Gradient winds refer to the flow of air in response to the pressure gradient force which is the difference in pressure between two points. Synonyms for gradient winds include pressure gradient winds, baroclinic winds, or geostrophic winds. These winds are created when the atmosphere attempts to balance the pressures across different regions. Wind speed increases as the pressure gradient force increases, and the direction of winds is generally from areas of high pressure to areas of low pressure. Understanding gradient winds is critical for predicting weather patterns and tracking storms. The study of gradient winds and other wind patterns is critical for meteorology and climatology.