A common misperception. I keep seeing this repeated over and over and rarely see a factual explanation or rebuttal. While it's true that warmer air holds more moisture in the form of water vapor, this is
the very reason that warmer air produces
less snowfall.
Bear with me, because this gets a bit technical. Or just dismiss it off hand, whichever you prefer. :tongue:
The "temperature" is the measure of thermal energy in the air. The "dewpoint temperature" is the temperature at which the water vapor which is contained in the air will condense into a liquid, and thereby form cloud droplets or ice crystals (if cold enough). This dewpoint temperature is largely a function of the density of the water vapor in the air (referred to as "saturation vapor pressure") - high water vapor density (more water vapor/volume) = higher dewpoint temperature. Low water vapor density (less water vapor/volume) = lower dewpoint temperature. This state, where the temperature just lowers to the dewpoint temperature is referred to as "saturation", and produces clouds made of either suspended tiny water droplets or suspended ice crystals, but not yet any precipitation.
As the water vapor changes state from a gas to either a liquid or solid, two primary things occur. Firstly, the density of the water vapor is reduced, thereby slightly lowering the dewpoint temperature. Secondly, the change of state from gas to liquid and liquid to solid releases latent heat to the air, thereby slightly raising the temperature. Consequently, the temperature can NEVER be less than the dewpoint temperature. As the temperature continues to drop, so must the dewpoint temperature. So the total water content of a parcel of air is ALWAYS capped by the temperature of that parcel. And as more and more water vapor changes state to either liquid or solid, the droplets and/or ice crystals present become more and more numerous (the cloud becomes more dense).
Precipitation is what occurs when the temperature
continues to lower past the dewpoint (referred to as "super-saturation"), adding increased condensed water droplets or ice crystals, which coalesce to form large enough and heavy enough particles to fall. In other words, Precipitation is the consequence of moisture being "squeezed" out of the atmosphere by a lowering temperature.
In an atmosphere with a temperature of 100F, the dewpoint temperature (again, proportional to water vapor content) can be up to and including 100F. If in this hypothetical scenario the dewpoint is 60F, you won't have any clouds until the temperature lowers to 60F, and no precipitation until the temperature lowers further. In a different scenario where both the atmospheric temperature and the dewpoint temperature are 20F, even though there's
much less total moisture available than in the 100F scenario, clouds and perhaps precipitation will occur because the temperature has lowered to and perhaps beyond the natural dewpoint.
So in summary, though you're correct in saying that warm air = more moisture
capacity (but not necessarily more moisture), warm air does
not necessarily = more snow. Super-saturation = more snow. And super-saturation is more likely the colder the air becomes.
Of course, none of that discussion has any bearing whatsoever on whether or not more snowy conditions are indicative of either a warming climate or a cooling climate. The amount of snow seen in a specific region during a specific season is dependent on much,
much more than simply temperature and dewpoint. Seasonal weather patterns, transient climate regimes, multi-year cycles like el-nino and la-nina, the state of the pacific decadal and atlantic multi-decadal oscillations, and many other factors can overwhelm any trend dictated by the principle illustrated above. The fact that there was more snowfall in the northeast US this past year bears no indication whatsoever of the impact or lack thereof of anthropogenic global warming.