An application of NOAA AVHRR thermal data to the study of urban heat islands

Hyoun-Young Lee
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引用次数: 83

Abstract

Brightness temperatures were derived from the Advanced Very High Resolution Radiometer (AVHRR) at channel 4 (10.5–11.5 μm) on the NOAA-9 and NOAA-10 satellites to examine the applicability of the AVHRR thermal data to the study of urban heat islands. Air and ground surface temperatures measured at meteorological stations in large cities (population over 300,000) in South Korea were compared with in situ brightness temperature data.

The correlation coefficient between air temperatures and brightness temperatures is 0.85 and the relationship may be expressed by the regression: AT=0.59 BT + 2.54. This equation explains 73% of variances at the 0.02% significance level. The best-fit line, however, underestimates air temperatures in such heat-processing industrial cities as Ulsan and Pohang, where smoke puffs up from the high stacks of industrial plants, and overestimates them in the Seoul metropolitan area. The regression equation of ground surface temperatures on brightness temperatures explains 72% of variances. Assuming that optimal meteorological conditions can be selected, the regression equation can be used as a tool to assess air temperature fields in cities.

Urban land-use, such as built-up, residential and industrial areas, was clearly identified from the AVHRR thermal data, while small-scale land-use, like parks, were not distinguishable. Brightness temperatures for the intensity of heat islands were related to the population size of cities. The areal magnitude of heat islands in the Seoul metropolitan area expanded considerably, reflecting the conurbation trend for the period 1986–1989. Urban temperatures in the area increased during the period, while temperature gradients declined.

NOAA AVHRR热数据在城市热岛研究中的应用
利用NOAA-9和NOAA-10卫星上先进甚高分辨率辐射计(AVHRR) 4通道(10.5 ~ 11.5 μm)的亮度温度数据,验证AVHRR热数据在城市热岛研究中的适用性。在韩国大城市(人口超过30万)的气象站测量的空气和地面温度与现场亮度温度数据进行了比较。气温与亮温的相关系数为0.85,可以用回归表示为AT=0.59 BT + 2.54。这个方程解释了0.02%显著性水平下73%的方差。然而,最合适的线低估了蔚山和浦项等高温加工工业城市的气温,这些城市的浓烟从工业厂房的高烟囱中冒出来,而在首都圈则高估了气温。地表温度对亮温的回归方程解释了72%的方差。在选取最优气象条件的前提下,回归方程可作为评价城市气温场的工具。从AVHRR热数据中可以清楚地识别城市土地利用,如建成区、住宅区和工业区,而小规模土地利用,如公园,则无法区分。热岛强度的亮温与城市人口规模有关。首都圈的热岛面积显著扩大,反映了1986-1989年期间的都市化趋势。在此期间,该地区的城市温度升高,而温度梯度下降。
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