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Black carbon indirect radiative effects in a climate model Cover

Black carbon indirect radiative effects in a climate model

Open Access
|Jan 2017

Abstract

The aerosol–cloud interactions due to black carbon (BC) aerosols, as well as the implied climate responses, are examined using an aerosol module in the coupled atmosphere–ocean general circulation model MPI-ESM. BC is simulated to enhance cloud droplet number concentration (CDNC) by 10–15% in the BC emission source regions, especially in the Tropics and mid-latitudes. Higher CDNC and reduced auto-conversion from cloud water to rain water explains the increased cloud water path over the tropical regions (30∘S–30∘N) in the model. In the global mean, the cloud water– as well as precipitation changes are negligibly small. The global-mean effective radiative forcing due to aerosol–cloud interactions for BC is estimated at-0.13±0.1Wm-2, which is attributable to the increase in CDNC burden and (regionally) cloud water in the model. Global mean temperature and rainfall response were found to be-0.16±0.04Kand-0.004±0.004mmday-1, respectively, with significantly larger regional changes mainly in the downwind regions from BC sources.

Language: English
Page range: 1369342 - 1369342
Submitted on: Mar 18, 2017
Accepted on: Aug 3, 2017
Published on: Jan 1, 2017
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2017 Ribu Cherian, Johannes Quaas, Marc Salzmann, Lorenzo Tomassini, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.