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Last update: 14:00, 9 Sept 2026
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Padua gets around 850-900 mm of rain a year with no true dry season — rain is spread through the year with a broad autumn maximum (Oct-Nov) and a spring secondary peak. A Padua rain radar shows this pattern in a way a monthly average cannot: hyperlocal radar catches the difference between a passing shower over the university district and a sustained system stalling upstream on the Bacchiglione.
That upstream detail matters because Padua's flood risk is driven more by what falls in the mountains than by rain over the city itself. Padua sits on the Bacchiglione river in the Po Valley basin, where stagnant humid air and Atlantic frontal systems from the W/SW dominate, and where autumn scirocco-fed Adriatic moisture can add heavy rain events. Because the Bacchiglione and its tributaries are fed from Alpine and pre-Alpine catchments, a dry afternoon in Padua can still be followed by a river rise hours later as upstream rain arrives downstream.
RainViewer pulls live radar from the Dipartimento della Protezione Civile alongside ARPA Veneto's regional feeds, refreshed every 5 minutes. During the 31 October-2 November 2010 "All Saints flood," up to 149.5 mm fell in the upper Brenta-Bacchiglione basin in 36 hours — the kind of upstream event a live radar map catches well before the river itself responds in the city.
The wet peak, the Po Valley's broad autumn maximum, and the highest-risk window for river flooding given saturated upstream catchments.
A secondary wet spell as frontal systems pick up again.
Hot and humid, with afternoon and evening convective storms and hail risk building over the plain.
Fog and cold with relatively low rainfall, typical of the enclosed Po basin. The Sant'Antonio feast (June) and the university's term calendar, tied to Europe's oldest institutions (founded 1222), mark Padua's seasonal rhythm alongside the weather.
The Bacchiglione river and the Piovego canal running through the historic center are the named flood-risk waterways, with low-lying riverside districts most exposed — as seen in the 2010 All Saints flood that affected roughly 130 Veneto municipalities.
One of Italy's busiest interchange stations, sitting on the Milan-Venice line, sees commuter disruption whenever a storm cell crosses; live radar helps travelers judge platform waits.
Padua sits where the A4 (Milan-Venice) and A13 (Padua-Bologna) intersect, a key freight corridor for the Veneto plain that hauliers monitor for convective storm activity.
With a large student population moving by bike and on foot around Prato della Valle and the historic center, a 5-minute radar update is more useful than a daily forecast for timing a ride.
Visitors to the Basilica and Prato della Valle can check live radar before a walking tour through Padua's historic center.
RainViewer draws radar data for Italy from the Dipartimento della Protezione Civile (Italian Civil Protection Department) national radar network, supplemented by regional radar systems from ARPA agencies including ARPA Veneto, ARPAE Emilia-Romagna, ARPA FVG, and ARPAL, updated every 5 minutes. Coverage spans the Italian mainland, Sicily, and Sardinia. Around Padua, the same feed covers the Veneto plain toward Venice and Vicenza, and upstream toward the Brenta and pre-Alpine catchments.
Check RainViewer's hyperlocal radar map for live rain over Padua, refreshed every 5 minutes from Protezione Civile and ARPA Veneto data. The map shows individual storm cells rather than a citywide average.
Use the 2-hour forecast in 5-minute slices to check whether a convective cell will cross the historic center before you head out.
Live radar shows storm cells approaching before they reach the station, since most systems arrive from the W/SW. Check the update just before you leave.
Yes — the Bacchiglione river and Piovego canal through the historic center overflowed in the 31 October-2 November 2010 All Saints flood, when up to 149.5 mm fell upstream in 36 hours, affecting Padua province and around 20,000 people regionally.
Winter carries the lowest rainfall, though fog is common; among the wetter months, summer's storms tend to be short convective bursts rather than sustained rain.
Because the Bacchiglione is fed by pre-Alpine and Alpine catchments upstream, heavy rain falling in the mountains can raise the river in Padua hours after the city itself stayed dry — a pattern a citywide forecast misses.
Data refreshes every 5 minutes from the Protezione Civile national network and ARPA Veneto's regional radar, showing storm cells as they build rather than an hourly snapshot.
Yes — set a rain alert for a specific point, such as Padova station or Prato della Valle, and RainViewer notifies you before the storm cell arrives based on its tracked direction.
Padua's A4/A13 logistics crossroads and Padova station both run on schedules that a sudden convective storm can disrupt within minutes, and the Bacchiglione's upstream flood risk means the city's own weather is only part of the picture. A static forecast cannot show either of these in time.
RainViewer gives you a 2-hour forecast in 5-minute slices, rain alerts before a storm reaches Padova station or Prato della Valle, direction arrows tracking systems in from the W/SW, 48 hours of radar history to see how an event like the 2010 All Saints flood developed, and the ability to track multiple locations at once — the historic center, the Bacchiglione riverbank, and the university district together.
A forecast says rain is possible in Padua today. Live hyperlocal radar shows you the storm cell already building over the Piovego canal.
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