Abstract

The Clouds and the Earth’s Radiant Energy System (CERES) project relies on geostationary (GEO) imager derived TOA broadband fluxes and cloud properties to account for the regional diurnal fluctuations between the Terra and Aqua CERES and MODIS measurements. Anchoring the GEO visible calibration to the MODIS reference calibration and stability is critical for consistent fluxes and cloud retrievals across the 16 GEO imagers utilized in the CERES record. The CERES Edition 4A used GEO and MODIS ray-matched radiance pairs over all-sky tropical ocean (ATO-RM) to transfer the MODIS calibration to the GEO imagers. The primary GEO ATO-RM calibration was compared with the deep convective cloud (DCC) ray-matching and invariant desert/DCC target calibration methodologies, which are all tied to the same Aqua-MODIS calibration reference. Results indicate that most GEO record mean calibration method biases are within 1% with respect to ATO-RM. Most calibration method temporal trends were within 0.5% relative to ATO-RM. The monthly gain trend standard errors were mostly within 1% for all methods and GEOs. The close agreement amongst the independent calibration techniques validates all methodologies, and verifies that the coefficients are not artifacts of the methodology but rather adequately represent the true GEO visible imager degradation.

Highlights

  • The Clouds and the Earth’s Radiant Energy System CERES project [1] synoptic gridded (SYN1deg) product relies on geostationary visible imager (GEO) derived TOA broadband fluxes and retrieved cloud properties to account for the regional diurnal fluctuations from times between the CERES and Moderate Resolution Imaging Spectroradiometer (MODIS) measurement intervals [2]

  • Each sensor may have unique contaminants, the exposure to solar radiation darkens the contaminants over time. It is critical for the CERES SYN1deg product to have uniform GEO cloud retrievals and computed surface fluxes across all 16 geostationary satellites (GEOsats) in the CERES record

  • The CERES Edition 4A reprocessing effort provided an opportunity to improve upon the Edition 3A GEO and MODIS coincident, collocated, all-sky tropical ocean ray-matching (ATO-RM) radiance pairs method of transferring the Terra-MODIS Collection 5 (C5) band 1 calibration

Read more

Summary

Introduction

The Clouds and the Earth’s Radiant Energy System CERES project [1] synoptic gridded (SYN1deg) product relies on geostationary visible imager (GEO) derived TOA broadband fluxes and retrieved cloud properties to account for the regional diurnal fluctuations from times between the CERES and Moderate Resolution Imaging Spectroradiometer (MODIS) measurement intervals [2]. The MODIS and GEO cloud properties are used to compute the hourly surface fluxes contained in the SYN1deg product [3]. The GEO-derived TOA SW fluxes are radiometrically scaled regionally to the CERES SW fluxes to maintain the CERES instrument calibration in the CERES SYN1deg product. The scaling removes any outstanding GEO derived flux artifacts as a result of inadequate calibration, cloud properties, narrowband to broadband models, or angular distribution models.

Methods
Discussion
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