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ZENODO
Dataset . 2021
License: CC BY
Data sources: Datacite
image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
ZENODO
Dataset . 2021
License: CC BY
Data sources: Datacite
image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
ZENODO
Dataset . 2021
License: CC BY
Data sources: ZENODO
image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
https://doi.org/10.5281/zenodo...
Dataset . 2021
License: CC BY
Data sources: Sygma
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Claim

Aerosol-light interactions reduce the carbon budget imbalance - DGVM output

Research datakeyboard_double_arrow_right Dataset 09 Nov 2021Publisher:ZenodoFunded by:EC | 4C
Authors: O'Sullivan, Michael; Zhang, Yuan;

doi: 10.5281/zenodo.5658676 , 10.5281/zenodo.5658677

Aerosol-light interactions reduce the carbon budget imbalance - DGVM output

Abstract

DGVM (JULES and ORCHIDEE_DF) output associated with the publication 'Aerosol-light interactions reduce the carbon budget imbalance' (O'Sullivan et al., 2021 - Environmental Research Letters). Files contain monthly data over the period 1901-2017. There are 7 simulations for each model, with varying surface solar radiation in each case. Atmospheric CO2 and all climate variables (except for incoming short-wave radiation) vary throughout all simulations. Historical: total and diffuse shortwave radiation depend on the solar zenith angle, temporally varying cloud cover and aerosol optical depth of the whole atmospheric column. FixedAero: Time-invariant (1901-1920 cycle) tropospheric aerosol and no stratospheric aerosol influence on total and diffuse shortwave radiation FixedTropAero: Time-invariant (1901-1920 cycle) tropospheric aerosol influence on total and diffuse shortwave radiation FixedStratAero: no stratospheric aerosol influence on total and diffuse shortwave radiation FixedAero_DF: Time-invariant (1901-1920 cycle) tropospheric aerosol and no stratospheric aerosol influence on diffuse shortwave radiation FixedTropAero_DF: Time-invariant (1901-1920 cycle) tropospheric aerosol influence on diffuse shortwave radiation FixedStratAero_DF: no stratospheric aerosol influence on diffuse shortwave radiation

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