Abstract

A Climate Hyperspectral Infrared Radiance Product (CHIRP) is introduced combining data from the Atmospheric Infrared Sounder (AIRS) on NASA’s EOS-AQUA platform, the Cross-Track Infrared Sounder (CrIS) sounder on NASA’s SNPP platform, and continuing with CRIS sounders on the NOAA/NASA Joint Polar Satellite Series (JPSS) of polar satellites. The CHIRP product converts the parent instrument’s radiances to a common Spectral Response Function (SRF) and removes inter-satellite biases, providing a consistent inter-satellite radiance record. The CHIRP record starts in September 2002 with AIRS, followed by CrIS SNPP and the JPSS series of CrIS instruments. The CHIRP record should continue until the mid-2040’s as additional JPSS satellites are launched. These sensors, in CHIRP format, provide the climate community with a homogeneous sensor record covering much of the infrared. We give an overview of the conversion of AIRS and CrIS to CHIRP, and define the SRF for common CHIRP format. Considerable attention is paid to removing static bias offsets among these three sensors. The CrIS instrument on NASA’s SNPP satellite is used as the calibration standard. Simultaneous Nadir Overpasses (SNOs) as well as large statistical samplings of radiances from these three satellites are used to derive the instrument bias offsets and estimate the bias offset accuracy, which is ~0.03 K. In addition, possible scene-dependent calibration differences between CHIRP derived from AIRS and CHIRP derived from CrIS on the SNPP platform are presented.

Highlights

  • Continuous hyperspectral satellite measurements of the earth’s up-welling infrared radiance spectrum started in 2002 with the The Atmospheric Infrared Sounder (AIRS)on NASA’s AQUA satellite platform [1] flying in a sun-synchronous polar orbit with a13:30 ascending node equator crossing time

  • We introduce a terminology for Climate Hyperspectral Infrared Radiance Product (CHIRP) here that will be used in the data product names: (1) CHIRP-AQ is CHIRP derived from AIRS on AQUA, (2) CHIRP-SN is CHIRP derived from Cross-Track Infrared Sounder (CrIS) on the SNPP platform, and (3) CHIRP-J1 is CHIRP derived from CrIS on the Joint Polar Satellite System (JPSS)-1 satellite

  • This choice means that CHIRP will not convert SNPPCrIS radiances from mission start to 4 December 2014 to CHIRP format, since Normal Spectral Resolution (NSR) mode radiances cannot be converted to CHIRP

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Summary

Introduction

Continuous hyperspectral satellite measurements of the earth’s up-welling infrared radiance spectrum started in 2002 with the The Atmospheric Infrared Sounder (AIRS). (Note that IASI is used in Section 3.1 to inter-compare SNPP CrIS with NOAA20 CrIS via SNOs.) This data set will provide a more stable and homogeneous set of radiances for retrievals and climate trend analyses than the existing disparate set of radiances from these satellite sounders In one sense it may provide a subset (thermal infrared) of climate information envisioned by the CLARREO mission, but with far greater temporal and spatial sampling. CHIRP data can be used to (1) help improve long-term records from 1Dvar retrievals by removing inter-instrument bias offsets and allowing the use of a single RTA across many instruments, and (2) provide an homogeneous radiance record crossing instrument boundaries for direct measurements of radiance anomalies and trends, and comparisons to climate models and reanalysis products properly converted to radiances. Work to produce gridded versions of CHIRP are underway, providing infrared radiance measurements similar to those envisioned for CLARREO

CHIRP Sensor Record
The AIRS to CHIRP Translation
NEdN Estimates
Inter-Satellite CHIRP Bias Corrections
CHIRP:AQ and CHIRP:J1 Bias Offsets versus CHIRP:SN
Findings
Summary
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