Dynamics of a Simulated North American Monsoon Gulf Surge Event

• Published in: Monthly weather review Vol. 141; no. 9; pp. 3238 - 3253
• Main Authors: NEWMAN, Andrew J, JOHNSON, Richard H
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 01.09.2013
• Subjects: Climatology; Convection; Cyclones; Disturbances; Earth, ocean, space; Exact sciences and technology; External geophysics; Gravity; Gulfs; Meteorology; Monsoons; Outflow; Principal components analysis; Severe weather; Simulation; Surges; Tropical cyclones; Weather; Gulf of California; Mexico; Pacific Ocean; Northeast Pacific; United States; North Pacific; ISE, Mexico, California Gulf; models; Gravity current; atmospheric precipitation; Surge; tropical zone; inundations; North America; Precursor; deserts; Dynamical evolution; Severe weather; Tropical cyclone; cooling; transient phenomena; Natural hazards; monsoons; Easterly wave
• ISSN: 0027-0644; 1520-0493
• DOI: 10.1175/MWR-D-12-00294.1

Gulf surges are transient disturbances that propagate along the Gulf of California (GoC) from south to north, transporting cool moist air toward the deserts of northwest Mexico and the southwest United States during the North American monsoon. They have been shown to modulate precipitation and have been linked to severe weather and flooding in northern Mexico and the southwest United States. The general features and progression of surge events are well documented but their detailed dynamical evolution is still unclear. In this study, a convection-permitting simulation is performed over the core monsoon region for the 12-14 July 2004 gulf surge event and the dynamics of the simulated surge are examined. Initially, convection associated with the tropical easterly wave precursor to Tropical Cyclone Blas creates a disturbance in the southern GoC on early 12 July. This disturbance is a precursor to the gulf surge on 13 July and is a Kelvin shock (internal bore under the influence of rotation) that dissipates in the central GoC. The surge initiates from inflow from the mouth of the GoC along with convective outflow impinging on the southern GoC. Continued convective outflow along the GoC generates multiple gravity currents and internal bores while intensifying the simulated surge as it propagates up the GoC. As the core of the surge reaches the northern GoC, a Kelvin shock is again the best dynamical fit to the phenomenon. Substantial low-level cooling and moistening are associated with the modeled surge along the northern GoC as is observed.