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The following diagram shows the relation between the line of solstice and the line of apsides of Earth's elliptical orbit.
The orbital ellipse with eccentricity exaggerated for effect goes through each of the six Earth images, which are sequentially the perihelion periapsis—nearest point to the sun on anywhere from 2 January to 5 January, the point of March equinox on 19, 20 or 21 March, the point of June solstice on 20 or 21 June, the aphelion apoapsis—farthest point from the sun on anywhere from 4 July to 7 July, the September equinox on 22 or 23 September, and the December solstice on 21 or 22 December.
These "astronomical" seasons are not of equal length, because of the elliptical nature of the orbit of the Earth, as discovered by Johannes Kepler.
From the March equinox it currently takes The times of the equinoxes and solstices are not fixed with respect to the modern Gregorian calendar, but fall about six hours later every year, amounting to one full day in four years.
They are reset by the occurrence of a leap year. The Gregorian calendar is designed to keep the March equinox no later than 21 March as accurately as is practical.
Gregorian calendar seasonal error. The calendar equinox used in the calculation of Easter is 21 March, the same date as in the Easter tables current at the time of the Council of Nicaea in AD The calendar is therefore framed to prevent the astronomical equinox wandering onto 22 March.
From Nicaea to the date of the reform, the years , , , , , , , and , which would not have been leap years in the Gregorian calendar, amount to nine days, but astronomers directed that ten days be removed.
Currently, the most common equinox and solstice dates are March 20, June 21, September 22 or 23 and December 21; the four-year average slowly shifts to earlier times as the century progresses.
This shift is a full day in about years compensated mainly by the century "leap year" rules of the Gregorian calendar and as was a leap year the current shift has been progressing since the beginning of the last century, when equinoxes and solstices were relatively late.
This also means that in many years of the twentieth century, the dates of March 21, June 22, September 23 and December 22 were much more common, so older books teach and older people may still remember these dates.
On the other hand, people living far to the west America whose clocks run behind UTC may experience an equinox as early as March Over thousands of years, the Earth's axial tilt and orbital eccentricity vary see Milankovitch cycles.
The equinoxes and solstices move westward relative to the stars while the perihelion and aphelion move eastward. Thus, ten thousand years from now Earth's northern winter will occur at aphelion and northern summer at perihelion.
The severity of seasonal change — the average temperature difference between summer and winter in location — will also change over time because the Earth's axial tilt fluctuates between Smaller irregularities in the times are caused by perturbations of the Moon and the other planets.
Solar timing is based on insolation in which the solstices and equinoxes are seen as the midpoints of the seasons.
It was the method for reckoning seasons in medieval Europe, especially by the Celts , and is still ceremonially observed in Ireland and some east Asian countries.
Summer is defined as the quarter of the year with the greatest insolation and winter as the quarter with the least.
The solar seasons change at the cross-quarter days, which are about 3—4 weeks earlier than the meteorological seasons and 6—7 weeks earlier than seasons starting at equinoxes and solstices.
Thus, the day of greatest insolation is designated "midsummer" as noted in William Shakespeare 's play A Midsummer Night's Dream , which is set on the summer solstice.
On the Celtic calendar , the start of the seasons corresponds to four Pagan agricultural festivals - the traditional first day of winter is 1 November Samhain , the Celtic origin of Halloween ; spring starts 1 February Imbolc , the Celtic origin of Groundhog Day ; summer begins 1 May Beltane , the Celtic origin of May Day ; the first day of autumn is 1 August Celtic Lughnasadh.
The traditional calendar in China forms the basis of other such systems in East Asia. Its seasons are traditionally based on 24 periods known as solar terms.
These dates were not part of the traditional lunar calendar, however, and moveable holidays such as Chinese New Year and the Mid-Autumn Festival are more closely associated with the seasons.
Some calendars in south Asia use a six-season method where the number of seasons between summer and winter can number from one to three. The dates are fixed at even intervals of months.
In the Hindu calendar of tropical and subtropical India, there are six seasons or Ritu that are calendar-based in the sense of having fixed dates: Vasanta spring , Greeshma summer , Varsha monsoon , Sharad autumn , Hemanta early winter , and Shishira prevernal or late winter.
The six seasons are ascribed to two months each of the twelve months in the Hindu calendar. The rough correspondences are:.
The Bengali Calendar is similar but differs in start and end times. It has the following seasons or ritu:. The Tamil calendar follows a similar pattern of six seasons.
The Noongar people of South-West Western Australia also recognise maar-keyen bonar  , or six seasons. Each season's arrival is heralded not by a calendar date, but by environmental factors  such as changing winds, flowering plants, temperature and migration patterns and lasts approximately two standard calendar months.
The seasons also correlate to aspects of the human condition, intrinsically linking the lives of the people to the world that surrounds them and also dictating their movements, as with each season, various parts of country would be visited which were particularly abundant or safe from the elements.
The timing and feel of the seasons has been noted as having changed due to the current trends in climate change. Any point north of the Arctic Circle or south of the Antarctic Circle will have one period in the summer when the sun does not set, and one period in the winter when the sun does not rise.
At progressively higher latitudes, the maximum periods of " midnight sun " and " polar night " are progressively longer. By October 13 the sun is above the horizon for only 1 hour 30 minutes and on October 14 it does not rise above the horizon at all and remains below the horizon until it rises again on 27 February.
First light comes in late January because the sky has twilight , being a glow on the horizon, for increasing hours each day, for more than a month before the sun first appears with its disc above the horizon.
From mid-November to mid-January, there is no twilight. In the weeks surrounding 21 June, in the northern polar region, the sun is at its highest elevation, appearing to circle the sky there without going below the horizon.
Eventually, it does go below the horizon, for progressively longer periods each day until around the middle of October, when it disappears for the last time until the following February.
For a few more weeks, "day" is marked by decreasing periods of twilight. Eventually, from mid-November to mid-January, there is no twilight and it is continuously dark.
In mid January the first faint wash of twilight briefly touches the horizon for just minutes per day , and then twilight increases in duration with increasing brightness each day until sunrise at end of February, then on 6 April the sun remains above the horizon until mid October.
Ecologically speaking, a season is a period of the year in which only certain types of floral and animal events happen e.
In this sense, ecological seasons are defined in absolute terms, unlike calendar-based methods in which the seasons are relative. If specific conditions associated with a particular ecological season don't normally occur in a particular region, then that area cannot be said to experience that season on a regular basis.
Six seasons can be distinguished which do not have fixed calendar-based dates like the meteorological and astronomical seasons. Conversely, prevernal and vernal seasons begin up to a month earlier near oceanic and coastal areas.
For example, prevernal crocus blooms typically appear as early as February in coastal areas of British Columbia , the British Isles , but generally don't appear until March or April in locations like the Midwest USA or parts of eastern Europe.
The actual dates for each season vary by climate region and can shift from one year to the next. Average dates listed here are for mild and cool temperate climate zones in the Northern Hemisphere:.
In the tropics, where seasonal dates also vary, it is more common to speak of the rainy or wet, or monsoon season versus the dry season.
For example, in Nicaragua the dry season November to April is called 'summer' and the rainy season May to October is called 'winter', even though it is located in the northern hemisphere.
In some tropical areas a three-way division into hot, rainy, and cool season is used. There is no noticeable change in the amount of sunlight at different times of the year.
However, many regions such as the northern Indian ocean are subject to monsoon rain and wind cycles.
Thus, the tropics are characterized by numerous "mini-seasons" within the larger seasonal blocks of time. In the tropical parts of Australia in the northern parts of Queensland , Western Australia and the Northern Territory , wet and dry seasons are observed in addition to or in place of temperate season names.
Indigenous people in polar, temperate and tropical climates of northern Eurasia, the Americas, Africa, Oceania, and Australia have traditionally defined the seasons ecologically by observing the activity of the plants, animals and weather around them.
Each separate tribal group traditionally observes different seasons determined according to local criteria that can vary from the hibernation of polar bears on the arctic tundras to the growing seasons of plants in the tropical rainforests.
In Australia, some tribes have up to eight seasons in a year,  as do the Sami people in Scandinavia.
Many indigenous people who no longer live directly off the land in traditional often nomadic styles, now observe modern methods of seasonal reckoning according to what is customary in their particular country or region.
As noted, a variety of dates are used in different countries to mark the changes of seasons, especially those that are calendar based.
These observances are often declared "official" within their respective jurisdictions by the local or national media, even when the weather or climate is contradictory.
From Wikipedia, the free encyclopedia. For other uses, see Season disambiguation. Effect of sun angle on climate. Regardless of the time of day i.
In addition to the density of incident light, the dissipation of light in the atmosphere is greater when it falls at a shallow angle. Diagram of the Earth's seasons as seen from the north.
Diagram of the Earth's seasons as seen from the south. Retrieved 27 April Retrieved 2 May Retrieved 14 May Equinoxes, Solstices, Perihelion, and Aphelion".
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