Climate of Kadalia
Kadalia, despite it's relatively small size, is very diverse climatically. 21 Köppen climate types are found there, from Af (tropical rainforest) to EF (polar ice cap). Since Kadalia is located in the Southern Hemisphere, it's northern parts are the warmest and southern ones are the coldest.
Kadalia's southernmost region, Sejuk, is dominated by frigid tundras. Due to close proximity of Sagastan it can become extremely cold during winters and barely gets mildly warm during summers. To the north, around the ice-capped Besar Mountains, warmer "austral zone" is located, with moist austral rainforests and "beech taiga" west of the mountains and dry semi-deserts and steppes east of them. Eastern coast has summerwet precipitation pattern. A few spots in the west have Cfc rather than Dfc climate.
Even more north is the area dominated by Dfb warm-summer continental climate; steppes and temperate forests are located there. In the east Dfb is replaced by Dwb. Northern coast of Sea of Sejuk is semi-arid, and in the west, the Dege Peninsula, mild Cfc/Cfb is most prevalent. Dege coast is the wettest part of Kadalia. Inland Dege is more continental. Hpt-summer continental is absent from Kadalia.
To the north, the mountain range divides the climates of west and east coast more drastically. Eastern Kadalia turns humid subtropical, summerwet at some localities. West coast, on the other hand, becomes winterwet mediterranean and then arid, with a large desert existing at the northern half of Voay Peninsula. Finally, Tanana Peninsula is tropical, with it's west coast dominated by Aw and Am and east coast being Af.
Such varied climatical zones cause Kadalia to be extraordinarily biodiverse.
About Kadalia
