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Last update: 04:00, 24 Aug 2026
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Katowice sees more rain than most major Polish cities — about 829mm a year, ranging from roughly 40mm in driest February to about 105mm in wettest July. A Katowice rain radar matters here for a reason no other major Polish city shares: mining-driven land subsidence. A single mining tremor near Bytom, part of the Katowice conurbation, can lower the ground by 20–35mm in a single day, disrupting how rainwater and meltwater drain naturally through the Upper Silesian basin.
The mechanism compounds regional rain with a century of coal extraction. The number of anthropogenic reservoirs formed from subsidence across the Katowice conurbation rose from 26 to 369 between 1902 and 1994 — rainwater pools in mining-caused depressions instead of draining normally. Regional Silesia sees 600–800mm of rain a year, predominantly from summer convective storms, which heightens flood vulnerability along the Oder and its tributaries, but in Katowice that rainfall interacts with a post-mining topography unlike anywhere else in Poland.
RainViewer draws its Katowice feed from IMGW, refreshed every 5 minutes, so the map reflects new radar scans rather than a forecast written hours earlier. What the live map shows and a forecast cannot: whether a convective cell is intense enough to overwhelm drainage already weakened by subsidence near Bytom.
July is Katowice's wettest month at around 105mm, driven by the same regional Silesian pattern of summer convective storms that dominates flood vulnerability along the Oder system.
Subsidence-driven reservoir formation is not seasonal — it is an ongoing process from mining activity — but it interacts most visibly with rainwater during the summer convective wet season, when heavy bursts meet already-altered drainage.
February is Katowice's driest month at around 40mm, the standard humid continental winter low.
Mining tremors near Bytom can subside land by 20–35mm in a single day, directly impairing rainwater and meltwater drainage in the area. Residents there benefit from tracking the radar closely during any heavy summer downpour, since standard drainage assumptions do not apply.
Katowice anchors the Silesian Metropolis, a dense agglomeration of more than 40 municipalities with a combined population over 2 million. Commuters checking the radar before a summer storm can time their trip around a passing convective cell in this heavily built-up region.
Katowice Wojciech Korfanty Airport, roughly 30km north of the city in Pyrzowice, is Poland's fourth-busiest with about 7.3 million passengers in 2025, serving 14.3 million people within a two-hour drive. Checking the radar before heading to the airport shows whether a storm cell will clear before departure.
The Katowice conurbation now has 369 subsidence-formed reservoirs, up from just 26 in 1902 — standing water that behaves differently than natural drainage during heavy rain. Nearby residents can use the radar to judge how a storm is tracking relative to these low-lying pools.
RainViewer draws radar data for Poland from the Institute of Meteorology and Water Management (IMGW) via danepubliczne.imgw.pl, updated every 5 minutes. Coverage is comprehensive across the country. Katowice sits at the center of the Upper Silesian basin, so storm systems moving through the wider Silesian Metropolis and toward Bytom are visible on the same map before they arrive.
The fastest way to know is a live hyperlocal radar, since a convective cell can hit one part of the Silesian Metropolis hard while another stays dry. RainViewer pulls fresh IMGW radar scans every 5 minutes, so the map reflects current conditions rather than a forecast written hours earlier.
July is Katowice's wettest month, with regional Silesian convective storms building fast across the dense, 2-million-resident metropolis. Checking the radar before outdoor plans is safer than relying on a single citywide forecast.
Convective storms during the summer peak can disrupt ground traffic and flight operations at the airport, located about 30km north of the city. Checking the radar before a trip to Pyrzowice shows whether a cell is passing through or settling in.
Katowice's flood risk is unusual in Poland because mining-driven land subsidence near Bytom — up to 20–35mm a day after a tremor — disrupts natural drainage, and rainwater now pools in 369 subsidence-formed reservoirs across the conurbation. Residents near mining zones should track the radar closely during any heavy summer rain.
February is Katowice's driest month, averaging around 40mm, well below the July peak near 105mm. Visitors planning time in the Silesian Metropolis or near Bytom should watch for summer convective storms, which build fastest in the June–August window.
A century of coal mining has left the Upper Silesian basin with subsidence-altered topography, so rainwater pools in mining-caused depressions instead of draining normally — a pattern with no equivalent in non-mining Polish cities. A live radar showing where a cell is falling matters more here than a forecast built on standard drainage assumptions.
Yes — RainViewer's hyperlocal radar for Katowice draws directly from IMGW, refreshing every 5 minutes with new scans instead of a periodic forecast update. The map covers the full Silesian Metropolis, so approaching systems are visible before they reach the city.
Yes — RainViewer's rain alerts can be set for a specific point like central Katowice or the Bytom mining zone, so residents get a notification as a cell approaches instead of checking the map manually. That advance window matters most in areas affected by subsidence-altered drainage.
Bytom-area residents and Silesian Metropolis commuters both live with a drainage system reshaped by more than a century of coal mining. A convective cell that would drain normally elsewhere can instead pool in one of the region's 369 subsidence-formed reservoirs.
A generic forecast says scattered showers for Katowice this week. RainViewer's live hyperlocal radar shows a convective cell building fast over Bytom's subsidence zone while central Katowice stays dry — that is the call a resident needs before the water starts pooling.
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See whether a cell over the Silesian Metropolis is heading toward Bytom's subsidence zone in the next two hours.
Set an alert for the Bytom mining area or central Katowice and get notified before a system reaches it.
See whether a storm is tracking across the Upper Silesian basin from the west or breaking apart before it arrives.
Review the last 48 hours to see how a regional Silesian storm system built before it hit the basin.
Track central Katowice, the Bytom mining zone, and Katowice Airport in Pyrzowice at the same time.