In the wee morning hours of Jan. 27, 2018, some kind of significant wind event managed to blow down 110 trees across a large swath of forest on the north shore of Lake Quinault, on Washington’s Olympic Peninsula.
Such wind was not recorded at nearby weather stations, nor did radar records from the time show anything more than some high and low-pressure systems meeting, according to Mass.
The explanation espoused by The Daily World was that the wind came from a “microburst,” a rare wind event that creates a downward wind in a localized area.
But a National Weather Service meteorologist told Mass it would’ve taken winds of 70 to 80 mph to snap trees off in the way it happened that night, so Mass dismissed that possibility.
National Park Service reports to Mass indicated that the wind event likely came from the north — a northerly wind — and records showed a seismic record of the event. In other words, it was such a force of trees falling that it looked like a small earthquake.
But surface wind records from around the time of the incident didn’t show any major winds, and those that were recorded were blowing in the wrong direction.
No convective system that would created a “microburst,” either, according to Mass.
The only thing that could, possibly, have created the wind to down the trees was this: “a frontal zone was approaching, with warm air and southerly flow surging in aloft, while cooler easterly flow dominated near the surface.”