The Structure and Evolution of Gap Outflow over the Gulf of Tehuantepec, Mexico

@article{Steenburgh1998TheSA,
  title={The Structure and Evolution of Gap Outflow over the Gulf of Tehuantepec, Mexico},
  author={W. J. Steenburgh and D. Schultz and B. Colle},
  journal={Monthly Weather Review},
  year={1998},
  volume={126},
  pages={2673-2691}
}
Abstract Mesoscale-model simulations are used to examine the structure and dynamics of a gap-outflow event over the Gulf of Tehuantepec, Mexico, that was associated with a surge of cold air along the eastern slopes of the Sierra Madre. The simulated gap-outflow winds emerged from Chivela Pass, reached a maximum speed of 25 m s−1, and turned anticyclonically as they fanned out over the gulf. Northerly winds were also able to ascend the mountains east, and to a lesser extent west, of Chivela Pass… Expand
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