Over the last 24 hours in New York City, temperatures have exhibited a typical diurnal pattern, cooling during the early hours before gradually warming up by the afternoon. The humidity levels have fluctuated but showed a significant increase in the last hour, which could be indicative of incoming moisture or a weather front. Air pressure has been relatively stable, with a notable rise in the later hours, suggesting a high-pressure system may be moving into the area, which is often associated with clearer skies. Wind speeds have varied, with a couple of peaks that could have contributed to a wind chill effect, making the air feel cooler than the actual temperature. Finally, the wind direction has been predominantly from the north to northeast, which is typical for cooler and drier air masses in the region.