which they used to buy automobiles and other goods that were not available during the war.
When the war ended, South Carolina and the United States were poised to enter a period of
prosperity (good economic times).
High salinity (lots of salt) and cooler temperatures :) the molecules in cold water are more densely packed
One of the most striking ongoing changes in the Arctic is the rapid melting of sea ice. Some climate models predict that, sometime during the first half of the 21st century, summer sea ice will vanish from the Arctic Ocean. An absence of summer ice would amplify the existing warming trend in Arctic tundra regions as well as in regions beyond the tundra, because sea ice reflects sunlight much more readily than the open ocean and, thus, has a cooling effect on the atmosphere. In addition, research indicates that the retreat of sea ice would enhance the productivity of tundra vegetation, and the resulting buildup of plant biomass might lead to more extreme events such as large tundra fires. Finally, an ice-free Arctic Ocean would improve access to high northern latitudes for recreational and industrial activities; this would likely place additional stress on tundra plants and animals as well as compromise the resilience of the tundra ecosystem itself. In alpine tundras too, climate warming could encourage more human activity and increase damage to plant and animal populations there.
The fate of permafrost in a warmer world is a particularly important issue. Together, tundra and taiga account for approximately one-third of global carbon storage in soil, and a large portion of this carbon is tied up in permafrost in the form of dead organic matter. Some of this organic matter has been preserved for many thousands of years, not because it is inherently difficult to break down but because the land has remained frozen. Thawing of the permafrost would expose the organic material to microbial decomposition, which would release carbon into the atmosphere in the form of CO2 and methane (CH4). Rates of microbial decomposition are much lower under anaerobic conditions, which release CH4, than under aerobic conditions, which produce CO2; however, CH4 has roughly 25 times the greenhouse warming potential of CO2. The Arctic has been a net sink (or repository) of atmospheric CO2 since the end of the last ice age. At the same time, however, the region has been a net source of atmospheric CH4, primarily because of the abundance of wetlands in the region.
There once was a little girl named Annabeth. She was walking home from school when she heard a voice, so she stopped walking and looked around in fright. She then heard it again and she said in a quiet but audible voice “Who’s there?” She heard the voice again and said “Help me, help me” repetitively, Annabeth walked a little closer and then looked to both sides and walked into the forest and looked around her and didn’t find anyone around her. So she walked further into the forest. She came to a stop when she saw an open door in a tree. She looked around to make sure no one was watching. She walked into the door and she gasped when she saw what was on the other side of the door. She saw a Unicorn galloping in the distance. She was amazed to see something so pretty. She walked forward and the Unicorn saw her and stopped, she stopped in her tracks and Unicorn slowly walked over to her, she reached her hand out and the horse let her pet him.
That is 183 words