New York or Prague: which climate?
New York (United States) has a hot-summer humid continental climate, whereas Prague (Czechia) has a warm-summer humid continental climate, according to the Köppen-Geiger classification.
The values compared here are normals computed over 86 complete calendar years, from 1940 to 2025, using ERA5 reanalysis data from the Copernicus programme. The same method and the same period apply to New York and to Prague.
New York is warmer than Prague by 3.3 °C in annual average: 12.1 °C against 8.8 °C.
New York gets more rain than Prague: 1,098 mm per year against 647 mm.
New York gets 8.8 hours of sunshine per day on average, against 7.9 hours in Prague.
Prague has warmed by +2.5 °C between 1940 and 2025, against +1.7 °C in New York. Prague is therefore warming faster than New York. Both trends are statistically significant.
New York averages 20 hot days (≥ 30 °C) and 75 frost days per year; Prague averages 6 and 89.
Data from ERA5 reanalysis (Copernicus Climate Change Service), redistributed under a CC-BY 4.0 licence. Normals are recomputed whenever the archive is updated.
| Indicator | New York | Prague | Difference |
|---|---|---|---|
| Mean daily temperature | 12.1 °C | 8.8 °C | -3.3 °C |
| Average daily high | 15.7 °C | 12.6 °C | -3.1 °C |
| Average daily low | 8.6 °C | 5.1 °C | -3.5 °C |
| Annual rainfall | 1,098 mm | 647 mm | -451 mm |
| Sunshine / day | 8.8 h | 7.9 h | -0.9 h |
| Hot days (≥ 30 °C) | 20 d/yr | 6 d/yr | -14 d/yr |
| Frost days (< 0 °C) | 75 d/yr | 89 d/yr | +14 d/yr |
| Rainy days (≥ 1 mm) | 118 d/yr | 130 d/yr | +12 d/yr |
| Mean relative humidity | 71 % | 76 % | +5 % |
| Average peak wind | 17.4 km/h | 15.9 km/h | negligible |
A difference is only reported when it exceeds the resolution of the data. ERA5 is a reanalysis on a grid of about 31 km: two nearby cities often fall in the same cell, and below half a degree you are reading the grid, not the climate.