UPDATED — We just had the longest night of the year – now we have the shortest day. This year the Winter Solstice (aka the shortest day of the year) is this morning at precisely 10:34am in New Zealand.
Oh and yes – tonight is basically just as long as last night was.
This time and date signals the “Astronomical” start to winter. June 1st marks the “Meteorological” start to winter.
So why have both?
This is because the astronomical seasons are based on the position of the Earth in relation to the sun – like tomorrow when we have our shortest day with least amount of available sunlight – and the northern hemisphere has their longest day with the most available amount of sunlight.
The meteorological seasons are based on the annual temperature cycle and to make statistics/data easier to keep.
As a side note here in New Zealand the start and end of seasons is definitely subjective – if you go by the astronomical date you have to say it’s the middle of winter while we have lambs born, flowers and buds coming out and t-shirt weather returning in September. However the meteorological date can also give you a false sense of the seasons – for example most years the first half of December is more like spring than summer.
WeatherWatch.co.nz has long said New Zealand has a two month summer (Jan, Feb) and a two month winter (July, August). The rest of the year New Zealand is transitioning through Autumn and Spring-like weather patterns thanks to our position on planet earth.
Graphic courtesy of NASA / US Govt
NOAA explains Meteorological vs Astronomical
People have used observable periodic natural phenomena to mark time for thousands of years. The natural rotation of the Earth around the sun forms the basis for the astronomical calendar, in which seasons are defined by two solstices and two equinoxes. Both the solstices and equinoxes are determined based on the Earthâ€™s tilt and the sunâ€™s alignment over the equator. The solstices mark the times when the sunâ€™s annual path is farthest, north or south, from the Earthâ€™s equator. The equinoxes mark the times when the sun passes directly above the equator. In the Northern Hemisphere, the summer solstice falls on or around June 21, the winter solstice on or around December 22, the vernal (spring) equinox on or around March 21, and the autumnal equinox on or around September 22. These seasons are reversed but begin on the same dates in the Southern Hemisphere.
Because the Earth actually travels around the sun in 365.24 days, an extra day is needed every fourth year, creating what we know as Leap Year. This also causes the exact date of the solstices and equinoxes to vary. Additionally, the elliptical shape of the Earthâ€™s orbit around the sun causes the lengths of the astronomical seasons to vary between 89 and 93 days. These variations in season length and season start would make it very difficult to consistently compare climatological statistics for a particular season from one year to the next. Thus, the meteorological seasons were born.
Meteorologists and climatologists break the seasons down into groupings of three months based on the annual temperature cycle as well as our calendar. We generally think of winter as the coldest time of the year and summer as the warmest time of the year, with spring and fall being the transition seasons, and that is what the meteorological seasons are based on. Meteorological spring includes March, April, and May; meteorological summer includes June, July, and August; meteorological fall includes September, October, and November; and meteorological winter includes December, January, and February.
These seasons were created for meteorological observing and forecasting purposes, and they are more closely tied to our monthly civil calendar than the astronomical seasons are. The length of the seasons is also more consistent for the meteorological seasons, ranging from 90 days for winter of a non-leap year to 92 days for spring and summer. By following the civil calendar and having less variation in season length and season start, it becomes much easier to calculate seasonal statistics from the monthly statistics, both of which are very useful for agriculture, commerce, and a variety of other purposes.
– WeatherWatch.co.nz & NOAA/US Govt