The California wildfires occurred in conjunction with dynamic anticyclogenesis over western North America. Downstream trough development triggered a Mexican cold surge and subsequent record-breaking heavy rains in the Mexican states of Chiapas and Tabasco. The focus for the heavy rains was strong low-level warm-air advection along the southeastern margin of the cold surge in the presence of westward-moving tropical moisture, in part from developing Tropical Cyclone (TC) Noel situated near Hispaniola. The cold surge-induced sea level pressure difference between northern and southern Mexico resulted in an exceptionally strong and moist northerly upslope flow that allowed sustained heavy rainfall to occur in Chiapas and Tabasco.
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