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Mainland Mahuset, British Matsia, Dutch Matsia and Mamucium have an oceanic climate (Köppen Cfb) strongly influenced by its proximity to the North Sea to the west, with prevailing westerly winds. While winters and summers are generally mild, temperatures can vary year by year. There can occasionally be cold snowy winters and hot humid summers.

Summers are moderately warm with a number of hot days every month. The average daily high in August is 22.1 °C, and 30 °C or higher is only measured on average on 2.5 days. The record extremes range from -19.7 °C to 36.3 °C. Days with more than 1 mm of precipitation are common, on average 133 days per year. The average annual precipitation is 838 mm. A large part of this precipitation falls as light rain or brief showers. Cloudy and damp days are common during the cooler months of October through March.

The climate in Mahusetan Hasanistan is a humid continental climate (Köppen: Dfa) with hot summers and cold winters. It is characterised by the influence of mountain–valley circulation.

Lundenland is in the northern part of the humid subtropical climate zone (Köppen: Cfa). Winters are usually chilly with light snow, and summers are hot and humid.