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- As noted, a variety of dates and even exact times are used in different countries or regions to mark changes of the calendar seasons.
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- Six ecological seasons can be distinguished without fixed calendar-based dates like the meteorological and astronomical seasons.
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- 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, for monthly data, if there is a seasonality effect, we would expect to see significant peaks at lag 12, 24, 36, and so on (although the intensity may decrease the further out we go). However, if the period is not known, the autocorrelation plot can help. Apart from these considerations, the organisations need to know if variation they have experienced has been more or less than the expected amount, beyond what the usual seasonal variations account for.
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Thus Russia, historically navally constrained when confined to using Arkhangelsk (before the 18th century) and even Kronstadt, has particular interests in maintaining and in preserving access to Baltiysk, Vladivostok, and Sevastopol. For navies, the presence of accessible ports and bases can allow naval operations during certain (variable) seasons of the year. Floral and animal activity variation near the equator depends more on wet/dry cycles than seasonal temperature variations, with different species flowering (or emerging from cocoons) at specific times before, during, or after the monsoon season. Each season’s arrival is heralded not by a calendar date, but by royaldogs casino environmental factors such as changing winds, flowering plants, temperature and migration patterns and lasts approximately two standard calendar months. The Noongar people of South-West Western Australia recognise maar-keyen bonar, or six seasons.
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- A less completely regular cyclic variation might be dealt with by using a special form of an ARIMA model which can be structured so as to treat cyclic variations semi-explicitly.
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In Europe, this is related to the English concept of Midsummer, High Summer or the Dog days, and related also to Spanish distinctions between primavera, estío and verano. 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. On the other hand, people living far to the west (America), whose clocks run behind UTC, may experience an equinox as early as March 19. People living farther to the east (Asia and Australia), whose local times are in advance, see the astronomical seasons apparently start later; for example, in Tonga (UTC+13), an equinox occurred on September 24, 1999, a date on which the equinox will not fall again until 2103. All the times are given in UTC (roughly speaking, the time at Greenwich, ignoring British Summer Time).
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Every periodic function can be approximated with the inclusion of Fourier terms. However, the seasonality of such a regression would be represented as the sum of sine or cosine terms, instead of a single sine or cosine term in a sinusoidal model. Similar to using the sinusoidal model, Fourier terms added into regression models utilize sine and cosine terms in order to simulate seasonality. A less completely regular cyclic variation might be dealt with by using a special form of an ARIMA model which can be structured so as to treat cyclic variations semi-explicitly. The index is based on a mean of 100, with the degree of seasonality measured by variations away from the base. An index value is attached to each period of the time series within a year.
Calendar-based reckoning defines the seasons in relative rather than absolute terms, so the coldest quarter-year is considered winter even if floral activity is regularly observed during it, despite the traditional association of flowers with spring and summer. The tropical and (to a lesser degree) subtropical regions see little annual fluctuation of sunlight and temperature due to Earth’s moderate 23.4-degree tilt being insufficient to appreciably affect the strength of the Sun’s rays annually. In the temperate and polar regions, seasons are marked by changes in the amount of sunlight, which in turn often causes cycles of dormancy in plants and hibernation in animals. Seasonal weather fluctuations (changes) also depend on factors such as proximity to oceans or other large bodies of water, currents in those oceans, El Niño/ENSO and other oceanic cycles, and prevailing winds. In general, the effect of orbital eccentricity on Earth’s seasons is a 7% variation in sunlight received. Between this effect and the shorter daylight hours, the axial tilt of the Earth accounts for most of the seasonal variation in climate in both hemispheres.