Large hemispheric difference in ultrafine aerosol concentrations in the lowermost stratosphere at mid and high latitudes

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Large hemispheric difference in ultrafine aerosol concentrations in the lowermost stratosphere at mid and high latitudes ; year:2021 ; pages:1-44
Atmospheric chemistry and physics / Discussions. Discussions ; (2021), 1-44

Creator: Williamson, Christina J.
Kupc, Agnieszka
Rollins, Andrew
Kazil, Jan
Froyd, Karl D.
Ray, Eric A.
Murphy, Daniel M.
Schill, Gregory P.
Peischl, Jeff
Thompson, Chelsea
Bourgeois, Ilann
Ryerson, Thomas
Diskin, Glenn
DiGangi, Joshua P.
Blake, Donald R.
Bui, Thao Paul V.
Dollner, Maximilian
Weinzierl, Bernadett
Brock, Charles A.

DOI: 10.5194/acp-2021-22

URN: urn:nbn:de:101:1-2021012804214161480802

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:32 AM CEST

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Associated

Williamson, Christina J.
Kupc, Agnieszka
Rollins, Andrew
Kazil, Jan
Froyd, Karl D.
Ray, Eric A.
Murphy, Daniel M.
Schill, Gregory P.
Peischl, Jeff
Thompson, Chelsea
Bourgeois, Ilann
Ryerson, Thomas
Diskin, Glenn
DiGangi, Joshua P.
Blake, Donald R.
Bui, Thao Paul V.
Dollner, Maximilian
Weinzierl, Bernadett
Brock, Charles A.

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Large hemispheric difference in ultrafine aerosol concentrations in the lowermost stratosphere at mid and high latitudes

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Other Objects (12)

Large hemispheric difference in nucleation mode aerosol concentrations in the lowermost stratosphere at mid-and high latitudes

Indications of thin cirrus clouds in the stratosphere at mid-latitudes

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Chemical evidence of inter-hemispheric air mass intrusion into the Northern Hemisphere mid-latitudes

Comparison of Inorganic Chlorine in the Southern Hemispheric lowermost stratosphere during Late Winter 2019

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Asymmetry and pathways of inter-hemispheric transport in the upper troposphere and lower stratosphere

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Large hemispheric difference in nucleation mode aerosol concentrations in the lowermost stratosphere at mid-and high latitudes

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