The main concept to understand is this: a warmer atmosphere can hold more water vapor. And water vapor is one of the building blocks for showers and storms. The more water vapor in a storm, the heavier the resulting rainfall can be.
In fact, Climate Central found that a one-degree rise in air temperature correlates to a 4% increase in water vapor content in a cloud. This means cities and towns within the path of these storms could receive more rainfall than the land is accustomed to or could hold.
RELATED: Flash Flood Alley: Why central Texas has a history of devastating floods
Flash Flood Alley: Why central Texas has a history of devastating floods
Furthermore, a study from Climate Central found that San Antonio has seen a 6% increase in rainfall intensity produced by showers and storms that develop over the region.
While that might not seem like much, for a region like theirs that is prone to flash flooding, possibly extreme, deadly flash floods, that small increase is the difference between a heavy rain event and a dangerous flash flood.
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