Why can drought occur in central and northeastern England?

Droughts occur in central and northeastern England primarily because these regions receive significantly less precipitation compared to other parts of the country. While England is generally characterized as a wet nation—particularly in the northwest and southwest—the central and northeastern areas receive less than 30 inches (750 mm) of rainfall annually.1

This lower volume of precipitation makes these regions susceptible to frequent drought conditions. In contrast, parts of the southeast experience even lower levels of annual rainfall, averaging only 20 inches (500 mm). The variability of the English climate is a defining feature of the region, often resulting in unpredictable weather patterns that have historically influenced the nation's culture and landscape.1