Pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluation

Top-of-atmosphere (TOA) spectrally resolved shortwave reflectances and long-wave radiances describe the response of the Earth's surface and atmosphere to feedback processes and human-induced forcings. In order to evaluate proposed long-duration spectral measurements, we have projected 21st Cent...

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Main Authors: D. R. Feldman, W. D. Collins, J. L. Paige
Format: Article
Language:English
Published: Copernicus Publications 2015-07-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/8/1943/2015/gmd-8-1943-2015.pdf
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spelling doaj-68c7a9bd082c4f189175d326767a7a6f2020-11-24T23:44:21ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032015-07-01871943195410.5194/gmd-8-1943-2015Pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluationD. R. Feldman0W. D. Collins1J. L. Paige2Lawrence Berkeley National Laboratory, Earth Sciences Division, Berkeley, CA, USALawrence Berkeley National Laboratory, Earth Sciences Division, Berkeley, CA, USALawrence Berkeley National Laboratory, Earth Sciences Division, Berkeley, CA, USATop-of-atmosphere (TOA) spectrally resolved shortwave reflectances and long-wave radiances describe the response of the Earth's surface and atmosphere to feedback processes and human-induced forcings. In order to evaluate proposed long-duration spectral measurements, we have projected 21st Century changes from the Community Climate System Model (CCSM3.0) conducted for the Intergovernmental Panel on Climate Change (IPCC) A2 Emissions Scenario onto shortwave reflectance spectra from 300 to 2500 nm and long-wave radiance spectra from 2000 to 200 cm<sup>−1</sup> at 8 nm and 1 cm<sup>−1</sup> resolution, respectively. The radiative transfer calculations have been rigorously validated against published standards and produce complementary signals describing the climate system forcings and feedbacks. Additional demonstration experiments were performed with the Model for Interdisciplinary Research on Climate (MIROC5) and Hadley Centre Global Environment Model version 2 Earth System (HadGEM2-ES) models for the Representative Concentration Pathway 8.5 (RCP8.5) scenario. The calculations contain readily distinguishable signatures of low clouds, snow/ice, aerosols, temperature gradients, and water vapour distributions. The goal of this effort is to understand both how climate change alters reflected solar and emitted infrared spectra of the Earth and determine whether spectral measurements enhance our detection and attribution of climate change. This effort also presents a path forward to understand the characteristics of hyperspectral observational records needed to confront models and inline instrument simulation. Such simulation will enable a diverse set of comparisons between model results from coupled model intercomparisons and existing and proposed satellite instrument measurement systems.http://www.geosci-model-dev.net/8/1943/2015/gmd-8-1943-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. R. Feldman
W. D. Collins
J. L. Paige
spellingShingle D. R. Feldman
W. D. Collins
J. L. Paige
Pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluation
Geoscientific Model Development
author_facet D. R. Feldman
W. D. Collins
J. L. Paige
author_sort D. R. Feldman
title Pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluation
title_short Pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluation
title_full Pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluation
title_fullStr Pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluation
title_full_unstemmed Pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluation
title_sort pan-spectral observing system simulation experiments of shortwave reflectance and long-wave radiance for climate model evaluation
publisher Copernicus Publications
series Geoscientific Model Development
issn 1991-959X
1991-9603
publishDate 2015-07-01
description Top-of-atmosphere (TOA) spectrally resolved shortwave reflectances and long-wave radiances describe the response of the Earth's surface and atmosphere to feedback processes and human-induced forcings. In order to evaluate proposed long-duration spectral measurements, we have projected 21st Century changes from the Community Climate System Model (CCSM3.0) conducted for the Intergovernmental Panel on Climate Change (IPCC) A2 Emissions Scenario onto shortwave reflectance spectra from 300 to 2500 nm and long-wave radiance spectra from 2000 to 200 cm<sup>−1</sup> at 8 nm and 1 cm<sup>−1</sup> resolution, respectively. The radiative transfer calculations have been rigorously validated against published standards and produce complementary signals describing the climate system forcings and feedbacks. Additional demonstration experiments were performed with the Model for Interdisciplinary Research on Climate (MIROC5) and Hadley Centre Global Environment Model version 2 Earth System (HadGEM2-ES) models for the Representative Concentration Pathway 8.5 (RCP8.5) scenario. The calculations contain readily distinguishable signatures of low clouds, snow/ice, aerosols, temperature gradients, and water vapour distributions. The goal of this effort is to understand both how climate change alters reflected solar and emitted infrared spectra of the Earth and determine whether spectral measurements enhance our detection and attribution of climate change. This effort also presents a path forward to understand the characteristics of hyperspectral observational records needed to confront models and inline instrument simulation. Such simulation will enable a diverse set of comparisons between model results from coupled model intercomparisons and existing and proposed satellite instrument measurement systems.
url http://www.geosci-model-dev.net/8/1943/2015/gmd-8-1943-2015.pdf
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