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EVALUATION OF SURFACE HEAT FLUX BASED ON SATELLITE REMOTE SENSING AND FIELD MEASUREMENT DATA

机译:基于卫星遥感和现场测量数据的表面热通量评估

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The objective of this study was to evaluate surface heat fluxes based on satellite remote sensing data and field measurement data. Surface heat fluxes were estimated around the city of Cheongju, South Korea using Landsat 5 TM data and modeler of ERDAS Imagine. Landsat data was acquired on 6 August, 2006 (path 115, row 35). Field measurement was conducted in the paddy field and upland. And it was collected the same day with acquisition of Landsat imagery using net radiometer (Q-7.1, Campbell Scientific Inc.) and geothermometer (MF-180M, EKO Instruments Trading Co.). The result of this study was that net radiation at the surface was 350 ~ 670 W/m~2. The percentage of surface heat fluxes were approximately 30% from sensible heat flux to the air, approximately 10% from soil heat flux, and 60% from latent heat flux. The surface heat flux in paddy field data was similar to Landsat data. The upland data was much alike, but they do have dissimilarities because the upland was too small area, considering Landsat image resolution. The results suggest that the methodology was feasible to estimate surface heat fluxes with reasonable accuracy over study areas.
机译:本研究的目的是评价根据卫星遥感数据和场测量数据表面的热通量。表面热通量是围绕使用的Landsat 5 TM数据和ERDAS的建模畅想城市清州,韩国的估计。大地卫星数据被获取8月6日,2006(路径115,行35)。场测量在稻田和高地进行。它收集与利用收购净辐射计(Q-7.1,坎贝尔科技公司)和地温(MF-180M,EKO仪器贸易有限公司)陆地卫星图像的同一天。这项研究的结果是在表面上的净辐射为350〜670瓦/米〜2。表面热通量的百分比分别为约30%,从显热通量在空气中,大约10%的从​​土壤热通量,并从潜热通量的60%。在水田数据表面热通量类似于大地卫星数据。高地数据是相像,但他们也有不同点,因为高地太小区,考虑陆地卫星图像分辨率。结果表明,该方法结束研究领域估算合理准确地表面热通量是可行的。

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