No upcoming precipitation for the next hour.
Last update: 11:00, 24 Aug 2026
Free to download * Essential from $0.83 * Prices vary by region and promotions.
Home, office, kids' school - all at once, no switching tabs.
Get notified 15 minutes before rain - while you can still change your plans.
Live radar without opening the app - on your lock screen or home screen.
Bialystok rain radar users watch a city where summer convective storms concentrate in a narrow window: July delivers roughly 91mm, the wettest month by a wide margin, while February holds the line at around 30mm. A hyperlocal radar for Bialystok matters most in that July peak, because the same storms that green up Podlaskie's dairy pastures also drop the heaviest single-event rainfall on a city center that has grown less able to absorb it.
The mechanism is urban, not just meteorological. Dense development and sealed surfaces across central Bialystok have amplified runoff intensity citywide, and a local flood-risk study documents that the share of annual rainfall coming from events above 20mm has risen roughly 15% over the past three decades — about 5% per decade. That trend, combined with a documented urban heat island effect, means a storm that would have been routine decades ago now carries more flood risk in the same streets today. A city-wide forecast built on an average cannot show which block absorbs that runoff and which one floods.
RainViewer draws its Bialystok feed from Poland's Institute of Meteorology and Water Management (IMGW), refreshed every 5 minutes, so the map reflects the newest radar scan rather than a forecast written hours earlier. Bialystok's snow cover holds for 80-100 days most winters, and the same radar that tracks summer storms also shows snowfall moving across the city in the cold months. What live radar reveals that a forecast cannot: whether a convective cell over the Biala River corridor is intensifying before it reaches downtown or dissipating on approach.
July is Bialystok's wettest month at around 91mm, driven by summer convective storms. Dairy cooperatives and farms across Podlaskie Voivodeship, the country's dairy-heavy agricultural region, run their heaviest logistics around this window, and the city center sees its highest flash-flood risk from short, intense downpours.
Bialystok is one of Poland's coldest regions, with snow cover typical for 80-100 days a year. February is the driest month for rain at around 30mm, though snow — not rain — dominates the radar picture through this stretch.
Snowmelt and early rain events overlap unpredictably in spring, feeding the Biala and Suprasl rivers before the summer convective season builds. Retention reservoirs have been identified as a needed adaptation given limited sewer capacity in this transition window.
A documented urban heat island effect intensifies convective and urban flooding risk in central Bialystok, and sealed surfaces from dense development amplify runoff. Checking the radar before a July storm shows whether a cell is passing through or stalling over downtown.
Podlaskie Voivodeship, with Bialystok as its capital, is Poland's dairy-heavy agricultural region. Farmers and cooperatives timing outdoor work and milk collection routes around summer storms benefit from watching a cell's radar track rather than a district-wide forecast.
The S8 expressway and rail line connect Bialystok to Warsaw, with Warsaw Modlin Airport reached by intercity bus. A driver or dispatcher checking radar before a run can tell whether rain on the route is a brief shower or a longer system.
The regional airport's grass runways make it more rain-sensitive than paved-runway fields. Flight planners watching the live radar can time takeoffs and landings around a passing cell instead of guessing from an hourly forecast.
The Biala River, the city's main urban rainwater receiver, runs south to north-east through Bialystok, while the Suprasl River forms a secondary flood-risk waterway nearby. Residents near either channel can track a storm's radar signature as it approaches instead of waiting for a flood bulletin.
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. Bialystok sits close enough to the Suwalki and Lomza areas that storm cells crossing the wider Podlaskie region show up on the same sweep before they reach the city.
The fastest way to know is a live hyperlocal radar, since summer convective storms can turn a dry afternoon wet within minutes and rain often falls on one side of the city while the other stays clear. RainViewer pulls fresh IMGW radar scans every 5 minutes, so the map reflects current conditions rather than an hourly forecast.
Bialystok is workable in June through August if visitors check the radar before outdoor plans, since July's convective storms can be short but intense. The city's parks and old town areas clear quickly after a passing cell, so a live map beats waiting out a forecast window.
Heavy convective rain on the S8 expressway and connecting rail line can slow the Bialystok-Warsaw corridor, particularly during July's storm peak. Checking the radar before a trip shows whether a cell is sitting over the route or has already moved through.
Central Bialystok carries documented flood risk from a combination of urban heat island effects and sealed surfaces that amplify runoff, concentrated along the Biala River corridor. A local hydrological study found that rainfall from events above 20mm has risen about 15% over the past 30 years, so residents near the Biala or Suprasl rivers should watch the radar closely during summer storms.
February is Bialystok's driest month for rain at around 30mm, though it falls within the region's snowiest stretch, with snow cover typical for 80-100 days a year. Visitors preferring rain-free outdoor time without snow should aim for early spring before the summer convective season builds in June.
July's convective storms form as isolated cells rather than steady regional rain, so one side of the city can get a heavy downpour while another stays dry. Dense development and sealed surfaces in the city center also mean the same storm produces more runoff downtown than in less-built areas, which a single regional forecast cannot show.
Yes — RainViewer's hyperlocal radar for Bialystok draws directly from Poland's Institute of Meteorology and Water Management (IMGW), refreshing every 5 minutes with new scans instead of a periodic forecast update. The map covers the wider Podlaskie region, so storms approaching from Suwalki or Lomza are visible before they reach the city.
Yes — RainViewer's rain alerts can be set for a specific point like the city center or the Biala River corridor, so residents get a notification as a cell approaches instead of checking the map manually. That advance window matters most in July, when convective storms can build and hit within the hour.
Central Bialystok floods fastest where sealed surfaces meet a heavy July storm, and dairy farms across Podlaskie time outdoor work around the same convective cells. A regional forecast cannot tell a resident near the Biala River whether this hour's storm is passing through or settling in.
A generic forecast says scattered storms for Bialystok this week. RainViewer's live hyperlocal radar shows it is already pouring over the Biala River corridor while the S8 expressway stays dry — that is the call a commuter makes every time a summer cell builds.
Track rain in Bialystok — free Upgrade to Essential for alerts, forecasts, and full radar history
See whether a cell building over the city center stays light or intensifies in the next two hours.
Set an alert for the Biala River corridor and get notified before a storm reaches downtown.
See whether a cell is tracking in from the southwest or building locally over Bialystok.
Review the last 48 hours to see how a July storm system developed before it reached the city.
Track the city center, the Suprasl River area, and the S8 expressway corridor at the same time.