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Advances in Meteorology
Volume 2014 (2014), Article ID 620410, 12 pages
Validation of ASTER Surface Temperature Data with In Situ Measurements to Evaluate Heat Islands in Complex Urban Areas
Department of Environmental Engineering, Changwon National University, 20 Changwondaehak-ro Uichang-gu Changwon-si, Gyeongsangnam-do 641-773, Republic of Korea
Received 27 August 2013; Accepted 6 December 2013; Published 20 January 2014
Academic Editor: Yuriy Kuleshov
Copyright © 2014 Bonggeun Song and Kyunghun Park. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
This study compared Advanced Spaceborne Thermal Emission Reflection Radiometer (ASTER) surface temperature data with in situ measurements to validate the use of ASTER data for studying heat islands in urban settings with complex spatial characteristics. Eight sites in Changwon, Korea, were selected for analyses. Surface temperature data were extracted from the thermal infrared (TIR) band of ASTER on four dates during the summer and fall of 2012, and corresponding in situ measurements of temperature were also collected. Comparisons showed that ASTER derived temperatures were generally 4.27°C lower than temperatures collected by in situ measurements during the daytime, except on cloudy days. However, ASTER temperatures were higher by 2.23–2.69°C on two dates during the nighttime. Temperature differences between a city park and a paved area were insignificant. Differences between ASTER derived temperatures and onsite measurements are caused by a variety of factors including the application of emissivity values that do not consider the complex spatial characteristics of urban areas. Therefore, to improve the accuracy of surface temperatures extracted from infrared satellite imagery, we propose a revised model whereby temperature data is obtained from ASTER and emissivity values for various land covers are extracted based on in situ measurements.
Cities all over the world are experiencing more common urban heat islands (UHIs), whereby urban settlements are hotter than rural areas because of the rapid increase in artificial land cover such as asphalt [1–4]. Urban heat islands can generate tropical nighttime conditions and exacerbate heat waves, which negatively affects the health and welfare of urban residents [5–8]. Moreover, temperature increases from UHIs greatly increase energy consumption from the use of coolers [9, 10] and the aggregated effects from UHIs can cause changes in urban ecosystems . The problems associated with UHIs are expected to worsen with global warming and UHIs are rapidly expanding into a global environmental issue of concern [12–14].
To alleviate adverse effects from UHIs, a wide range of studies have been performed using data on land surface temperatures (LSTs) extracted from remotely sensed thermal infrared data [15–18]. Surface temperature data derived from satellite images can be used to assess characteristics of UHIs such as how temperatures vary across the canopy layer of roofs and other surface features [19–23] or how temperatures are related to the surface energy balance [24–28]. In addition, satellite images of surface temperature data can supplement in situ temperature measurements collected by meteorological networks. Thus, satellite data can be used to analyze the general features of atmospheric UHIs in urban areas [29, 30].
To use satellite image-based surface temperature data for heat island studies in urban areas with complex spatial characteristics, important factors that influence surface temperatures must be considered comprehensively [31, 32]; these factors include the coverage texture type, the color of the surface layer, sky view factors, street geometry, traffic loads, and other anthropogenic activities. It is also important to validate the accuracy of satellite image surface temperature data by comparing it to in situ surface temperature data. Such analyses are necessary to diagnose UHIs more accurately and prepare appropriate relief plans.
Several recent studies have been conducted to validate or improve the accuracy of satellite temperature measurements by comparing satellite image surface temperature data to temperatures measured onsite. Mihalcea et al.  compared surface temperatures from onsite measurements and Advanced Spaceborne Thermal Emission Reflection Radiometer (ASTER) video images according to supraglacial debris coating and depth. Rigo et al.  validated the effectiveness of thermal infrared satellite images by comparing the earth radiation energy extracted from the images to data collected from eight fixed weather stations that were installed in urban, suburban, and rural areas of Basel, Switzerland. Nichol et al.  attempted to investigate UHIs and validate the accuracy of ASTER image surface temperature data by measuring surface temperatures at 18 sites located throughout the urban region of Kowloon in Hong Kong and the nonurban area of the New Territories in Hong Kong. In Scottsdale, Arizona, which is located in the Phoenix Metropolitan Area, Hartz et al.  classified land cover into asphalt, concrete, roof, and plant life and measured the surface temperature of each material using a thermal infrared camera. Then, the results were compared to surface temperatures derived from ASTER video images. All of these studies found that satellite temperature data were useful as surrogate measures for in situ temperature data.
Nonetheless, most relevant studies to date that compare in situ temperature data to satellite-based measurements are limited to homogeneous areas or rural areas. In addition, studies that have analyzed UHIs in urban areas with complex spatial characteristics are limited by their use of low resolution satellite images. Therefore, this study aimed to validate the accuracy of satellite image surface temperature data in an urban area through comparisons of relatively high resolution ASTER video data to onsite temperature measurements. Analyses were conducted in the urban area of Changwon, Gyeongsangnam-do, Korea, which is going through rapid urbanization and has various land use and coverage characteristics. Additionally, we evaluated and compared temperature measurements collected during the day and the night because thermal characteristics can vary diurnally.
2. Materials and Methods
2.1. Experiment Site
The urban area of Changwon, Gyeongsangnam-do, Korea (35°14′01.02′′N, 128°41′19.95′′E), has a population of approximately 500,000 people. The area is 125.91 km2 wide, and it is located in a basin surrounded by mountains that are approximately 600 m in height. The city, in which residential, commercial, and business areas are concentrated, contains a large floating population (i.e., nonresidential population) and dense traffic. Its annual average temperature is 15°C, and the annual precipitation is 1,396 mm .
The experiment site was established as the first planned city in Korea . The site contains clear divisions of residential, commercial, and industrial quarters. It is composed of various structural patterns and coverage materials such as asphalt, concrete, greenery, sidewalk bricks, and tiles. In this study, we selected a total of eight sites for analyses, including a university campus, an urban park, a commercial area, low-rise apartments, high-rise apartments, a single residential area, an open lawn square of homogeneous coverage material, and a sidewalk brick square (Figure 1). These sites were selected because of their diverse land use and coverage characteristics, and in situ measurements at these sites were compared to data from satellite images.
2.2. Setup of GIS Data and Satellite Imagery
2.2.1. ASTER Video Data
Satellite image-based surface temperature data were extracted using the Level 2B03 Product (surface kinetic temperature) from the thermal infrared (TIR) band of ASTER. The ASTER instrument, located onboard the Terra satellite, is composed of three sensors: SWIR (short wave infrared), VNIR (visible near infrared), and TIR (thermal infrared). It also has 14 spectrum channels to analyze radiance. Among them, the TIR generates products between channels 10 and 14 (8.15–11.65 μm) . The spatial resolution of the ASTER 2B03 product is 90 m, and it is used to generate data for the Temperature Emissivity Separation (TES) algorithm used for determining the emissivity of land coverage values [36, 40].
This study collected four ASTER video images on almost cloudless, sunny days between June and September 2012. In particular, the acquisition times were at 02:10 pm UTC on July 28, 2012 (daytime), 01:31 am UTC on September 21, 2012 (nighttime), 02:16 pm UTC on September 23, 2012 (daytime), and 01:37 am UTC on September 28, 2012 (nighttime). Surface temperatures were extracted after geometric corrections and coordinate transformations had been performed using the Geodetic Reference System (GRS) 80 equipped with PG-STEAMER version 4.2 (Pixoneer Corp.) software, an image processing program.
2.2.2. Urban Characteristics Data
Surface fabric classification of the eight subject areas was performed through onsite investigations and the use of 10 cm high spatial resolution aerial photograph orthoimagery and land coverage maps from the Changwon Environment Atlas. The land coverage maps in the Changwon Environment Atlas are composed of very detailed GIS spatial data that contain 31 coverage properties such as structures, asphalt, concrete, trees, and bare lands at a 1 : 1,000 scale . The reserve surface fabrics were selected after considering the unclassified fabrics based on the land coverage maps. A total of 21 surface fabrics, identifiable on the maps when compared to the aerial photograph, were ultimately selected.
Temperatures may vary in areas with the same surface fabric because trees and buildings will form shadows during the daytime that alter the amount of radiant energy flowing into the surface . Thus, shaded areas during the daytime of July 28th and September 23rd were classified as surface fabrics and reflected in the analyses. Analyses were performed through use of the Hillshade function of the ArcGIS 9.3 program using digital terrain models (DTM) extracted from light interferometry detection and ranging (LiDAR) images with a 1 m spatial resolution. The input variables of sun altitude and azimuth were matched to the times of the video collection. The values used were as follows: 63°52′51.60′′ and 188°31′40.10′′ for the July 28 and 44°17′04.40′′ and 220°47′57.60′′ for the September 23. Because the inflow of radiant energy was blocked in shaded areas, the surface temperatures in these regions were almost equivalent to air temperatures; hence, site temperatures measurements were substituted as surface temperatures at some locations .
2.3. In Situ Measurement Data and Methods
2.3.1. Measurements of Surface Temperature and Weather Variables
By considering the composition ratio of the surface fabric and measurement times at each subject site, a total of 366 points were chosen from the 8 sites for analyses (78 places in the university campus, 64 in the park, 53 in the low-rise apartments, 63 in the commercial area, 41 in the single residential area, 55 in the high-rise apartments, 6 from the lawn square, and 6 from the sidewalk bricks) (Figure 2). Onsite measurements were carried out for approximately an hour at each site (daytime: 14:00 - 15:00 and nighttime: 01:00 - 02:00). The measurements were collected so that the data would span 30 minutes before and after the time in which the satellite took pictures.
Temperatures were measured using thermal infrared thermometers that were held 10 cm vertically off the surface. A portable Kestrel 4500 Weather Meter was also used to measure weather related variables such as temperature, relative humidity, and wind speed at each measuring point (air temperature accuracy: ±1.0°C, wind speed accuracy: ±3%, and relative humidity (RH) accuracy: ±3%).
To account for changes in the surface temperature according to the elapsed site measurement time, we attempted to perform a correction through the use of linear regression techniques. However, the temperature differences over time were below 0.5°C; hence, the data were not corrected for time differences. Furthermore, we were limited in our ability to perform measurements on top of single residential buildings; hence, roof temperatures in these areas were measured using thermal imaging cameras (temperature accuracy: ±2°C) from the roofs of nearby high-rise business buildings.
2.3.2. Emissivity Calculation Method
Emissivity refers to the ability of a surface fabric to absorb, transmit, and reflect external radiant energy. Emissivity values are rated against a black body, which theoretically will only absorb energy without reflecting it .
Surface temperature data extracted from the satellite image represents radiant temperature, which is the temperature conversion of radiant energy released from the surface, and it is closely related to the emissivity for surface fabrics [33, 45]. Valor and Caselles  and Caselles et al.  stated, “retrieval of LST from TIR data requires an accurate measurement of emissivity values of the surface.” Therefore, it is necessary to compare it to actual measurements of emissivity from various surface fabrics of the urban area.
Emissivity was calculated using the Stefan-Boltzmann law as follows:
Here, is the emissivity of fabric , is the earth radiant energy of fabric measured by the CNR4 net-radiometer, is the set emissivity of the thermal infrared thermometer (0.95), is the surface temperature of the fabric using a thermal infrared thermometer, and is the Stefan-Boltzmann constant (5.67 × 10−8 W m-2 K−4).
Emissivity for each surface fabric was calculated after measuring the surface temperature and radiant energy of the 21 surface fabrics classified in the city characteristic data (Table 2). Radiant energy was measured using a CNR4 net-radiometer (Kipp and Zonen Inc.) by holding it horizontally approximately 10 cm away from the surface for a minute to two. The surface temperature was measured by holding a thermal infrared thermometer (Testo 381 model, accuracy: ±1.5°C, emissivity: 0.95) 10 cm perpendicular to the surface.
Measurements were performed during 10:00 to 16:00 on three days, May 27, June 5, and June 24, which consisted of clear weather. Measurement points were selected with the composition ratio of surface fabric per subject area in mind and measurements were collected in spots that were as homogeneous as possible (i.e., not mixed with other fabric types).
2.4. Comparison Method for ASTER and In Situ Measurements of Surface Temperature
Direct comparisons between the surface temperatures of satellite derived pixel images and geographically identical pixel locations were performed for ASTER image data and onsite measurements. To do so, the entire field measurement site was divided into Vector GRIDs of 90 m × 90 m, which was identical to the spatial resolution of the ASTER image (Figure 3).
For the field measured surface temperatures, the mean surface temperature of each GRID was calculated after analyzing the area ratio per surface fabric per GRID according to the following equation:
Here, is the mean surface temperature per GRID, is the emissivity of fabric , is the surface temperature of fabric , and is the area ratio of the fabric .
The mean surface temperature calculated for each GRID was compared to the surface temperature of the exact location on the ASTER image. The difference in the surface temperature between the satellite image and the field measurement was contemplated in connection with the spatial characteristics of the subject area and the pixels.
3. Results and Discussion
3.1. Spatial Patterns of ASTER Surface Temperature
Figure 4 shows the surface temperature results that were extracted from the ASTER images. Surface temperature was high during the day mostly in places covered with concrete and asphalt. Although the commercial area, low-rise apartments, and high-rise apartments had higher surface temperatures during the night compared to the daytime, the differences were insignificant. According to the image taken on July 28, portions of the commercial area, high-rise apartments, and single residential area had low surface temperatures due to the influence of clouds.
Among the mean surface temperatures at each of the 8 sites, the block square (07/28: 44.3°C, 09/23: 33.2°C) had the highest temperature during the day, and the commercial area (09/21: 19.4°C, 09/28: 19.0°C) and the high-rise apartments (09/21: 18.7°C, 09/28: 19.2°C) had the highest temperatures during the night (Table 3).
3.2. Classification of Surface Fabric and Shaded Areas per Location
Figure 5 shows the classification of surface fabric. The university campus was mostly composed of asphalt, sidewalk bricks, trees, and grass. Low-rise apartments and commercial areas were mostly composed of concrete on the building roofs (grey) and asphalt. Single residential areas had a high amount of asphalt and tiled roofs of various colors. High-rise apartments were composed of various fabrics such as asphalt, concrete (grey) sidewalk bricks, trees, grass, and tile. Asphalt was common in the areas around homogeneous lawn squares and sidewalk brick plazas.
Analyses of the shaded areas created by buildings and other structures were limited to the date the satellite photography and field measurements took place. As the altitude of the sun was higher and the azimuth was smaller on July 28 than on September 23, the amount of shaded area was smaller. The commercial area and the high-rise apartment area, which were packed with tall buildings, had a high percentage of shaded areas (Figure 6), while the lawn square area was the least affected by the shade because of its location in an open space (Table 1).
3.3. Emissivity and Surface Temperature by Field Measurements
Of the 21 types of surface fabrics, water and tile had the highest emissivity of 1.00, while the green roof system had the lowest at 0.93, according to measurement results of the emissivity per surface fabric (Table 2). The results of Sobrino et al.  demonstrated an emissivity of 0.985 for water surfaces, 0.990 for trees, 0.914 for concrete, 0.965 for asphalt, 0.902 for sidewalk bricks, 0.898 for bright bare soil, 0.970 for dark bare soil, and 0.897 for rooftops. These values were obtained by mapping emissivity per land coverage with ASTER images, and the values were somewhat different from those that were obtained during measurements in this study. Emissivity was especially different for artificial surface textures such as concrete, sidewalk bricks, and rooftops.
Field measurements of surface temperatures showed that temperatures were higher on September 23 than on July 28 by approximately 10°C on average. Wooden boards had the highest surface temperature (07/28: 69.0°C, 09/23: 52.2°C), followed by urethane (07/28: 66.2°C, 09/23: 49.3°C). Water had the lowest surface temperature (07/28: 27.0°C, 09/23: 21.4°C). More open areas such as sidewalk brick squares (07/28: 62.0°C, 09/23: 46.2°C) and lawn squares (07/28: 43.5°C, 09/23: 33.0°C) had higher surface temperatures than areas that were not open spatially (Table 2). This was likely caused by more continuous short wave radiation flowing into open areas.
Nighttime measurements showed little differences in surface temperatures between the different surface fabrics. In general, however, artificial fabrics such as asphalt (09/21: 19.6°C, 09/28: 18.7°C), concrete (09/21: 19.7°C, 09/28: 18.8°C), and granite (09/21: 21.4°C, 09/28: 19.3°C) had relatively higher surface temperatures. Extraordinarily, wooden boards, which had the highest surface temperature during the day, had the lowest temperature during the night (09/21: 12.1°C, 09/28: 12.2°C) and water surfaces, which had the lowest temperature during the day, had the highest temperature during the night (09/21: 17.3°C, 09/28: 19.9°C) (Table 2). This is because water has a large heat capacity. Thus, when water is subjected to external heat energy, the temperature rises and falls slowly and it can be relatively high during the night [48, 49]. Open areas such as lawn squares (09/21: 12.8°C, 09/28: 12.3°C) had lower surface temperatures than lawns that were not as open (09/21: 13.4°C, 09/28: 14.6°C). This is because more compact spaces release less terrestrial radiation energy from the earth to the atmosphere, which leads to a greater aggregation of energy at the surface [18, 50]. Temperatures reached 35.8°C on July 28, 20.2°C on September 21, 27.7°C on September 23, and 20.7°C on September 28.
Surface temperatures calculated for each GRID using field measurement data showed that sidewalk brick squares had the highest surface temperature during daytime (07/28: 51.0°C, 09/23: 38.2°C), and this was also demonstrated in the ASTER image. Although high-rise apartments had high amounts of asphalt, which typically have a high surface temperature, these areas had relatively low surface temperatures because they were affected by shade (07/28: 32.5%, 09/23: 44.3%) (Table 1). The highest nighttime surface temperatures were measured in situ in the commercial area (17.3°C) on September 21 and the sidewalk brick square area (16.9°C) on September 28. In contrast, lawn squares had the lowest nighttime surface temperatures (09/21: 14.3°C, 09/28: 13.9°C) (Table 3).
3.4. Comparisons of ASTER Image and Field Measured Surface Temperatures
Figure 7 shows a graph of the surface temperature difference between the field-based measurements and the satellite-based measurements for each pixel of the subject sites. Surface temperatures derived from ASTER images differed greatly from those measured onsite (between 20 and 30°C) in the commercial area and parts of the high-rise apartment area on July 28 because of the influence of clouds. Hence, the root mean square error (RMSE) was relatively high in these areas and it amounted to 10.73°C. Satellite image surface temperatures of the water area in the park were 7.8°C higher than field measured temperatures. Except for a clouded area, the single residential area showed large differences in temperature; in contrast, adjacent vegetation covered areas showed very little differences in temperature that only amounted to 0.8°C. In pixels composed of identical fabrics such as grass and sidewalk bricks, the differences were very small and amounted to 0.5°C and 0.4°C, respectively. The park area had some of the lowest differences in temperature according to the RMSE (Table 3).
The RMSE was 2.23°C on September 21. The vegetation area pixel, which had the least difference in the single residential area data from July 28, had the largest difference of 3.9°C on September 21. Pixels composed of identical grass fabric also demonstrated differences more than 5°C, and the differences were the greatest for the data from September 21. Subject areas with small temperature variances included the single residential area (1.6°C), the university campus (1.9°C), and the sidewalk brick square (1.9°C) (Table 3).
Similar patterns were observed on September 23 and July 28. Surface temperatures from the satellite images of water in the park were higher than the field-measured surface temperatures by 1.7°C. In the single residential area, the pixels with vegetation had the least difference (0.1°C). Interestingly, in the homogeneous lawn pixels and the vegetation pixels in the university campus, the surface temperatures from the satellite images were higher than the field measured temperatures. The university campus (3.2°C), low-rise apartment area (3.7°C), and the commercial area (3.8°C) had low RMSEs (Table 3).
On September 28th, similar to the nighttime of September 21st, the homogeneous lawn pixel had the greatest temperature differences range from 5.9°C to 6.4°C. In the single residential area, however, and unlike the data observed on September 21st, other pixels along with the vegetation pixels displayed large temperature differences. Homogeneous sidewalk bricks had the lowest RMSE of 1.1°C, followed by the university campus (1.6°C) (Table 3).
Therefore, as the results of the comparisons described above show, the temperature data derived from satellite images has accuracy problems that vary according to land coverage and land use in the urban area. First, higher building densities are associated with larger differences between satellite-based and field-based temperature measurements. According to an earlier study by Hartz et al. , areas with greater population have greater temperature differences between ASTER image measurements and field measurements of surface temperatures. Barring et al.  and Eliasson  discovered that more densely built up areas had greater surface temperature differences of about 4~8°C. Voogt and Oke  speculated that the limited horizontal surface view from ASTER was the cause of the discrepancy. Therefore, in a spatial structure with high density characteristics, the amount of radiation energy from the earth sensed by the satellite may be misjudged because of the limited horizontal surface view. For example, during the night denser areas (e.g., commercial areas, low-rise apartments, and high-rise apartments) had greater differences in temperature between satellite and field measurement data. This is believed to be because in areas packed with buildings, the radiation energy released from the earth into the atmosphere is blocked and aggregated in the earth [18, 50]; and because satellites cannot sense this, it causes differences. Moreover, denser areas had greater differences in surface temperatures for the satellite imagery between the walls of the buildings, and not the temperature of the surface, and field measurements due to the off-nadir angle (ASTER = 22.5°) of the satellite image. Furthermore, there may be effects on the emissivity values used to extract the surface temperatures from the satellite images. According to Han et al. , “a 1% change in emissivity can change the surface temperature up to 2 K.” Therefore, because satellite images have low spatial resolutions, they are limited in their ability to analyze exact and detailed emissivity values in urban areas composed of various surface fabrics, and the resulting data will show different surface temperatures from field measurements.
In this paper, we compared surface temperatures measured onsite and via ASTER images during both the day and the night to validate the accuracy of surface temperature satellite imagery used frequently in UHI studies. The results indicated that surface temperatures from field measurements were higher than those derived from satellite images during the day, while the opposite pattern was observed during the night, except for in a few locations. Despite the influence of clouds on the images from July 28, the temperature difference between ASTER images and field measurements was smaller during the night than during the day. While surface temperature differences were small for pixels containing trees and grass during the day, at night the artificial fabrics showed a lesser difference.
This study confirmed problems with the accuracy of surface temperature data derived from satellite images, and these problems vary according to the time of day and the presence of different urban area characteristics. In particular, areas of high density displayed greater discrepancies in temperature compared to open areas. The difference in temperature between field-based and satellite-based measurements was also affected by whether the surface fabric was artificial or not. Overall, differences between infrared satellite image surface temperature data and onsite measurements may be caused by the off-nadir angle of the satellite image, the limited horizontal surface view of earth’s surface, the low spatial resolution of the satellite image, and the application of emissivity values that do not consider the complex spatial characteristics of urban areas. To improve the accuracy of surface temperatures extracted from infrared satellite imagery, we propose a revised model whereby temperature data is obtained from ASTER and emissivity values for various land covers that are extracted based on in situ measurements.
In the future, we will aim to use the data collected in this study to develop a way to improve the accuracy of satellite derived surface temperature data in urban areas. Also, we plan on further assessing the relationship between radiant energy and surface temperatures according to variations in the spatial characteristics of urban areas. Such studies may help to improve the usability of satellite image data in urban areas and likely will also aid urban planners, developers, and researchers in mitigating the adverse effects of heat islands.
Conflict of Interests
The authors declare that there is no conflict of interests regarding the publication of this paper.
This research was supported by Korea Aerospace Research Institute (KARI) (no. 2012-0091-0000) and Basic Science Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Education, Science and Technology (no. 2013-0095-0000).
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