Chlouvānem/Calendar and time: Difference between revisions

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The solar and sidereal year of Calémere (in Chlouvānem ''heirah'') is 418 Calemerian days long (about 609,6 days on Earth), and this period is divided, in the Chlouvānem calendar, in fourteen mostly arbitrary months (''asena'', pl. ''asenai'') which are grouped by season (''demibuñjñasusah'').
The solar and sidereal year of Calémere (in Chlouvānem ''heirah'') is 418 Calemerian days long (about 609,6 days on Earth), and this period is divided, in the Chlouvānem calendar, in fourteen mostly arbitrary months (''asena'', pl. ''asenai'') which are grouped by season (''demibuñjñasusah'').


The month names reflect climatic conditions of those particular months in the Lāmiejāya plain, the “heartlands” of the Chlouvānem civilization. Not all of the Inquisition, due to different climates and latitudes, has the same conditions — and the months are grouped in four “seasons”, corresponding to the temperate areas of the Northern hemisphere (about 90% of the population of the Inquisition is north of the Equator, and most areas in the Southern hemisphere do not have distinct seasons anyway). This is despite the Lāmiejāya plain itself having mostly two seasons (and some parts of the “heartlands” even have no seasons, most notably the area around Līlasuṃghāṇa, which has a local “equatorial” microclimate despite being nearly 15º north of the Equator).
The month names reflect climatic conditions of those particular months in the Nīmbaṇḍhāra plain, the “heartlands” of the Chlouvānem civilization. Not all of the Inquisition, due to different climates and latitudes, has the same conditions — and the months are grouped in four “seasons”, corresponding to the temperate areas of the Northern hemisphere (about 90% of the population of the Inquisition is north of the Equator, and most areas in the Southern hemisphere do not have distinct seasons anyway). This is despite the Nīmbaṇḍhāra plain itself having mostly two seasons (and some parts of the “heartlands” even have no seasons, most notably the area around Līlasuṃghāṇa, which has a local “equatorial” microclimate despite being nearly 15º north of the Equator).


The four seasons the calendar is based on are autumn (''kanami''), winter (''tandaikin''), spring (''tandayena'') and summer (''enaukam''), in the order they appear in the year — these ones are defined by equinoxes and solstices and not by  climate alone (even if the origins of their names, all Toyubeshian, are related to climate). Climatic seasons are totally not uniform across the Inquisition: even in the Lāmiejāya plain, the two seasons (''būṃṣoe'' or dry season and ''dašoe'' or rainy/monsoon season) have vastly different start/end dates and lengths in it. Some areas even define more than four seasons: in and around the metropolitan area of Cami (the most populated on the planet), five seasons are traditionally distinguished, with rain patterns being the defining factor (that area having a markedly wet humid subtropical climate).
The four seasons the calendar is based on are autumn (''kanami''), winter (''tandaikin''), spring (''tandayena'') and summer (''enaukam''), in the order they appear in the year — these ones are defined by equinoxes and solstices and not by  climate alone (even if the origins of their names, all Toyubeshian, are related to climate). Climatic seasons are totally not uniform across the Inquisition: even in the Nīmbaṇḍhāra plain, the two seasons (''būṃṣoe'' or dry season and ''dašoe'' or rainy/monsoon season) have vastly different start/end dates and lengths in it. Some areas even define more than four seasons: in and around the metropolitan area of Cami (the most populated on the planet), five seasons are traditionally distinguished, with rain patterns being the defining factor (that area having a markedly wet humid subtropical climate).


The autumn equinox (''kanampeiṃlalyā'') is the first day of the year, and likewise the spring equinox (''tandayempeiṃlalyā'') is on the (functional) mid-point the year, being the first day of the eighth month — it is not the true mid-point because seasons are not equal: spring is the longest with 108 days, then autumn with 107, winter with 103, and summer with 100. Thus the first part of the year has 210 days while the second one has 208.<br/>
The autumn equinox (''kanampeiṃlalyā'') is the first day of the year, and likewise the spring equinox (''tandayempeiṃlalyā'') is on the (functional) mid-point the year, being the first day of the eighth month — it is not the true mid-point because seasons are not equal: spring is the longest with 108 days, then autumn with 107, winter with 103, and summer with 100. Thus the first part of the year has 210 days while the second one has 208.<br/>
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