Answer:
- high CAPE values
- strong vertical wind shear
- strong upper-level divergence
Explanation:
A supercell thunderstorm is a type of storm that is characterized by a deep and rotating updraft. Supercells can be quite severe, but tend to last between 2 and 4 hours. These storms are particularly associated with the Great Plains area of the United States and the area known as Tornado Corridor in South America (Argentina, Uruguay and southern Brazil).
HERE IS YOUR ANSWER
Explanation:
<em>ACTUALLY</em><em> </em><em> </em><em>NO</em><em> </em><em>MISUNDERSTANDINGS</em><em> </em><em>AND</em><em> </em><em>QUESTIONS</em><em> </em><em>IS</em><em> </em><em>THE</em><em> </em><em>ANSWER</em><em>.</em><em> </em><em>PLEASE</em><em> </em><em>MARK</em><em> </em><em>MY</em><em> </em><em>ANSWER</em><em> </em><em>AS</em><em> </em><em>BRAINLIEST</em><em> </em><em>IF</em><em> </em><em>THE ANSWERS ARE</em><em> </em><em>CORRECT</em><em>. </em>
Answer:
from what I've read up on at least 40,000 I'm really sorry if I'm wrong I'm
Explanation:
tbh I'm look at the same type of problems
Answer: The release of methane from thawed permafrost
Explanation:
With increasing global warming, permafrost in the arctic is melting. The carbon and methyl clathrates present in permafrost escape into the atmosphere to form carbon dioxide and methane, both greenhouse gases.
In the Arctic, molecules of methane are trapped in ice crystals as methyl clathrates. When the temperature increases, these crystals release methyl clathrates which become methane when in contact with the atmosphere.
The cause of the increasing atmospheric
is due to the the thawing of dead organisms present in the permafrost. As the permafrost melts, these organisms decay and release
into the atmosphere.