Sentinel-2A MSI and Landsat 8 OLI Provide Data Continuity for Geological Remote Sensing

被引:126
作者
van der Werff, Harald [1 ]
van der Meer, Freek [1 ]
机构
[1] Univ Twente, Fac Geoinformat Sci & Earth Observat, Drienerlolaan 5, NL-7522 NB Enschede, Netherlands
来源
REMOTE SENSING | 2016年 / 8卷 / 11期
关键词
Sentinel-2A MSI; Landsat; 8; OLI; geology; alteration; band ratios; simulation; Cabo de Gata; Rodalquilar; SPACEBORNE THERMAL EMISSION; IMAGING SPECTROMETRY DATA; SIMULATED SENTINEL-2; AIRBORNE; CROP; RESOLUTION; MISSIONS; INDEX; LAI; CAPABILITIES;
D O I
10.3390/rs8110883
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Sentinel-2A MSI is the Landsat-like spatial resolution (10-60 m) super-spectral instrument of the European Space Agency (ESA), aimed at additional data continuity for global land surface monitoring with Landsat and Satellite Pour l'Observation de la Terre (SPOT) missions. Several simulation studies have been conducted in the last several years to show the potential of Sentinel-2A MSI (MultiSpectral Instrument). Now that real data are available, the first confirmations of this potential and comparisons with other operational systems are being made. This paper aims at evaluating Sentinel-2A MSI band ratio products that are relevant for geological remote sensing. A Sentinel-2A MSI and a Landsat 8 OLI (Operational Land Imager) scene were processed from their respective levels L1C and L1T to level L2A (bottom of atmosphere reflectance). Then, three band ratios originally defined for Landsat TM (Thematic Mapper) were used to map mineralogy associated with a hydrothermal alteration system in southeast Spain. The results obtained with Sentinel-2A MSI were compared with those obtained with Landsat 8 OLI and a simulated Sentinel-2A MSI dataset that was used before actual data were released. Results show that the images appear similar to the human eye having a correlation of approximately 0.8 and higher, but that the associated data ranges differ significantly. The resulting products are also compared to a published geologic map of the study area, and it is shown that the resulting maps correspond with the conceptual geologic model of the epithermal deposit.
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页数:16
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