A three-dimensional model study of methanesulphonic acid to non sea salt sulphate ratio at mid and high-southern latitudes

H. Castebrunet; P. Martinerie; C. Genthon; E. Cosme

doi:10.5194/acp-9-9449-2009

A three-dimensional model study of methanesulphonic acid to non sea salt sulphate ratio at mid and high-southern latitudes

H. Castebrunet
, P. Martinerie
, C. Genthon
, E. Cosme

Research output: Contribution to journal › Article › peer-review

Abstract

The Antarctic and sub-Antarctic methanesulphonic acid (MSA) to non sea salt sulphate (nssSO₄) ratio is simulated with the Laboratorie de Mééorologie.

Original language	English
Pages (from-to)	9449-9469
Number of pages	21
Journal	Atmospheric Chemistry and Physics
Volume	9
Issue number	24
DOIs	https://doi.org/10.5194/acp-9-9449-2009
Publication status	Published - 1 Jan 2009
Externally published	Yes

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title = "A three-dimensional model study of methanesulphonic acid to non sea salt sulphate ratio at mid and high-southern latitudes",

abstract = "The Antarctic and sub-Antarctic methanesulphonic acid (MSA) to non sea salt sulphate (nssSO4) ratio is simulated with the Laboratorie de M{\'e}{\'e}orologie.",

author = "H. Castebrunet and P. Martinerie and C. Genthon and E. Cosme",

year = "2009",

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doi = "10.5194/acp-9-9449-2009",

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AU - Castebrunet, H.

AU - Martinerie, P.

AU - Genthon, C.

AU - Cosme, E.

PY - 2009/1/1

Y1 - 2009/1/1

N2 - The Antarctic and sub-Antarctic methanesulphonic acid (MSA) to non sea salt sulphate (nssSO4) ratio is simulated with the Laboratorie de Mééorologie.

AB - The Antarctic and sub-Antarctic methanesulphonic acid (MSA) to non sea salt sulphate (nssSO4) ratio is simulated with the Laboratorie de Mééorologie.

U2 - 10.5194/acp-9-9449-2009

DO - 10.5194/acp-9-9449-2009

M3 - Article

AN - SCOPUS:72849142079

SN - 1680-7316

VL - 9

SP - 9449

EP - 9469

JO - Atmospheric Chemistry and Physics

JF - Atmospheric Chemistry and Physics

IS - 24

ER -

A three-dimensional model study of methanesulphonic acid to non sea salt sulphate ratio at mid and high-southern latitudes

Abstract

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