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Meinrat O. Andreae

Researcher at Max Planck Society

Publications -  722
Citations -  80116

Meinrat O. Andreae is an academic researcher from Max Planck Society. The author has contributed to research in topics: Aerosol & Cloud condensation nuclei. The author has an hindex of 131, co-authored 700 publications receiving 72714 citations. Previous affiliations of Meinrat O. Andreae include Florida State University & University of California, San Diego.

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Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate

TL;DR: The major source of cloud-condensation nuclei (CCN) over the oceans appears to be dimethylsulphide, which is produced by planktonic algae in sea water and oxidizes in the atmosphere to form a sulphate aerosol as mentioned in this paper.
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Emission of trace gases and aerosols from biomass burning

TL;DR: In this article, the authors present a set of emission factors for a large variety of species emitted from biomass fires, where data were not available, they have proposed estimates based on appropriate extrapolation techniques.
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Biomass Burning in the Tropics: Impact on Atmospheric Chemistry and Biogeochemical Cycles

TL;DR: Widespread burning of biomass serves to clear land for shifting cultivation, to convert forests to agricultural and pastoral lands, and to remove dry vegetation in order to promote agricultural productivity and the growth of higher yield grasses, but it may also disturb biogeochemical cycles, especially that of nitrogen.
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Black carbon or brown carbon? The nature of light-absorbing carbonaceous aerosols

TL;DR: In this article, the authors show that brown carbon may severely bias measurements of atmospheric "black carbon" and "elemental carbon" over vast parts of the troposphere, especially those strongly polluted by biomass burning, where the mass concentration of C brown is high relative to that of soot carbon.
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Flood or drought: How do aerosols affect precipitation?

TL;DR: A conceptual model is proposed that explains this apparent dichotomy of pristine tropical clouds with low CCN concentrations rain out too quickly to mature into long-lived clouds and heavily polluted clouds evaporate much of their water before precipitation can occur.