Urban heat pockets are localized areas within cities that experience significantly higher temperatures compared to their surrounding areas. This phenomenon is especially noticeable in densely populated urban centers like New York City, where the combination of human activities, infrastructure, and limited vegetation contributes to elevated temperatures. Several factors exacerbate the urban heat island effect in New York City, including dense building materials like concrete and asphalt, which absorb and retain heat. The scarcity of green spaces reduces the cooling effect of evapotranspiration, while high energy consumption from buildings and transportation generates additional heat. Recent reports also indicate that the city's infrastructure and business activities significantly contribute to localized temperature increases.