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Last update: 19:00, 9 Jul 2026
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Salt Lake City receives its most impactful rain during November–March (frontal+snow) and July–September (monsoonal convection), and the Salt Lake City rain radar shows what a standard forecast cannot: exactly which streets are in the path of an incoming cell and how many minutes remain before it arrives. A hyperlocal radar is the practical tool for anyone navigating Salt Lake City's weather — from commuters on the freeway to outdoor event organizers to residents near Jordan River and Mill Creek flooding.
The geography that shapes Salt Lake City's rain risk comes from semi-arid Wasatch Front; Great Salt Lake-effect snow; spring snowmelt flooding; summer afternoon convection. When intense cells develop, they approach primarily from west over Wasatch Mountains, and the local terrain concentrates runoff into Jordan River and Mill Creek flooding rapidly. Standard 12-hour forecasts cover the broader region; a live radar shows the cell boundary at 250-meter resolution — the neighborhood-level distinction that changes whether you leave now or wait 30 minutes.
RainViewer pulls live NEXRAD data from KMTX (Salt Lake City), updated every 4–6 minutes. The map shows the exact storm position and movement vector over Salt Lake City, Utah, including direction arrows showing whether a cell is tracking toward the city center or moving away. What the live map reveals that no forecast can: whether the cell building to the west will reach your specific block in Salt Lake City or dissipate before arrival.
Salt Lake City's highest-risk weather window aligns with November–March (frontal+snow) and July–September (monsoonal convection), when semi-arid Wasatch Front drives the most intense precipitation events. This is when Jordan River and Mill Creek flooding is most likely to cause disruption and when the radar is most operationally valuable for anyone planning outdoor activities, managing outdoor venues, or commuting through flood-prone corridors in Salt Lake City.
The weeks before and after the main rain season bring unpredictable conditions in Salt Lake City — storm intensity varies widely, and forecast models are least reliable during these transitions. Outdoor activities, construction schedules, and event planning in Salt Lake City are most vulnerable to unexpected weather during the seasonal transition windows.
During May–June (snowmelt) and April–May (frontal), Salt Lake City sees its lowest rain probability. Outdoor events, construction, and recreational activities proceed with reduced weather risk. Some residual risk remains from occasional frontal systems or isolated convection, but Salt Lake City is most reliably dry during this period.
Salt Lake City's Jordan River and Mill Creek flooding can rise rapidly during intense rain events. A live radar showing an intense cell approaching from west over Wasatch Mountains gives residents and property managers 20–30 minutes to move vehicles, prepare drainage systems, and alert household members before conditions become dangerous.
Rain events in Salt Lake City can close roads and create dangerous driving conditions with minimal warning. Checking the radar 20 minutes before departure reveals whether an incoming cell will clear before your route or whether a 30-minute delay will mean dry roads — a practical decision that saves time and reduces flood-crossing risk on Salt Lake City's most weather-sensitive corridors.
Salt Lake City's outdoor venues, parks, and recreational areas are directly exposed to the seasonal rain events that characterize Utah's November–March (frontal+snow) and July–September (monsoonal convection) weather window. A live radar check 30–60 minutes ahead tells event managers and outdoor enthusiasts whether to proceed with outdoor plans or prepare for disruption.
Salt Lake City's Church of Jesus Christ of Latter-day Saints HQ sector operates facilities and transportation networks sensitive to weather disruptions. Rain events that cause road closures, reduce visibility, or create safety hazards for outdoor workers are most actionable with 20–30 minutes' advance warning from a live radar — enough time to shelter workers, delay vehicle dispatches, or alert logistics teams before conditions deteriorate.
RainViewer aggregates radar data for the United States from the NEXRAD network operated by NOAA's National Weather Service — 160 WSR-88D stations covering the contiguous US, Alaska, Hawaii, and US territories. Data updates every 4–6 minutes as each station completes its scan cycle. RainViewer processes and displays NEXRAD data at up to 250-meter resolution, preserving the raw scan data rather than smoothing it into regional averages. For Salt Lake City, Utah, the primary NEXRAD source is KMTX (Salt Lake City), providing hyperlocal radar coverage across the area.
Yes — Salt Lake City's Jordan River and Mill Creek flooding creates documented flood risk during intense rain events. Semi-arid wasatch front means that rainfall runs off rapidly into drainage channels and low-lying streets. Avoiding jordan crossings and low underpasses during active radar cells reduces flood risk significantly.
Salt Lake City's primary rain season runs through November–March (frontal+snow) and July–September (monsoonal convection), when semi-arid Wasatch Front drives the most active weather. The driest period is typically May–June (snowmelt) and April–May (frontal), when outdoor activities and travel planning carry the lowest weather risk.
Salt Lake City's rain character is shaped by semi-arid Wasatch Front, which creates localized precipitation patterns that vary significantly across the city. A forecast covers the broader Utah region; a hyperlocal radar at 250-meter resolution shows the actual cell position over Salt Lake City in real time, updated every 4–6 minutes from KMTX (Salt Lake City).
Yes — RainViewer displays live NEXRAD data for Salt Lake City at up to 250-meter resolution, updated every 4–6 minutes from KMTX (Salt Lake City). The map shows current precipitation, storm movement direction, and a 2-hour nowcast — so you can see whether the cell approaching from west over Wasatch Mountains will reach Salt Lake City or change track before arrival.
Storm speed varies, but most convective cells affecting Salt Lake City move at 20–40 mph, giving 15–30 minutes of advance warning when a cell appears on the radar 10–15 miles away. Stalling systems — which bring the most severe flooding — are visible on radar as cells with little lateral movement over Salt Lake City's watershed.
RainViewer Essential sends a rain alert 10–15 minutes before precipitation reaches your saved location in Salt Lake City. Set an alert for your home, workplace, or outdoor venue — the alert fires when radar confirms rain approaching your specific pin, not just a general Salt Lake City area warning.
NEXRAD radar data from KMTX (Salt Lake City) is updated every 4–6 minutes and processed at up to 250-meter resolution — significantly more precise than standard weather app forecasts. For Salt Lake City, this means the radar can distinguish whether rain is falling in one neighborhood while an adjacent area remains dry, a distinction that is common during Salt Lake City's primary rain season.
When the radar shows a fast-moving intense cell (deep red or purple colors) approaching Salt Lake City from west over Wasatch Mountains, allow 20–30 minutes to complete outdoor tasks, move vehicles from flood-prone areas near jordan corridors, and ensure outdoor workers or guests are aware. Most Salt Lake City convective cells clear within 45–90 minutes, so waiting out an approaching cell is often the practical choice.
Salt Lake City's Jordan can rise within 30 minutes of an intense cell — the radar gives you the window a forecast cannot.
A forecast tells you rain is likely. The radar tells you the cell is approaching from west over Wasatch Mountains and will reach Salt Lake City in 18 minutes.
Your weather app says storms likely for Salt Lake City. RainViewer shows the cell is 8 miles from Salt Lake City center and arriving in 12 minutes.
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Salt Lake City storms arrive predominantly from west over Wasatch Mountains; arrows show the exact track
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