The sinking water table of the Homokhátság

Shallow groundwater depth at three monitoring wells on the Danube–Tisza sand ridge — Hungary’s slowly drying interior. Yearly mean depth to groundwater has grown by roughly 2.5–4 metres since the mid-20th century, and all three wells are near their deepest readings on record. Public OVF well data retrieved by an AI agent through ovf-data-mcp. Operational data — preliminary, unchecked.

Yearly mean depth to groundwater (cm below well datum)

One panel per well · deeper is lower · y-scales aligned per panel · hover or focus + arrow keys for values

Data table — yearly mean depth, all three wells