🇷🇺 Moscow vs 🇺🇸 New York City

Moscow's continental climate features harsh winters and warm summers, shaped by its position on the East European Plain with no nearby mountains or seas to moderate extremes. The Moscow River and its tributaries create humidity corridors through the city, while the vast urban sprawl generates one of Europe's most pronounced urban heat islands — the city center can be 5–10°C warmer than surrounding countryside on calm winter nights. Extensive parklands, Soviet-era green belts, and elevation changes between river valleys and glacial moraine hills produce distinct microclimates across the metropolitan area.

Humid continental — hot summers, cold winters, year-round precipitation

New York City has four distinct seasons. Fall is the sweet spot: mild temps, low humidity, and the city at peak energy. Summers are hot and muggy; winters bring snow and bitter wind chill, especially near the waterfront.