Using the OKCNET observations, a detailed analysis was conducted on an intense heat wave that produced record temperatures over 40oC in central Oklahoma during July and August 2008. In Oklahoma City, a consistent urban heat island (UHI) was present throughout the diurnal cycle with mean magnitudes of approximately 1oC during the day and over 2oC at night. Further, while the rural areas cooled to minimum low temperature values spanning 22-26oC, the low temperature values were often significantly warmer (26-29oC) in the urban zones. However, due to the increased warmth near the urban core due to the UHI along with sufficient humidity, heat index values were also typically greater than (a) the rural conditions and (b) the temperature values alone. In some cases, the urban heat index values were as much as 2.5oC warmer than the actual temperatures yielding apparent temperature values at night that were nearly 5oC warmer than the surrounding rural areas.
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