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Posted

Dry north-northwesterly upper level flow, either nonexistent or weak offshore surface winds, and clear skies under a deep trough.

In the winter, record lows are usually set in the days after an arctic frontal passage, immediately after a snowpack has been established during the transition, and while the new arctic airmass remains trapped in the low levels relatively unmoderated underneath a building ridge, forming an arctic inversion.

During the Summer, the logic is pretty similar, though deep nighttime inversions are basically nonexistent on any appreciable scale. What this means is that we really need that mid-upper level cold air to support whatever barely noticeable inversion forms during the few hours of nighttime we get. So there's going to be less of a timing offset between the arrival of that "chilly" airmass diving out of the north-northwest, and the record low which ensues, since any building ridging will reduce the surface's ability to cool and will simply mix to the ground during the daytime.

  • Snow 1

Weather stats for MBY

Snowfall:

-Total snowfall since joining: 56"

-2018-19: 21"

-2019-20: 2.5"

-2020-21: 13"

-2021-22: 8.75"

-2022-23: 5.75"

-2023-24: 0.25"

-2024-25*: 4.75"

-Most recent snowfall: 0.25”; February 14th, 2025

-Largest snowfall (single storm): 8.5"; February 12-13, 2021

-Largest snow depth: 14"; 1:30am February 12th, 2019

Temperatures:

-Warmest: 109F; June 28th, 2021

-Coldest: 13F; December 27th, 2021

-Phreeze Count 2023-24: 40

  • 1 month later...
Posted
On 5/5/2025 at 2:01 AM, Meatyorologist said:

Dry north-northwesterly upper level flow, either nonexistent or weak offshore surface winds, and clear skies under a deep trough.

In the winter, record lows are usually set in the days after an arctic frontal passage, immediately after a snowpack has been established during the transition, and while the new arctic airmass remains trapped in the low levels relatively unmoderated underneath a building ridge, forming an arctic inversion.

During the Summer, the logic is pretty similar, though deep nighttime inversions are basically nonexistent on any appreciable scale. What this means is that we really need that mid-upper level cold air to support whatever barely noticeable inversion forms during the few hours of nighttime we get. So there's going to be less of a timing offset between the arrival of that "chilly" airmass diving out of the north-northwest, and the record low which ensues, since any building ridging will reduce the surface's ability to cool and will simply mix to the ground during the daytime.

Does that mean the 'hitbox' for the possibility gets narrower in the summer for when this cold trough does happen giving us a rough run of the  game map? Would this be a win by the skin-of-your- teeth-when-all-hope-seems-lost scenario?

Posted
On 7/1/2025 at 8:59 PM, MrWeatherTalk said:

Does that mean the 'hitbox' for the possibility gets narrower in the summer for when this cold trough does happen giving us a rough run of the  game map? Would this be a win by the skin-of-your- teeth-when-all-hope-seems-lost scenario?

I guess so, yeah. But if you advect enough cool dry air into the region and clear things out after dusk, you still stand a fighting chance at recording a record low without upper level assistance. That's what Eugene did in early July 2018* to match the monthly record low temperature. Highs still reached the 70s with that one.

Weather stats for MBY

Snowfall:

-Total snowfall since joining: 56"

-2018-19: 21"

-2019-20: 2.5"

-2020-21: 13"

-2021-22: 8.75"

-2022-23: 5.75"

-2023-24: 0.25"

-2024-25*: 4.75"

-Most recent snowfall: 0.25”; February 14th, 2025

-Largest snowfall (single storm): 8.5"; February 12-13, 2021

-Largest snow depth: 14"; 1:30am February 12th, 2019

Temperatures:

-Warmest: 109F; June 28th, 2021

-Coldest: 13F; December 27th, 2021

-Phreeze Count 2023-24: 40

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