利用FY-1D极轨气象卫星分裂窗区通道计算陆表温度
LAND SURFACE TEMPERATURE ESTIMATED BY REMOTE SENSING DATA FROM FY-1D POLAR METEOROLOGICAL SATELLITE
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摘要: 根据理论和经验上已证明的地表温度与AVHRR窗区通道4、5的亮度温度存在线性或非线性关系, 通过对2818条全球晴空大气廓线做不同比辐射率地表的FY-1D窗区通道4、5辐射率的模拟计算, 推导出FY-1D极轨气象卫星的红外通道4、5亮温与地表温度的二次回归关系式。同时详细介绍了由这一回归关系式和FY-1D高分辨率图像传输 (HRPT) 遥测数据计算陆表温度的方法, 最后给出陆表温度计算结果的精度:用中国地面气象台站的0 cm地温观测数据与相同时刻的分辨率为0.01°×0.01°经纬度的卫星陆表温度相对比, 两者非常吻合, 绝大部分台站|ΔT|<3.0 K。Abstract: The split window method was widely used to retrieve the land surface temperature (LS T) from satellite remote sensing data in the 1980s and the 1990s.The scientists demonstrated theoretically or statistically that there exists a linear or non-linear relationship between the LST and AVHRR channel 4, 5 brightness temperatures.2818 clear sky radiosonde profiles were used to simulate the FY-1D HRPT channel 4, 5 brightness temperatures for different ground emissivities.The derived no n-linear regression equation for each ground type is :TLS=T4 +A(T4-T5)+B(T4-T5)2 +D.Meanwhile, the calculating method of LST by using FY-1D HRPT data and the regression equation were described.Finally, the accuracy of the calculated LST in main land of China was given :compared with the 0 cm soil temperatures observed by Chinese meteorological ground stations, the LSTs calculated by FY-1D data are very co-ordinate with the station observations.For most ground stations, the deviations between the satellite LST and stations observations are less than 3.0 K.
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图 3 不同时间不同地理范围的卫星地表温度计算结果与同一地理位置、同一时刻地面气象台站0 cm地温观测数据对比 (a)2002年11月1日01:35 UTC
(地理范围:33°~43°N, 115°~125°E), (b)2003年1月14日01:05 UTC (地理范围:18°~28°N, 108°~118°E), (c)2002年12月10日02 :40 UTC (地理范围:26°~36°N, 88°~98°E)(图中TS是地面0 cm温度观测数据, TLS是卫星地表温度, 实心圆点代表地温观测数据是用白天地面0 cm地温最高值出现在当地时13 :00推算出的, 三角形代表地温观测数据是用白天地面0 cm地温最高值出现在当地时12:00推算出的)
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