Davostag stretches across a large extent of the north-west of the island-continent Makon. From north to south the East Makonian Plain is clad sequentially in tundra, coniferous forest, mixed and broad-leaf forests, grassland, and mountains (fringing the Makonian Sea) as the changes in vegetation reflect the changes in climate.
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| - Davostag stretches across a large extent of the north-west of the island-continent Makon. From north to south the East Makonian Plain is clad sequentially in tundra, coniferous forest, mixed and broad-leaf forests, grassland, and mountains (fringing the Makonian Sea) as the changes in vegetation reflect the changes in climate.
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| - Federal Republic Of Davostan
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| - Liberty, Democracy, Capitalism
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| - National Anthem of Davostan
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abstract
| - Davostag stretches across a large extent of the north-west of the island-continent Makon. From north to south the East Makonian Plain is clad sequentially in tundra, coniferous forest, mixed and broad-leaf forests, grassland, and mountains (fringing the Makonian Sea) as the changes in vegetation reflect the changes in climate. The climate of Davostag formed under the influence of several determining factors. The enormous size of the continent and the remoteness of many areas from the sea result in the dominance of the continental climate, which is prevalent in Davostag except for the tundra Mountains in the south obstructing the flow of warm air masses from the Makonian Sea and the plain of the north makes the country open to Arctic and Atlantic influences. Throughout much of the territory there are only two distinct seasons — winter and summer; spring and autumn are usually brief periods of change between extremely low temperatures and mildly high. The coldest month is January (on the shores of the sea—February), the warmest usually is July. Great ranges of temperature are typical. In winter, temperatures get colder both from south to north and from west to east. Summers can be quite hot and humid. The continental interiors are the driest areas.
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