Abstract

Tropical deep convective clouds (DCC) are an excellent invariant target for vicarious calibration of satellite visible (VIS) and near-infrared (NIR) solar bands. The DCC technique (DCCT) is a statistical approach that collectively analyzes all identified DCC pixels on a monthly basis. The DCC reflectance in VIS and NIR spectrums is mainly a function of cloud optical depth, and provides a stable monthly statistical mode. However, for absorption shortwave infrared (SWIR) bands, the monthly DCC response is found to exhibit large seasonal cycles that make the implementation of the DCCT more challenging at these wavelengths. The seasonality assumption was tested using the SNPP-VIIRS SWIR bands, with up to 50% of the monthly DCC response temporal variation removed through deseasonalization. In this article, a monthly DCC bidirectional reflectance distribution function (BRDF) approach is proposed, which is found to be comparable to or can outperform the effects of deseasonalization alone. To demonstrate that the SNPP-VIIRS DCC BRDF can be applied to other JPSS VIIRS imagers in the same 13:30 sun-synchronous orbit, the VIIRS DCC BRDF was applied to Aqua-MODIS. The Aqua-MODIS SWIR band DCC reflectance natural variability is reduced by up to 45% after applying the VIIRS-based monthly DCC BRDFs.

Highlights

  • In 2017, NOAA began on the follow-on Joint Polar Satellite System (JPSS)-3 and JPSS-4 satellites, each having 5–6 instruments [1]

  • The Visible Infrared Imaging Radiometer Suite (VIIRS)-based all-season and monthly deep convective clouds (DCC) bidirectional reflectance distribution function (BRDF) models for shortwave infrared (SWIR) bands are evaluated

  • For Moderate Resolution Imaging Spectroradiometer (MODIS), the IR calibration is stable over time to within 0.1 K when compared to the Atmospheric Infrared Sounder (AIRS) [26]

Read more

Summary

Introduction

In 2017, NOAA began on the follow-on Joint Polar Satellite System (JPSS)-3 and JPSS-4 satellites, each having 5–6 instruments [1]. The CERES Edition 3 fluxes were impacted by a Moderate Resolution Imaging Spectroradiometer (MODIS) imager band 1 (0.65 μm) collection 5 calibration drift of 2% [5], which reduced the cloud optical depth over time, and thereby changed the scene selection, causing a reduction in the CERES shortwave (SW) flux by −0.25 Wm−2 [6]. This reduction is close to the SW flux stability requirement for climate accuracy, i.e., 0.3 Wm−2/decade [7]. This inter-series continuity will be the topic of a follow-on paper

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call