The comparison is based on climate patterns rather than geography.

The eastern United States and eastern China, for example, share humid summers, significant rainfall, and four distinct seasons.

The Pacific Northwest has a climate remarkably similar to parts of the United Kingdom and western Europe, thanks to the moderating influence of nearby oceans.

Meanwhile, much of the Great Plains experiences temperature swings and precipitation patterns comparable to regions of Mongolia and Central Asia.

One of the biggest reasons North America and Eurasia differ is the orientation of their mountain ranges.

In North America, major ranges like the Rockies run north to south, allowing cold Arctic air to plunge deep into the continent. In Europe, mountain systems tend to run east to west, helping block extreme temperature shifts and creating milder conditions across much of the continent.

The map is not claiming these places are identical. Culture, vegetation, soils, and local weather patterns can vary dramatically.

But, it highlights how regions on opposite sides of the world can share surprisingly similar climate characteristics despite looking nothing alike on a political map.

Added Fact: Western Europe is significantly warmer than most places at the same latitude because of the North Atlantic Current. London sits farther north than Calgary, Canada, yet its winters are generally much milder due to warm ocean currents carrying heat from the tropics.

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