
Our dewpoints tend to be low during the summer; it has been close to 50 for some time, with a brief rise to near sixty yesterday afternoon. In contrast, the weather station linked to my home town of Athens, Ohio (the airport at Parkersburg, West Virginia) has been reporting dewpoints of 70-74 during the course of the day today, or 20 degrees higher. High dewpoints not only mean higher relative humidity- the way most weather reports relay humidity information- but they also restrict cooling in two important ways. First, when water condenses, either as fog or dew, it releases the heat that went into evaporating it in the first place. So everything else being equal, if water is condensing, the temperature will tend to stay steady; latent heat of condensation will balance out heat being lost through radiation. A related phenomenon is that if the water is condensing as fog, the presence of fog will interfere with heat loss by radiation. Once a fog forms, the temperature will typically stay pretty steady until it burns off or is dispersed by wind. The second issue is that water vapor (vapor, not fog) is the most important greenhouse gas in the atmosphere; it very strongly absorbs and re-emits infrared radiation. So if the dewpoints are high where you live, it won't cool down at night nearly as much as if the dewpoints are low.
So even though the daytime highs are a little warmer than I'd like, I can count on it getting down to around 50 at night. And if I can cool down at night, I'm pretty much good. Our high yesterday was 91; our low was 51, a 40-degree diurnal range- and I've seen ranges over 50 degrees- over a hundred during the day, and in the forties at night. The high at Parkersburg yesterday was 87, and the low was 71 (with fog).
I do not miss Midwest humidity... I miss thunderstorms, but I don't miss the climate it takes to generate them.
1 comment:
Monsoons begun around here. Thankfully.
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