Abstract
The Joint Polar Satellite System-1 (renamed NOAA-20 after reaching the polar orbit) was successfully launched on November 18, 2017, into an afternoon orbit with a local equator crossing time of ∼1:30 p.m. , in the same orbital plane as the Suomi National Polar-orbiting Partnership (S-NPP) but with a time separation of 50 min. The NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) will become the primary operational imager succeeding the VIIRS onboard S-NPP, which has been in orbit for more than six years. Although the VIIRS onboard S-NPP and NOAA-20 have identical designs, there are small differences in the relative spectral response (RSR) in most bands. Previous studies have shown that minor differences in the S-NPP RSRs at thermal emissive bands (TEBs) can lead to several effects at the detector level, such as striping in sensor data record (SDR) products. Such differences may explain the striping pattern found in S-NPP VIIRS sea surface temperature (SST) products. This article analyzes the detector-level and operational band-averaged RSRs for NOAA-20 VIIRS TEBs and examines the radiometric response to them using the line-by-line radiative transfer model at a very high spectral resolution for convolving with the RSRs. We also evaluate the impact of RSR differences between S-NPP and NOAA-20 for radiometric biases and potential striping in VIIRS TEB SDR brightness temperature. This article will contribute toward measurement consistency for long-term observations in the thermal infrared bands and ensure the quality of retrieval data produced by VIIRS, such as SST, fire, and other retrievals.
Highlights
The Joint Polar Satellite System-1 was successfully launched on November 18, 2017, into an afternoon orbit with a local equator crossing time of ∼1:30 P.M., in the same orbital plane as the Suomi National Polar-orbiting Partnership (S-NPP) but with a time separation of 50 min
We examine the effects of the detector-level and band-averaged relative spectral response (RSR) on NOAA-20 Visible Infrared Imaging Radiometer Suite (VIIRS) thermal emissive bands (TEBs)
The striping in the NOAA-20 TEB sensor data record (SDR) is expected to be ∼20% less than that in the S-NPP TEB SDRs, which may be reflected in the sea surface temperature (SST) retrievals
Summary
N NOVEMBER 18, 2017, the Joint Polar System-1 satellite was successfully launched. Satellite into an Manuscript received September 12, 2018; revised May 6, 2019 and June 26, 2019; accepted August 26, 2019. Onboard both NOAA-20 and S-NPP satellites is the Visible Infrared Imaging Radiometer Suite (VIIRS), which is a scanning imaging radiometer that produces global imagery and radiometric measurements of the land, atmosphere, cryosphere, and oceans in the visible and infrared bands with moderate spatial resolutions. We examine the effects of the detector-level and band-averaged RSRs on NOAA-20 VIIRS TEBs. We assess in detail the impact of the spectral response differences between S-NPP and NOAA-20 on VIIRS TEBs using radiative transfer model simulations and SDR brightness temperature products.
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More From: IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
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