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Comparing contact and immersion freezing from continuous flow diffusion chambers

Comparing contact and immersion freezing from continuous flow diffusion chambers

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_gale_infotracmisc_A482100467

Comparing contact and immersion freezing from continuous flow diffusion chambers

About this item

Full title

Comparing contact and immersion freezing from continuous flow diffusion chambers

Publisher

Copernicus GmbH

Journal title

Atmospheric chemistry and physics, 2016-02, Vol.2016 (2), p.1

Language

English

Formats

Publication information

Publisher

Copernicus GmbH

More information

Scope and Contents

Contents

Ice nucleating particles (INPs) in the atmosphere are responsible for glaciating cloud droplets between 237 K and 273 K. Different mechanisms of heterogeneous ice nucleation can compete under mixed-phase cloud conditions. Contact freezing is considered relevant because higher ice nucleation temperatures than for immersion freezing for the same INPs...

Alternative Titles

Full title

Comparing contact and immersion freezing from continuous flow diffusion chambers

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_gale_infotracmisc_A482100467

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_gale_infotracmisc_A482100467

Other Identifiers

ISSN

1680-7316

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