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Last update: 11:00, 24 Aug 2026
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Boguszow-Gorce sits in the Central Sudetes, 5 km west of Walbrzych, close enough to the Chelmiec massif and the Walbrzych and Kamienne Mountains that the terrain itself changes how rain behaves from one part of town to another. A Boguszow-Gorce rain radar earns its value from that mountain-moderated setting: precipitation runs higher here than in Poland's lowland regions, and elevation shifts within the town limits mean rain lower down can fall as frost or snow higher up on the same day. A hyperlocal radar is the only way to see that split as it happens.
The mechanism is altitude and ridge proximity rather than any single river. Annual average daytime highs run around 13°C, dropping to about 4°C overnight, with a year-round daily average near 8°C — cooler than lowland Polish cities at the same latitude. Spring, from March through April, brings frequent rain lower in town alongside lingering frost and snowfall risk at higher elevations, a two-tier pattern tied directly to the town's varied terrain. Beneath all of it sits a documented risk layer of a different kind: mining shafts dating to 1502, including one historically located in the town square itself, create known subsidence risk that can interact with heavy rain and groundwater.
RainViewer draws its Boguszow-Gorce feed from IMGW, refreshed every 5 minutes, so the map reflects new radar scans rather than a forecast written before a cell reached the higher ground near the Chelmiec massif. What a live map shows and a forecast cannot: whether rain building over the ridge is falling as rain in the lower town or as snow near the mountain-facing edges.
Summer here is moderately warm rather than hot, running 18–22°C with a town-wide max near 24°C and min near 13°C, cooler than lowland Polish cities at the same latitude because of the surrounding Sudetes terrain.
January is the coldest month, with a max around 0°C and a min near -6°C, bringing the elevated terrain's frost and snow exposure to its peak.
Spring brings frequent rain in the lower parts of town while frost and snowfall remain possible at higher elevations within the city limits, a pattern tied directly to local altitude variation near the Chelmiec massif.
Boguszow-Gorce's mining terrain dates to 1502, when it became one of the most important lead and silver centers in the Sudeten part of Silesia, and one shaft was historically located directly in the town square — a factor that can interact with heavy rain and rising groundwater even without a confirmed direct link on record. Residents near known mining terrain can watch the radar during a heavy rain event rather than waiting for a subsidence report.
Skład Opału "Alanex" operates as a qualified coal supplier and transport provider for Polish mining companies based in Boguszow-Gorce, running outdoor loading operations exposed to the town's mountain-moderated rain pattern. Checking the radar before a loading window shows whether a cell is building over the ridge or has already passed.
Rail line no. 274 runs through Boguszow-Gorce on the Walbrzych–Jelenia Gora section, with the Boguszow-Gorce Zachod station connecting directly to Walbrzych, Jelenia Gora, and Wroclaw. Rail staff checking the radar before a shift get more warning of an incoming mountain storm than the timetable alone provides.
The provincial road linking Walbrzych and Jelenia Gora runs through Boguszow-Gorce, the main road-transport artery connecting the former mining twin-town to both regional centers. Drivers and dispatchers checking the radar before a route decision can see whether rain is settling over the ridge or clearing.
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. Boguszow-Gorce sits close enough to Walbrzych and Jelenia Gora that ridge-building storms across the Central Sudetes are visible on the same map before they cross into town.
The fastest way to know is a hyperlocal radar, since rain here can fall as light showers in the lower town while turning to frost or snow near the Chelmiec massif's higher ground. RainViewer pulls fresh IMGW radar scans every 5 minutes, showing conditions as they are rather than a forecast written before the cell reached the ridge.
Yes — Skład Opału "Alanex" runs outdoor coal-supply and transport operations exposed to Boguszow-Gorce's mountain-moderated rain pattern. Checking the radar before a loading window shows whether a cell is building over the ridge or has already cleared.
Rail line no. 274 connects Boguszow-Gorce Zachod station to Walbrzych, Jelenia Gora, and Wroclaw, and mountain storms near the Chelmiec massif can affect conditions along the route. Checking the radar before a scheduled departure gives more warning than the timetable alone.
No specific historical flood event has been documented for Boguszow-Gorce, but the town's historic mining terrain — including shafts dating to 1502, one of which sat in the town square — creates a documented subsidence risk that can interact with heavy rain and groundwater. Residents near known mining ground should still track the radar during any heavy rain event as a precaution.
Summer runs moderately warm at 18–22°C, cooler than lowland Polish cities at the same latitude, while January brings the coldest and snowiest stretch of the year. The March–April spring transition carries the widest swing, with rain lower in town and lingering frost or snow at higher elevations.
The town's position near the Chelmiec massif and the Walbrzych and Kamienne Mountains means elevation changes rain into frost or snow within the same city limits, a two-tier pattern most visible during the spring transition. A single town-wide forecast cannot show that split — only a live radar tracking the cell's position relative to the ridge can.
Yes — RainViewer's hyperlocal radar for Boguszow-Gorce draws directly from IMGW, refreshing every 5 minutes with new scans covering the town and the surrounding Central Sudetes terrain. That ridge-level coverage is what shows a storm intensifying before it reaches the lower town.
Yes — RainViewer's rain alerts can be set for a point like the town square or the Boguszow-Gorce Zachod station, so residents and rail staff get a notification as a cell approaches instead of checking the map manually. That advance window matters most during the two-tier spring transition.
Alanex's coal-loading operations and rail staff at Boguszow-Gorce Zachod station both work in a town where elevation changes rain into frost or snow within the same city limits. The historic mining shafts beneath the town square add another layer of caution during heavy rain, and a mountain storm near the Chelmiec massif can build faster than a valley forecast suggests.
A generic forecast says light rain for Boguszow-Gorce this afternoon. RainViewer's live hyperlocal radar shows the same system already dropping snow near the Chelmiec massif while rain continues in the lower town — that is the gap between a forecast and what the ridge is actually doing.
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See whether a cell over the Chelmiec massif clears the ridge or intensifies toward the lower town.
Set an alert for the town square or the Alanex coal yard and get notified before rain reaches it.
See whether a front is tracking in from the Kamienne Mountains or breaking apart before it crosses into town.
Review the last 48 hours to see how a mountain storm built and moved across the Central Sudetes.
Track the town square, the Alanex coal yard, and the Boguszow-Gorce Zachod station at the same time.