Climate of Zhenia

The climate of Zhenia comprises a wide range of long-term average weather conditions across Zhenia's vast geographic scale and diverse topography, from subtropical to subarctic. Being situated at the eastern seaboard of a continent in the northern hemisphere, northern Zhenia is generally colder than southern Zhenia, while western Zhenia is generally drier than eastern Zhenia. Based on the, there are 14 different major climatic subtypes that can vary greatly, ranging from near its southern edges and  throughout much of southern Zhenia to  throughout much of northern and northeastern Zhenia, and from arid deserts in the northwest, alpine tundras and glaciers in the north and west to  subarctic climate in the far north. Its diverse topography has resulted in the existence of several contrasting. With the exception of arid deserts and tropical monsoon regions as well as alpine tundra and glaciers, four seasons are visible throughout most of Zhenia, with local adjustments: spring (usually March, April and May), summer (June, July, August and early September), autumn (late September, October and early November) and winter (late November, December, January, February).

Northeastern Zhenia
Despite being situated in a similar latitude with most of northern continental Zhenia, northeastern Zhenia is home to a significantly different climate pattern from the inland.

Southern Zhenia
Due to its low latitude, southern Zhenia is home to the warmest and most humid climates in the nation. It is mostly home to a characterized by hot, humid summers and mild winters. Southern Zhenia is also mostly influenced by the existence of seasonal, which result in high concentrations of the region's annual precipitation in the summer season.

Towards the southern tip of the nation, near the Chang River delta, the climate becomes more of a tropical monsoon climate.

Natural disasters and effects
Situated along the eastern seaboard of Tarsis and directly facing the Hanmaric Ocean, Zhenia is susceptible to seasonal.