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Last update: 10:00, 5 Jul 2026
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Jeddah's rain character is dominated by the Red Sea Trough — a northward extension of southern Red Sea low-pressure systems that triggers intense mesoscale convective outbreaks in winter. The city receives ~63 mm annually on average, but individual events dump 70-182 mm in 6-24 hours. November 2022 broke records with 182 mm in 24 hours. This is not steady rain; it's explosive, concentrated bursts that catch forecasts completely off guard. A Jeddah rain radar must track minute-by-minute movement because the intensity shifts block-to-block across the Corniche and pilgrimage districts.
The coastal escarpment creates a moisture amplifier. The Hejaz mountains 150 kilometers east redirect plumes of humid air from the Red Sea toward the coastal plain. December-March relative humidity climbs above 80 percent, building instability layers that convective storms exploit. When a cell develops, it taps ocean moisture and terrain forcing simultaneously — the result is far more intense than inland Riyadh gets. This geographic mechanism explains why Jeddah floods catastrophically while inland cities stay dry.
RainViewer draws radar data from regional meteorological networks, updated every 5 minutes. The live map reveals exactly where the Red Sea Trough cell is overhead — whether rain is hitting the Islamic Port, Umrah-district hotels, or the Haramain High Speed Railway corridor near Wadi Alaqiq. No forecast can show you that precision; only a live hyperlocal radar gives you the street-level view.
Peak December-January, when Umrah pilgrimage volumes peak at 30 million-plus annual passengers through King Abdulaziz Airport. The Red Sea Trough intensifies during these months, triggering the year's most severe convective events. This is the most operationally disruptive period — pilgrim delays cascade when the airport closes, port operations freeze during storm surge, and the Corniche becomes inaccessible.
Sporadic thunderstorm onsets occur, but intensity is less predictable than core season. October shows the first pulses; April shows the last. Forecasts are least reliable here because models struggle with boundary timing.
Effectively zero precipitation. Heat and humidity define operations.
Millions of pilgrims arrive December-January intending to perform Umrah. Heavy rain disrupts access to Prophet's Mosque (second-holiest Islamic site), closes parking, floods pedestrian routes, and strands buses and taxis. Checking the radar 20-30 minutes ahead tells pilgrims whether to leave their hotel now, wait an hour, or reschedule the mosque visit — the difference between a meaningful experience and a chaotic evacuation.
Jeddah's main airport (19 km north of city) handles 30 million-plus annual passengers, many Umrah-bound. Heavy rain triggers runway closures and cascades to delayed flights, missed connections, and pilgrim logistics standdowns. The radar shows exactly when convective cells will pass overhead, letting air traffic control adjust landing sequences before announcing cancellations.
Jeddah's port is the western gateway for Hajj logistics — containers of food, supplies, and goods destined for Mecca and Madinah stage here. Extreme rainfall (like the 182 mm event) causes port drainage failures and crane shutdowns. Checking the radar prevents loading during incoming cells and resumes operations after cells clear.
Both festivals run January-March during peak rainy season. Outdoor screenings and waterfront events on the Corniche promenade are canceled by convective outbreaks. A live radar tells organizers within 30 minutes whether to relocate indoors or postpone.
RainViewer aggregates radar data for Saudi Arabia from regional meteorological networks, updated every 5 minutes. Coverage focuses on the populated Hejaz corridor (Jeddah, Makkah, Madinah), the Najd plateau (Riyadh and central oasis cities), and the Eastern Province Gulf coast (Dammam, Al Khobar, Al Jubail). Coverage in remote interior desert and southern highlands varies. From Jeddah, radar visibility extends inland toward Makkah and Madinah along the pilgrimage route, and northward along the Red Sea coast toward Yanbu.
Only a live radar answers this because rain in Jeddah is hyper-localized — when the Red Sea Trough cell is overhead, it's violent and sudden. A hyperlocal radar shows the exact convective cell position and whether it's parked over the Corniche or approaching from the gulf. If the cell is on the map moving toward your location, expect heavy rain within 15-20 minutes.
Check the radar for intense cells in the next 2-3 hours. If you see a convective signature over Wadi Alaqiq or the inland zones, timing matters — rain hits hard but clears fast (typically under an hour). Wait 90 minutes and go; the mosque access will be normal. If the radar is clear, go immediately.
If the radar shows a convective cell within 40 kilometers of the airport (19 km north), expect delays; if a cell is directly overhead, expect closure. Check 2-3 hours before departure — the radar shows whether King Abdulaziz will reopen in time for your flight window or you should reschedule.
Yes, catastrophically. Wadi Alaqiq (five major sub-catchments) and Wadi Al-Rummah are the primary flood corridors. November 2009 killed 113 people and damaged 10,000 homes; January 2011 and November 2022 both brought devastating floods. The Hejaz terrain accelerates runoff into these narrow wadis. Avoid wadi crossings and low-lying districts (Corniche exposed to Red Sea storm surge plus inland flooding) during active rain events.
May through September is bone-dry. If you're visiting December-January for Umrah, expect rain — January is the peak wet month. Book late September, June, or July for guaranteed clear skies. Note: December and January are also peak pilgrimage season, so booking early is essential.
The Red Sea and Hejaz mountains create a focusing mechanism that inland cities (Riyadh) don't have. Moist air from the gulf is forced upslope and redirected toward the coastal plain by 150-kilometer-distant escarpment. This orographic lifting combined with extreme coastal humidity (80%+ in winter) creates instability that convective cells exploit — the result is 70-182 mm events, not the 20-36 mm bursts Riyadh gets. Forecasts fail because they don't resolve this 150-kilometer geographic boundary accurately.
Every 5 minutes from regional meteorological networks. This update frequency is critical in Jeddah because convective cells develop and dump their full intensity within an hour — a forecast updated daily or even twice daily has already missed the decision window entirely.
Yes. Set a rain alert on the railway corridor near Wadi Al-Rummah or Wadi Alaqiq. RainViewer notifies you 10-15 minutes before heavy rain arrives, letting you confirm whether the rail link will close, reschedule passenger movements, or prepare drainage systems before the cell arrives.
Red Sea storms in winter build fast and dump catastrophic rain on Jeddah's wadi network.
Forecasts update once or twice daily; convective cells develop and intensify within minutes. By the time a forecast updates, the decision window has closed.
Your weather app says "heavy rain expected January 15." RainViewer shows the Red Sea Trough cell is 60 kilometers offshore and arriving over the Corniche in 28 minutes — that's the decision pilgrims and port operators make in Jeddah every winter.
Track rain in Jeddah — free Upgrade to Essential for alerts, forecasts, and full radar history
watch convective cells develop over the Red Sea and track exactly when they'll reach the Corniche or inland pilgrimage districts.
set one on King Abdulaziz Airport or Prophet's Mosque route and get 10-15 minutes notice before the cell hits.
winter systems typically approach from the Red Sea and move inland; the arrows show whether the cell is accelerating or stalling overhead.
scroll back to see where yesterday's cell went and predict where today's system will track.
monitor rain over King Abdulaziz Airport, Jeddah Islamic Port, and the Umrah route simultaneously.