Every year, in January, after the Winter Solstice (December 21-22), there is often a period of calm, warm weather that mimics the “Indian Summer” of Fall.
This year, where I live, it ran for a total of about 10 days. Maximum daytime temperature rose from roughly +40F to a high of +59F. Nighttime lows showed lesser change. Snow and ice disappeared, melt-water ran in gutters everywhere. A few sluggish flies came out to circle in the sunlight at the height of the day’s warmth.
The Internet tells me this unseasonably mild weather is called the “January Thaw” or the “Winter Thaw,” and that it’s a common meteorological phenomenon akin to “Indian Summer.”
Various online sites describe it in meteorological jargon, but claim that among scientists it is unclear whether this is related to the Winter Solstice. The Winter Solstice is the moment when the Earth reaches the farthest point of the South Pole’s tilt towards the sun, marking Summer in the Southern Hemisphere, and (conversely) the first day of Winter in the Northern Hemisphere.
I assume that the Earth reaches a point of perfect stasis in this tilt, then recovers to begin a slow acceleration towards the perfect middling of the next Equinox, with the Sun directly overhead at the Equator (marking the first day of Spring in the Northern Hemisphere).
–My question is whether this December 21-22 stasis in the Earth’s tilt is the originating cause of the brief but dramatic change sometimes seen in January weather? Why would a weather window like that occur at all, why the delay, and why does ordinary winter weather soon return with a vengeance?
When scientists say they don’t know, sometimes they mean, “We don’t know, really,” and sometimes they mean, “We think we know by theory, but won’t say so because we don’t have data to prove it.”
Anyone in the weather or science business want to clarify which it is here?