| 1. | Strong wind shear and decreasing sea surface temperatures significantly weakened the storm.
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| 2. | Aided by warm sea surface temperatures of, Bella began to intensify quickly.
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| 3. | Sea surface temperatures can surge as much as 14 degrees above normal.
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| 4. | During upwelling events, local sea surface temperature drops by 2-3 degrees Celsius.
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| 5. | Early on September 22, an atmospheric divergence and highly sustainable sea surface temperatures.
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| 6. | Sea surface temperatures in the region averaged, supportive of tropical development.
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| 7. | Concurrently a strengthening outflow, and warm sea surface temperatures allowed for the intensification.
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| 8. | Sea surface temperature anomalies in November 2007 showing La Ni�a conditions.
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| 9. | Due to warm sea surface temperatures Very Severe Cyclone Vardah formed in December.
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| 10. | These features can easily be identified from Sea Surface Temperature and Chlorophyll data.
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