Abstract

The latest CERES FM-5 instrument launched onboard the S-NPP spacecraft will use the VIIRS visible radiances from the NASA Land Product Evaluation and Analysis Tool Elements (PEATE) product for retrieving the cloud properties associated with its TOA flux measurement. In order for CERES to provide climate quality TOA flux datasets, the retrieved cloud properties must be consistent throughout the record, which is dependent on the calibration stability of the VIIRS imager. This paper assesses the NASA calibration stability of the VIIRS reflective solar bands using the Libya-4 desert and deep convective clouds (DCC). The invariant targets are first evaluated for temporal natural variability. It is found for visible (VIS) bands that DCC targets have half of the variability of Libya-4. For the shortwave infrared (SWIR) bands, the desert has less variability. The brief VIIRS record and target variability inhibits high confidence in identifying any trends that are less than ±0.6%/yr for most VIS bands, and ±2.5%/yr for SWIR bands. None of the observed invariant target reflective solar band trends exceeded these trend thresholds. Initial assessment results show that the VIIRS data have been consistently calibrated and that the VIIRS instrument stability is similar to or better than the MODIS instrument.

Highlights

  • The Clouds and the Earth’s Radiant Energy System (CERES) [1] provides the climate community with a continuous global top-of-atmosphere (TOA) shortwave and longwave flux observation record beginning in 2000 using CERES instruments mounted onboard the Terra, Aqua and Suomi NationalPolar-orbiting Partnership (S-NPP) spacecrafts

  • This study has provided an initial assessment of the radiometric calibration stability of the Suomi NationalPolar-orbiting Partnership (S-NPP)

  • Visible Infrared Imaging Radiometer Suite (VIIRS) reflective solar bands (RSB) of the NASA Land Product Evaluation and Analysis Tool Elements (PEATE) AS3100 product archived at ASDC using the Libya-4 desert and the deep convective clouds (DCC) pixels located over the Tropical West Pacific (TWP) region as two independent radiometrically stable targets

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Summary

Introduction

The Clouds and the Earth’s Radiant Energy System (CERES) [1] provides the climate community with a continuous global top-of-atmosphere (TOA) shortwave and longwave flux observation record beginning in 2000 using CERES instruments mounted onboard the Terra, Aqua and Suomi National. CERES does not incorporate the official NASA Goddard Space Flight Center (GSFC) imager cloud product properties [4], and applies its own retrieval algorithm, designed to be stable throughout the record, and consistent in providing cloud properties for all identified cloud pixels [5] This method ensures that the cloud properties do not introduce any artificial trends in the radiance-to-flux conversion. The latest of the CERES instruments, Flight Model-5 (FM-5), was launched aboard the S-NPP spacecraft on 28 October 2011 from the Vandenberg Air Force Base, California [6] Another key instrument onboard S-NPP is the Visible Infrared Imaging Radiometer Suite (VIIRS), which collects the Earth view data in 22 spectral bands with wavelengths ranging from 0.41 to 12 μm [7,8].

Sensor Overview and Dataset Selection
Methodology
Desert Approach
DCC Approach
Target Temporal Variability
Trend Significance
Concluding Remarks
Findings
Conflicts of Interest
Full Text
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