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An anomalous low level trough as a part of an anomalous wave train from the Ural-Siberia regisn iseenen anchored to the Indian latitudes by the anomalous Matsuno-Gill response to the anomalous equatorial tropical convection from 2 days before the start of the event and is seen persisting throughout the life of the cold wave.
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A weak low-level trough extended from the Caribbean Sea to south of Mexico, disrupting the normal flow of westward steering currents.
A low-level trough and a cluster of convection associated with a tropical wave interacted in the Gulf of Mexico in early September 2000.
A broad low-level trough approached the storm from the northwest, pulling the convection northward as the storm's low-level center accelerated eastward.
The wave drifted westward, and after several days began to interact with a low-level trough near the Gulf of Tehuantepec, and as a result deep convection increased.
Around the same time, a low-level trough emerged from the Intertropical Convergence Zone, heading north off the coast of Nicaragua.
As Beti intensified into a severe tropical cyclone, the ridge of high pressure weakened as it interacted with an upper level trough of low pressure.
While most of the mid to upper level moisture associated with the storm got pulled inland by a shortwave trough, the low level center dissipated in the northern Gulf on August 27.
Since the monsoon trough is an area of convergence in the wind pattern, and an elongated area of low pressure at the surface, the trough focuses low level moisture and is defined by one or more elongated bands of thunderstorms when viewing satellite imagery.
Thereafter, the strength of the storm diminishes as the cyclone couples with the upper level trough or upper level low, becoming increasingly cold core.
Originating in the monsoon trough in the South China Sea in early August, a low level circulation was first spotted about 370 km east of Vietnam on August 8.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com