Over the past 24 hours in New York City, the temperature has exhibited a gradual increase, reaching a peak in the late afternoon before starting to decline in the evening. Humidity levels started at saturation but showed a significant decrease during the day, suggesting the dissipation of morning fog or rain and the development of drier conditions. Air pressure remained relatively stable with only minor fluctuations, indicating no significant frontal systems passing through the area. Wind speeds varied, with some periods of calm and others of moderate speed, peaking in the evening, which could have contributed to a wind chill effect making it feel cooler than the actual temperature. Finally, wind direction was predominantly westerly, with some variability, which is typical for New York City's weather patterns and can influence the distribution of air masses and moisture.