Pressure is provided in mbar and the gas constant is in Jmol-1K-1. The above equation cannot be generalized because units cannot be converted.
Density=Pressure/gas constant* temperature. Since both examples have the same pressure (1018.6 mb), only the temperature varies. Temperature affects density. Lower temperatures increase density and vice versa. Since the station north of New Orleans has 66°F cooler air than New Orleans, its air density is higher.
This is further explained below.
<h3>How must the sea level air density in new Orleans differ from the station directly north near the other surface high-pressure center?</h3>
Since the gas constant is provided in Jmol-1K-1 and the pressure is given in mbar, the unit is different. The above equation cannot be generalized because the unit cannot be converted.
In conclusion, we are aware that density is equal to pressure times gas constant temperature. Since the only variable remaining is temperature, the pressure in both scenarios is the same (1018.6 mb).
The temperature will have an inverse relationship with density. The density will be greater at lower temperatures and vice versa. Since the station just north of New Orleans has a temperature that is 66 degrees Fahrenheit lower than the city's high pressure, it follows that the station's air density is higher than that of New Orleans.
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