| 21. | Deep convection increased as it reached open waters, with trough.
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| 22. | It began to convection and eventually degenerated by the next day.
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| 23. | Deep convection was flaring around the low-level circulation center.
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| 24. | Deep convection rapidly dissipated shortly thereafter due to interaction with land.
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| 25. | Convection soon redeveloped as the storm moved northwestward through warm waters.
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| 26. | Later that day, the depression began to regain deep convection.
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| 27. | Usually, convection occurs as a result of the diffusion process.
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| 28. | Convection currents are the cause of almost all weather on Earth.
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| 29. | As a result, the eye dissipated and the convection weakened.
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| 30. | Low wind shear allowed the convection to sustain around the eyewall.
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