Over the past 24 hours, New York City experienced a gradual rise in temperature through the day, reaching its peak in the late afternoon before a slight decline towards the evening. The humidity showed significant variations, with notably higher levels during the early morning hours, indicating the possibility of morning fog or dew, which then decreased as temperatures rose. Air pressure remained relatively stable, with a slight decreasing trend towards the end of the period, which could suggest an approaching weather system. Wind speeds varied, but there was an increase in the evening, which could have contributed to a wind chill effect, making the air feel cooler than the actual temperature. The prevailing wind direction was predominantly from the southwest, shifting slightly throughout the day, which is typical for the region and could influence coastal and inland weather patterns.