Although parts of the GOES-16/17 satellite scan ranges overlap (See 'GOES Coverage' article), the scans they produce can turn out quite different. For example, take a look at their scans for the same moment over the Cherrywood Fire in Nevada (about (37, -116)).
library(MazamaSatelliteUtils) library(MazamaSpatialUtils) setSatelliteDataDir("~/Data/Satellite") setSpatialDataDir("~/Data/Spatial") loadSpatialData("NaturalEarthAdm1") bbox <- c(-122.5, -111.5, 34.5, 42.5) scanFileG16 <- goesaodc_downloadScanFiles( satID = "G16", datetime = "2021-05-20 00:30", timezone = "UTC" ) scanRasterG16 <- goesaodc_createScanRaster( filename = scanFileG16, bbox = bbox, dqfLevel = 3, cellSize = 0.05 ) goesaodc_plotScanRaster( raster = scanRasterG16, bbox = bbox, legendLimits = c(-0.1, 5.1), stateCodes = c("OR", "ID", "NV", "CA", "AZ", "UT"), title = "G16 at 2021-05-20 00:30 UTC" )
scanFileG17 <- goesaodc_downloadScanFiles( satID = "G17", datetime = "2021-05-20 00:30", timezone = "UTC" ) scanRasterG17 <- goesaodc_createScanRaster( filename = scanFileG17, bbox = bbox, dqfLevel = 3, cellSize = 0.05 ) goesaodc_plotScanRaster( raster = scanRasterG17, bbox = bbox, legendLimits = c(-0.1, 5.1), stateCodes = c("OR", "ID", "NV", "CA", "AZ", "UT"), title = "G17 at 2021-05-20 00:30 UTC" )
There are several differences between these two images. For instance, GOES-17 appears to record more cloud cover than GOES-16. Additionally, GOES-16 reads AOD values over the ocean (maybe all bodies of water?) as ~0, while GOES-17 reads them as ~5.
Even though GOES-17 is positioned closer to Nevada, from these two plots we can see that the clearest images we'd get of the Cherrywood fire would come from GOES-16 scans. A bit counterintuitive, isn't it?
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