Specific Heat The amount of heat required to raise the temperature of 1g of a substance by one degree Celsius *The higher the specific heat, the slower the heating AND cooling of a substance (“more stubborn”)*

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Sea Breeze During the day, land heats quicker than water - Warm air over land rises - Rising air cools (and may condense) - Cooled air moves back over ocean and sinks Ocean is cooler compared to land (cold source, aka heat sink)

Land Breeze During the night, land cools quicker than water - Warm air over water rises - Rising air cools (and may condense) - Cooled air moves back over land and sinks

Monsoons Seasonal wind changes Summer monsoon  land warmer so wind blows toward land Winter monsoon  ocean warmer so wind blows toward the ocean