Which storm trajectory results when differential solar heating and the Coriolis effect intensify?

💡 Explanation

Deepening mid-latitude cyclones develop because intensified heating amplifies pressure gradients, which enhances the Coriolis effect, leading to stronger cyclonic rotation centered at low pressure; therefore, a more intense cyclone forms, rather than the other weather phenomena.

• Which outcome occurs when freshwater influx disrupts circulation?
• Which consequence results when localized sticking halts transform fault creep?
• Which risk increases where a large, locked fault experiences episodic tremor and slip (ETS)?
• Which outcome occurs when differential slip exceeds friction limits on strike-slip faults traversing sedimentary strata?
• Which risk increases when surface ocean gyre strength lessens?
• Which landscape outcome results when groundwater flows along limestone fractures?