Over the last 24 hours, New York City has experienced a gradual increase in temperature, peaking during the late afternoon hours which is typical for the diurnal cycle. Humidity levels showed a decreasing trend as temperatures reached their peak, suggesting an inverse relationship between temperature and humidity during this period, a pattern that is not uncommon. Atmospheric pressure remained relatively stable, with only minor fluctuations, indicating no significant weather fronts moving through the area during this time. Wind speeds were mostly light to gentle with some variability, and there was a notable shift in wind direction from predominantly westerly to northerly and variable by the end of the period. These conditions are consistent with fair weather, but the low humidity and higher temperatures may increase discomfort for some individuals, especially during the warmest part of the day.