Ummmm, it's getting icy here Bowersville-Lavonia area
I would think that if temps remain below freezing, accrual would be more affected by the duration of the event rather than the intensity. There is probably an optimal intensity for maximum ice accrual for a specific temp below freezing....I.e. too little precip, you don’t reach max accrual, while too much precip is a waste.Consider this possible more simplistic reason heavier ZR may tend to accrete on branches at a lower rate: If for no other reason, a higher % of heavier rain likely drips off branches too quickly for it to have time to freeze on those branches. I'll exaggerate to make a point: What if somebody were to rapidly pour a bucket (representing extremely heavy ZR) of supercooled water on a branch? Wouldn't almost all of it go right to the ground below the branch? Compare that to pouring it very slowly over said branch. Wouldn't more of it accrete?
That is true in part to increase in surface area to accrue, (i.e. increase in diameter if ice crusted pine needles)I would think that if temps remain below freezing, accrual would be more affected by the duration of the event rather than the intensity. There is probably an optimal intensity for maximum ice accrual for a specific temp below freezing....I.e. too little precip, you don’t reach max accrual, while too much precip is a waste.
Very light intensity will result in a higher percentage of precipitation to accrue, while intensity that is too high will result in wasted precip.
My guess is that in the end, once the optimal intensity for a temp is reached, accrual rates from that point forward will be mostly affected by the duration of the event and not fall off as intensity increases....as long as the temp remains below freezing. I just guessing here, so I could be wrong.
That’s a good point. I was trying to simplify it so I left that out. But you’re exactly right. Ice accrual on an object leads to more surface area which leads to more accrual on the object and so on.That is true in part to increase in surface area to accrue, (i.e. increase in diameter if ice crusted pine needles)
I would think that if temps remain below freezing, accrual would be more affected by the duration of the event rather than the intensity. There is probably an optimal intensity for maximum ice accrual for a specific temp below freezing....I.e. too little precip, you don’t reach max accrual, while too much precip is a waste.
Very light intensity will result in a higher percentage of precipitation to accrue, while intensity that is too high will result in wasted precip.
My guess is that in the end, once the optimal intensity for a temp is reached, accrual rates from that point forward will be mostly affected by the duration of the event and not fall off as intensity increases....as long as the temp remains below freezing. I just guessing here, so I could be wrong.
As liquid mass turns into ice, it releases heat. Basically think of it as a solid changing to a liquid, the energy "trasnfer" has to give off some sort of warmth. Anything in motion will give off some form of heat.
As the liquid mass freezes on contact, the energy expunged creates a tiny little pocket of heat. As the rates become heavier, more heat is released and eventually the ground level comes above freezing.
Lighter ZR is letting less heat off as fast, because the droplets are smaller or the rate of precipitation as a whole, is lighter. From what I have seen, the bigger ice storms that have occurred in heavy precipitation scenarios were when the surface was too cold (26-28F) to be overcome by the liquid to solid change, and the end result being destructive ice accretion.
At least this process is what I was taught in my reading.
@Webberweather53 will hopefully, have a better response to this process.
Light rain 35/31 yuck. Hrrr has it near 60 here this afternoon. Good luck
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