What can be inferred when isobars are closely packed?

When isobars are closely packed on a weather map, it indicates a significant pressure gradient between adjacent areas. This steep gradient creates a stronger force that acts on the air, leading to higher wind speeds. In essence, the closer the isobars, the faster the air will move from high-pressure areas to low-pressure areas in an effort to balance the pressure differences.

The presence of closely spaced isobars typically signals an active weather pattern with more intense wind conditions, which is why the assertion of strong winds is correct. Understanding this relationship between isobar spacing and wind speed is crucial for interpreting meteorological data.