Cited by 960Atmospheric aerosols and cloudsClimate variability and modelsCalibration and Measurement Techniques

Toward Optimal Closure of the Earth's Top-of-Atmosphere Radiation Budget

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Loeb, Norman G., Wielicki, Bruce A., Doelling, David R., Smith, G. Louis, Keyes, Dennis F., Kato, Seiji, Manalo-Smith, Natividad, Wong, Takmeng·2009·Journal of Climate

Abstract

Despite recent improvements in satellite instrument calibration and the algorithms used to determine reflected solar (SW) and emitted thermal (LW) top-of-atmosphere (TOA) radiative fluxes, a sizeable imbalance persists in the average global net radiation at the TOA from satellite observations. This imbalance is problematic in applications that use earth radiation budget (ERB) data for climate model evaluation, estimate the earth’s annual global mean energy budget, and in studies that infer meridional heat transports. This study provides a detailed error analysis of TOA fluxes based on the latest generation of Clouds and the Earth’s Radiant Energy System (CERES) gridded monthly mean data products [the monthly TOA/surface averages geostationary (SRBAVG-GEO)] and uses an objective constrainment algorithm to adjust SW and LW TOA fluxes within their range of uncertainty to remove the inconsistency between average global net TOA flux and heat storage in the earth–atmosphere system. The 5-yr global mean CERES net flux from the standard CERES product is 6.5 W m−2, much larger than the best estimate of 0.85 W m−2 based on observed ocean heat content data and model simulations. The major sources of uncertainty in the CERES estimate are from instrument calibration (4.2 W m−2) and the assumed value for total solar irradiance (1 W m−2). After adjustment, the global mean CERES SW TOA flux is 99.5 W m−2, corresponding to an albedo of 0.293, and the global mean LW TOA flux is 239.6 W m−2. These values differ markedly from previously published adjusted global means based on the ERB Experiment in which the global mean SW TOA flux is 107 W m−2 and the LW TOA flux is 234 W m−2.

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Crossref · 10.1175/2008jcli2637.1

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  • All radiative metrics but one were given a 1σ tolerance to error of ±5 W/m2 for an observational uncertainty of about 4 W/m2 for the CERES-EBAF L3b satellite product.

    “All the radiative metrics but one were given a 1σ tolerance to error of ±5 W/m2 for an observational uncertainty of about 4 W/m2 for the CERES-EBAF L3b satellite product used as target”

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Authors
Loeb, N. G., Wielicki, B. A., Doelling, D. R., Smith, G. L., Keyes, D. F., Kato, S., Manalo-Smith, N., & Wong, T.
Affiliations
  • Langley Research Center (US)
  • National Institute of Aerospace (US)
  • Science Systems and Applications, Inc., Hampton, Virginia
Venue
Journal of Climate
Published
2009-02-01
Volume
22
Issue
3
Pages
748-766
ISSN
  • 0894-8755 (ISSN-L)
  • 1520-0442
OpenAlex
W2015320755
Cited by
960
References
0
Citations by year
2026: 24 · 2025: 30 · 2024: 49 · 2023: 49 · 2022: 46 · 2021: 55 · 2020: 57 · 2019: 63 · 2018: 71 · 2017: 90 · 2016: 69 · 2015: 94 · 2014: 83 · 2013: 62 · 2012: 57
FWCI
17.85
Type
journal article
Language
en
Open access
Locations
Journal of Climate (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric aerosols and clouds
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Physical Sciences › Engineering › Aerospace Engineering › Calibration and Measurement Techniques
Keywords
Earth radiation budget, top-of-atmosphere radiation budget, Ceres, total solar irradiance, ocean heat content, thermal energy storage, climate model evaluation

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