Over the past 24 hours, New York City has experienced a gradual increase in temperature, which peaked in the late afternoon before starting to decline slightly, indicative of typical diurnal variation. Humidity levels were high throughout most of the period, with a noticeable drop during the time when temperatures were at their highest, suggesting an inverse relationship between temperature and humidity. Air pressure remained relatively stable with minor fluctuations, indicating no significant weather fronts moving through the area during the observed time. Wind speeds varied, with a period of calm and a few instances of moderate breeze; however, the overall wind conditions were light. The wind direction shifted throughout the day, primarily coming from the south and west, which could have contributed to the variations in temperature and humidity.