Technology and Methodology |
|
|
|
|
|
The Feasibility of Replacing Surface Temperature with Surface Radiation Temperature: A Case Study of "FY-2C" and MODIS Data |
RONG Yuan1,2, YANG Yong-min1,2 |
1. Key Laboratory of Water Cycle & Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China |
|
|
Abstract In order to invert the land surface temperature data of a whole day, the authors first used data for MODIS land surface temperature and the same passing time of the two infrared channels of FY-2C satellite to obtain the regression coefficient by linear fitting of each pixel without considering atmospheric water vapor content and land surface emissivity, and then inverted the land surface radiation temperature with the spatial resolution of 5 km per hour of the day. Based on the transit time, the maximum and minimum surface temperatures appeared, which were downscaled to the spatial resolution of 1 km. Comparing the distribution of the 5 km spatial resolution land surface radiation temperature inverted from FY-2C data with the distribution of MODIS 5 km spatial resolution land surface temperature at the same time and same scale, the authors found that their spatial distributions are similar. Finally, the authors calculated the average 1 km spatial resolution surface radiation temperature inverted from FY-2C remote sensing data and MODIS 1 km spatial resolution land surface temperature in the regions with different vegetation types in combination with the vegetation cover classification map, and the results suggest that the absolute error is 1.95 K and the relative error is 10.7%, which means that the error of the land surface radiation temperature inverted by the method and the land surface temperature is below 2 K when the main body of the land surface is covered with soil and vegetation.
|
Keywords
Land surface temperature(LST)
ASTER
NDVI
Urban heat island effect
|
|
Issue Date: 16 December 2011
|
|
|
[1] Wan Z M,Li Z L.A Physics-based Algorithm for Retrieving Land-surface Emissivity and Temperature from EOS/MODIS Data[J].IEEE Transactions on Geoscience and Remote Sensing,1997,35(4):980-996.[2] Li Z L,Becker F.Feasibility of Land Surface Temperature and Emissivity Determination from AVHRR Data[J].Remote Sensing of Environment,1993,43(1):67-85.[3] Mao K,Qin Z,Shi J,et al.A Practical Split-window Algorithm for Retrieving Land-surface Temperature from MODIS Data[J].International Journal of Remote Sensing,2005,26(15):3181-3204.[4] Qin Z H,Karinieli A.Progress in the Remote Sensing of Land Surface Temperature and Ground Emissivity Using NOAA-AVHRR Data[J].International Journal of Remote Sensing,1999,20(12):2367-2393.[5] Kaufman Y J,Gao B C.Remote Sensing of Water Vapor in the Near IR from EOS/MODIS[J].IEEE Transactions on Geoscience and Remote Sensing,1992,30(5):871-884.[6] 张仁华.定量热红外遥感模型及地面实验基础[M].北京:科学出版社,2009.[7] Hurtado E,Vidal A,Caselles V.Comparison of Two Atmospheric Correction Methods for Landsat TM Thermal Band[J].International Journal of Remote Sensing,1996,17(2):237-247.[8] Tang B H,Bi Y Y,Li Z L,et al.Generalized Split-window Algorithm for Estimate of Land Surface Temperature from Chinese Geostationary FengYun Meteorological Satellite(FY-2C)Data[J].Sensors,2008,8(2):933-951.[9] Shu Y Q,Stisen S,Jenen K H,et al.Estimation of Regional Evapotranspiration over the North China Plain Using Geostationary Satellite Data[J].International Journal of Applied Earth Observation and Geoinformation,2011,13(2):192-206.[10] Sobrino J A,Romaguera M.Land Surface Temperature Retrieval from MSG1-SEVIRI Data[J].Remote Sensing of Environment,2004,92(2):247–254.[11] 覃志豪,Zhang M H,Karnieli A,等.用陆地卫星TM6数据演算地表温度的单窗算法[J].地理学报,2001,56(4):456-466.[12] 黄妙芬,刘绍民,刘素红,等.地表温度和地表辐射温度差值分析[J].地球科学进展,2005,20(10):1075-1082.[13] Kustas P W,Norman J M.Evaluation of Soil and Vegetation Heat Flux Predictions Using a Simple Two-source Model with Radiometric Temperatures for Partial Canopy Cover[J].Agricultural and Forest Meteorology,1999,94(1):13-29.[14] Zhan X,Kustas W P,Humes K S.An Intercomparison Study on Models of Sensible Heat Flux over Partial Canopy Surfaces with Remotely Sensed Surface Temperature[J].Remote Sensing of Environment,1996,58(3):242-256.[15] 王鹏新,龚健雅.基于植被指数和土地表面温度的干旱监测模型[J].地球科学进展,2003,18(4):527-533.[16] 张仁华.对于定量热红外遥感的一些思考[J].国土资源遥感,1999(1):1-6.[17] Wan Z M,Dozier J.A Generalized Split-window Algorithm for Retrieving Land-surface Temperature from Space[J].IEEE Transactions on Geoscience and Remote Sensing,1996,34(4):892-905.[18] 张仁华,孙晓敏,王伟民,等.一种可操作的区域尺度地表通量定量遥感二层模型的物理基础[J].中国科学D辑,2004,34(Z2):200-216. |
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
|
Shared |
|
|
|
|
|
Discussed |
|
|
|
|