Over the past 24 hours, New York City has experienced a slight decrease in temperatures followed by a gradual increase, indicative of a typical diurnal temperature variation. Humidity levels have shown fluctuations, with a general decrease during the afternoon hours, which is common due to increased temperatures lowering relative humidity. Air pressure readings displayed a significant spike, suggesting the likely presence of a transient high-pressure system which could lead to stable and clearer weather conditions. Wind speeds were mostly light to moderate, with no pronounced sustained periods of high winds, pointing to relatively calm weather conditions. The wind direction varied throughout the day but predominantly came from the west, with occasional shifts which could have influenced localized weather patterns.