uneven heating causes certain areas of the atmosphere to be warmer than others and variations in volume and pressure that result in an upward current of air.
Temperature and pressure variances result from uneven heating of the earth's surface. Higher air pressure results from heavier air at lower temperatures. Where the wind is coming from is used to describe wind direction. For instance, a northerly breeze moves southward from north to north.
Convection is usually brought up while addressing the uneven heating of the Earth's surface. As a result of the uneven heating, certain areas of the atmosphere become warmer than others, and variations in volume and pressure lead to updrafts, which can result in thunderstorms and other severe weather.
This is caused by the Earth's surface's albedo, or degree of reflection, and the angle at which the sun's rays hit it. A field coated in snow and ice will reflect light far more than an asphalt parking lot. As a result, the parking lot receives substantially more shortwave solar energy and warms up considerably.
Solar heating of the Earth's surface is uneven because land heats faster than water, and this causes air to warm, expand and rise over land while it cools and sinks over the cooler water surfaces.
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