1,237 first-hand accounts of flood events in Arizona, ranked by impact. Each is a NOAA-written narrative of the moment.
A long wave trough moved across Arizona on on New Year's Day with bringing widespread precipitation. Snow levels were initially relatively high for this time of the year. The snow levels dropped rapidly as a cold front associated with the trough moved across the area.
Read the full account →A breach in a berm along Rucker Creek near the northeast edge of Elfrida caused flash flooding in part of town on August 23. Additional rainfall in town and upstream of the breach exacerbated the flooding later that day.
Read the full account →Thunderstorms developed over the Tucson mountains causing several washes to flood in northwest Tucson. At 1815 MST, a spotter reported that he had to pull his car over due to flooding on Camino del Cerro Road.
Read the full account →There was a swift water rescue, when a driver was washed a quarter of a mile downsteam in a wash located north of Kolb Road in Sahuarita. Also, there was a family on Tatanka Lane that had to take refuge in a tree when the home became flooded.
Read the full account →Aa high pressure circulation centered near the Four Corners allowed deep monsoon moisture to become thoroughly entrenched across northern Arizona. Surface dew points were generally above 60 F south of the Mogollon Rim, with values in the 50s along and north of the Rim.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
Read the full account →In a classical monsoonal regime, with deep-layered east to southeast flow, high instability (MLCAPE in excess of 1000-1500 J/KG) along with abundant moisture (PWAT 1.8+ inches) resulted in an environment favorable for thunderstorms.
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