Arctic fire aerosols simulated by a modified version of the ECHAM-HAM global model

This file contains modeling outputs generated using a modified version of the global aerosol-climate model ECHAM6.3-HAM2.3. The simulations focus on aerosols originating from biomass burning over the boreal region (>55°N) and cover both the current period (2000–2021) and future projections. The data provide annual summer (June–August) seasonal averages for each year within these periods. The future scenario simulations assume a global warming level of 1°C above present-day temperatures, which results in higher biomass burning emissions in the boreal region. These future simulations are driven by projected biomass burning emissions that remain constant, with meteorological fields nudged to the 2000-2020 period to account for the impacts of transport conditions. The following aerosol-related variables are provided: od550er: Aerosol optical depth at a wavelength of 550 nmabs550aer: Absorption aerosol optical depth at 550 nmERE: Effective radiative effect (all-sky condition) at the top of the atmosphere (TOA)ARI: Radiative effect due to aerosol-radiation interactionACI: Radiative effect due to aerosol-cloud interaction For further information or inquiries, please contact Dr. Qirui Zhong at [email protected].

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2024-09-19
DOI
https://doi.org/10.5281/zenodo.13789810
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
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article

Arctic fire aerosols simulated by a modified version of the ECHAM-HAM global model

Zenodo (CERN European Organization for Nuclear Research)
Atmospheric aerosols and clouds
article

Arctic fire aerosols simulated by a modified version of the ECHAM-HAM global model

article en

Abstract

This file contains modeling outputs generated using a modified version of the global aerosol-climate model ECHAM6.3-HAM2.3. The simulations focus on aerosols originating from biomass burning over the boreal region (>55°N) and cover both the current period (2000–2021) and future projections. The data provide annual summer (June–August) seasonal averages for each year within these periods. The future scenario simulations assume a global warming level of 1°C above present-day temperatures, which results in higher biomass burning emissions in the boreal region. These future simulations are driven by projected biomass burning emissions that remain constant, with meteorological fields nudged to the 2000-2020 period to account for the impacts of transport conditions. The following aerosol-related variables are provided: od550er: Aerosol optical depth at a wavelength of 550 nmabs550aer: Absorption aerosol optical depth at 550 nmERE: Effective radiative effect (all-sky condition) at the top of the atmosphere (TOA)ARI: Radiative effect due to aerosol-radiation interactionACI: Radiative effect due to aerosol-cloud interaction For further information or inquiries, please contact Dr. Qirui Zhong at [email protected].

Zenodo (CERN European Organization for Nuclear Research)
Peking University (CN)
Climate action
Openalex Percentile: Top 72%
Atmospheric aerosols and clouds
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