
People talk about being a summer person or a winter person as though it were fixed at birth. It is usually more about pace: whether you start things or finish them, whether you like long light or early dark, whether you want the diary full or empty.
Seven questions, no calendar involved. At the end you get the season that matches how you are running at the moment, which may well be different from the one you would have claimed. Underneath, four short pieces on where our season boundaries actually come from, including a calendar that counts seventy-two of them.
See all the outcomes this quiz can land on, and what each one means →
Ask when autumn starts and you will get two defensible answers. The astronomical seasons hang on solstices and equinoxes, which drift by a day or two because the orbital year is not a tidy 365 days. The June solstice lands anywhere from the 20th to the 22nd.
Meteorological seasons ignore all that and cut the year into three-month blocks beginning on 1 December, 1 March, 1 June and 1 September. Weather services prefer them because statistics compare more easily across equal, fixed periods. Neither version is more correct; they were built for different jobs.
Older calendars often put the solstice mid-season rather than at the start. In the traditional East Asian solar terms, lichun, the beginning of spring, falls around 4 February, and the winter solstice sits in the middle of winter, which is where the word midwinter comes from.
Irish tradition does something similar, with spring beginning at Imbolc on 1 February. If February has ever felt oddly like the start of something, that instinct has a long calendar behind it.
The Japanese calendar divides the year into twenty-four sekki, borrowed from China, and then splits each of those into three ko, giving seventy-two microseasons of roughly five days. The Chinese originals described a climate that did not match Japan, so the astronomer Shibukawa Shunkai rewrote them for local conditions in the 1680s.
The names are the point. East wind melts the ice. Bush warblers start singing in the mountains. Rotten grass becomes fireflies. Bears retreat to their dens. Reading a year at that resolution is a genuinely different experience from reading it in four chunks, and you can copy the habit anywhere by writing down what changed outside this week.
Day length is the one seasonal fact that is not up for debate. London gets roughly sixteen and a half hours of daylight at the June solstice and under eight in December. Reykjavik swings from about twenty-one hours to a little over four. At the equator the difference is minutes.
Whether that swing reliably moves how populations feel is genuinely contested among researchers. A large analysis of United States survey data published in 2016 by Traffanstedt and colleagues found no seasonal pattern in the scores they examined, a direct challenge to a well-established assumption. That argument is still running, and a quiz result has nothing to add to it.
What this one does is much smaller: it sorts a few preferences into a metaphor with weather in it, and metaphors are for thinking with.







