The Guardian (Charlottetown)

A refresher on winter precipitat­ion types

- ALLISTER AALDERS weather@saltwire.com @allisterca­nada Allister Aalders is the weather specialist for the Saltwire Network, providing forecasts and analysis for Atlantic Canada. #Askalliste­r

Whether you like it or not, winter is gradually making its presence known.

With winter weather sometimes comes confusion about the type of precipitat­ion falling from the sky.

The two most common misunderst­andings during winter weather are that it’s hailing and that it’s freezing rain when it isn’t.

Let’s start with hail – I received reports of hail falling in parts of Nova Scotia Wednesday afternoon.

The key to remember is that hail is formed within thundersto­rms. So, unless we’re experienci­ng thundersno­w that’s producing hail – which is quite rare — it’s not hail you’re seeing. It’s likely ice pellets or graupel.

Ice pellets form when snowflakes in the upper levels of the atmosphere start melting in a warmer layer or air below but refreeze once they enter a cooler layer and land at the surface.

Graupel, sometimes referred to as snow pellets and at times soft hail, forms when supercoole­d water droplets freeze onto snow crystals through a process called riming, then fall to the ground as tiny white snow pellets.

This leads me to my next point. People often think these frozen pellets are freezing rain, but it’s far from it.

Freezing rain occurs when snowflakes melt completely in a warmer layer of air. The droplet then enters colder air directly at the surface, supercooli­ng it and allowing it to freeze on direct contact with surfaces.

The key to remember is that freezing rain is not frozen until it reaches the surface. Thus, it does not fall as a frozen water droplet and builds an ice accretion on surfaces.

These are just a few things to remember when reporting precipitat­ion this winter season.

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 ?? ?? Air temperatur­es at the surface and aloft have a major impact on the precipitat­ion type during the winter months.
Air temperatur­es at the surface and aloft have a major impact on the precipitat­ion type during the winter months.

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