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The urban heat island of San Antonio, Texas (USA)

机译:美国德克萨斯州圣安东尼奥市的城市热岛

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A study of the urban heat island effect was carried out comparing 45-year daily temperature records (1946-1990) of San Antonio, Texas (USA), with three small surrounding towns; New Braunfels, Poteet, and Boerne, These towns are all within 40 kilometers of San Antonio and were chosen because they form a nearly equilateral triangle around the city from northeast to south to northwest, respectively. The study shows that, on average, the minimum temperatures at the San Antonio International Airport (the location of the weather station) are increasing at an average rate of about 0.3℃ per decade relative to surrounding small towns with similar elevation. The difference in minimum temperatures is most pronounced during the summer months. The summer temperature minimum differences relative to New Braunfels indicated the largest increase at 0.4 +- 0.1℃ per decade and an increase of 0.2 +- 0.1℃ per decade relative to Poteet. In 1947, the minimum temperatures in New Braunfels were on average about 0.2℃ warmer than San Antonio and they were about equal between San Antonio and Poteet. In 1990, summer minimum temperatures were more than 1.7℃ cooler in New Braunfels and more than 1.0℃ cooler in Poteet. A similar trend in the minimum summer temperatures is seen in comparisons with Boerne but the magnitudes are smaller and there are larger temperature fluctuations in the data. This may be due to the higher elevation of Boerne (about 700 meters above sea level) whereas San Antonio, New Braunfels, and Poteet all have similar elevations (about 200 meters above sea level). The same effects are found in the maximum temperatures in the winter months for New Braunfels and Poteet. They are increasing at average rates of about 0.8℃ per decade compared to New Braunfels and 0.5℃ per decade compared to Poteet in the winter months. No statistical change in the winter maximum temperatures between San Antonio and Boerne was found. Despite many mitigating influences (e.g., much vegetation, little polluting industry), it has been shown that San Antonio has an increasing urban heat island effect.
机译:对城市热岛效应进行了研究,将美国得克萨斯州圣安东尼奥的45年每日温度记录(1946-1990年)与周围的三个小城镇进行了比较。这些城镇均位于圣安东尼奥市40公里之内,之所以选择这些城镇,是因为它们分别从东北到南到西北形成一个几乎等边的三角形。研究表明,相对于周围海拔相似的小城镇,平均而言,圣安东尼奥国际机场(气象站的位置)的最低温度以每十年约0.3℃的平均速度增长。在夏季,最低温度的差异最为明显。相对于新布朗费尔斯,夏季温度的最小差异表明,每十年增加0.4 +-0.1℃,而相对于Poteet,则增加每十年0.2 +-0.1℃。 1947年,新布朗费尔斯的最低温度比圣安东尼奥平均高0.2度左右,并且在圣安东尼奥和波特特之间大约相等。 1990年,新布朗费尔斯的夏季最低温度降低了1.7℃以上,而波特镇的最低温度降低了1.0℃以上。与Boerne相比,夏季最低温度有相似的趋势,但幅度较小,数据中的温度波动较大。这可能是由于Boerne海拔较高(海拔约700米),而San Antonio,New Braunfels和Poteet的海拔都相似(海拔约200米)。在新布朗费尔斯和波特的冬季最高温度中也发现了相同的影响。与新布朗费尔相比,它们每十年的平均增长率为0.8℃,而与冬季波特相比,则每十年的平均增长率为0.5℃。没有发现圣安东尼奥和博恩之间的冬季最高温度的统计变化。尽管有许多减轻影响的措施(例如植被多,污染少的工业),但已证明圣安东尼奥的城市热岛效应正在增加。

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