The laws of thermodynamics dictate that a warmer atmosphere can hold more water vapor, but new research has found that atmospheric moisture has not increased as expected over arid and semi-arid regions of the world as the climate has warmed.
The findings are particularly puzzling because climate models have been predicting that the atmosphere will become more moist, even over dry regions. If the atmosphere is drier than anticipated, arid and semi-arid regions may be even more vulnerable to future wildfires and extreme heat than projected.
The authors of the new study, led by the U.S. National Science Foundation National Center for Atmospheric Research (NSF NCAR), are uncertain what’s causing the discrepancy.
“The impacts could be potentially severe,” said NSF NCAR scientist Isla Simpson, lead author of the study. “This is a global problem, and it’s something that is completely unexpected given our climate model results.”
When I was studying climatology, I wondered if an increased evening out of global temperatures (with higher latitudes warming disproportionately more than lower) would lead to a kind of lethargy in weather systems, since it is ultimately temperature differentials that are the driving force to their movement. So systems that bring rain to the coast might be less likely to wander inland, for example. That would then intensify the continental effect and make interiors more prone to drought.
