Upper stratospheric ozone decrease events due to a positive feedback between ozone and the ozone dissociation rate

Sonnemann, G. R.; Hartogh, P.

doi:https://doi.org/10.5194/npg-16-409-2009

Articles | Volume 16, issue 3

https://doi.org/10.5194/npg-16-409-2009

© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/npg-16-409-2009

© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 16, issue 3

19 Jun 2009

| 19 Jun 2009

Upper stratospheric ozone decrease events due to a positive feedback between ozone and the ozone dissociation rate

G. R. Sonnemann and P. Hartogh

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Total article views: 1,769 (including HTML, PDF, and XML)

HTML	PDF	XML	Total	BibTeX	EndNote
883	770	116	1,769	138	95

HTML: 883
PDF: 770
XML: 116
Total: 1,769
BibTeX: 138
EndNote: 95

Views and downloads (calculated since 01 Feb 2013)

Month	HTML	PDF	XML	Total
Feb 2013	4	8	1	13
Mar 2013	1	10	1	12
Apr 2013	2	9	0	11
May 2013	4	18	1	23
Jun 2013	3	9	0	12
Jul 2013	2	12	0	14
Aug 2013	10	4	0	14
Sep 2013	11	0	11
Oct 2013	6	11	0	17
Nov 2013	10	0	10
Dec 2013	3	8	1	12
Jan 2014	3	11	4	18
Feb 2014	4	10	4	18
Mar 2014	11	7	1	19
Apr 2014	2	9	0	11
May 2014	5	7	0	12
Jun 2014	2	6	2	10
Jul 2014	1	17	0	18
Aug 2014	2	14	1	17
Sep 2014	3	10	0	13
Oct 2014	1	13	2	16
Nov 2014	4	10	1	15
Dec 2014	2	15	1	18
Jan 2015	3	0	3
Feb 2015	6	3	0	9
Mar 2015	8	1	0	9
Apr 2015	10	1	1	12
May 2015	6	5	0	11
Jun 2015	23	5	0	28
Jul 2015	17	1	0	18
Aug 2015	4	7	0	11
Sep 2015	2	0	2
Oct 2015	10	0	10
Nov 2015	8	3	0	11
Dec 2015	2	3	0	5
Jan 2016	12	5	0	17
Feb 2016	5	7	0	12
Mar 2016	9	3	1	13
Apr 2016	7	2	0	9
May 2016	5	1	0	6
Jun 2016	4	1	0	5
Jul 2016	5	3	1	9
Aug 2016	5	3	0	8
Sep 2016	5	2	0	7
Oct 2016	3	0	3
Nov 2016	4	2	0	6
Dec 2016	3	3	0	6
Jan 2017	2	0	2
Feb 2017	5	1	0	6
Mar 2017	9	4	0	13
Apr 2017	9	9	1	19
May 2017	13	2	0	15
Jun 2017	13	2	0	15
Jul 2017	10	5	0	15
Aug 2017	4	3	2	9
Sep 2017	7	5	0	12
Oct 2017	4	3	0	7
Nov 2017	3	6	0	9
Dec 2017	10	6	3	19
Jan 2018	13	13	7	33
Feb 2018	10	6	2	18
Mar 2018	8	6	3	17
Apr 2018	8	8	4	20
May 2018	9	7	3	19
Jun 2018	10	8	4	22
Jul 2018	13	6	4	23
Aug 2018	11	4	2	17
Sep 2018	11	5	4	20
Oct 2018	10	10	4	24
Nov 2018	7	8	0	15
Dec 2018	7	3	1	11
Jan 2019	15	5	2	22
Feb 2019	15	6	2	23
Mar 2019	10	6	1	17
Apr 2019	9	6	1	16
May 2019	10	9	3	22
Jun 2019	4	6	1	11
Jul 2019	2	4	0	6
Aug 2019	1	2	0	3
Sep 2019	2	2	0	4
Oct 2019	1	2	0	3
Nov 2019	5	6	0	11
Dec 2019	1	10	0	11
Jan 2020	7	10	3	20
Feb 2020	2	3	0	5
Mar 2020	3	3	2	8
Apr 2020	2	5	0	7
May 2020	5	3	0	8
Jun 2020	12	11	0	23
Jul 2020	18	10	10	38
Aug 2020	7	5	5	17
Sep 2020	10	6	0	16
Oct 2020	10	11	1	22
Nov 2020	3	8	0	11
Dec 2020	9	6	0	15
Jan 2021	17	4	0	21
Feb 2021	7	4	0	11
Mar 2021	7	6	0	13
Apr 2021	3	5	0	8
May 2021	3	4	0	7
Jun 2021	4	2	0	6
Jul 2021	3	9	0	12
Aug 2021	2	1	0	3
Sep 2021	10	6	0	16
Oct 2021	4	18	0	22
Nov 2021	7	14	0	21
Dec 2021	8	5	0	13
Jan 2022	6	13	0	19
Feb 2022	4	6	1	11
Mar 2022	4	4	0	8
Apr 2022	1	4	0	5
May 2022	5	3	1	9
Jun 2022	3	2	1	6
Jul 2022	3	4	0	7
Aug 2022	7	3	0	10
Sep 2022	3	2	1	6
Oct 2022	4	1	0	5
Nov 2022	4	6	0	10
Dec 2022	6	5	0	11
Jan 2023	3	3	0	6
Feb 2023	8	6	0	14
Mar 2023	3	3	0	6
Apr 2023	3	1	0	4
May 2023	6	3	2	11
Jun 2023	2	2	0	4
Jul 2023	2	3	0	5
Aug 2023	6	4	1	11
Sep 2023	2	2	0	4
Oct 2023	4	2	0	6
Nov 2023	1	0	1
Dec 2023	6	1	0	7
Jan 2024	1	3	0	4
Feb 2024	3	5	0	8
Mar 2024	1	3	0	4
Apr 2024	7	2	2	11
May 2024	9	4	2	15
Jun 2024	35	6	2	43
Jul 2024	11	4	2	17
Aug 2024	35	3	3	41
Sep 2024	3	1	0	4

Cumulative views and downloads (calculated since 01 Feb 2013)

Month	HTML	PDF	XML	Total
Feb 2013	4	8	1	13
Mar 2013	1	10	1	12
Apr 2013	2	9	0	11
May 2013	4	18	1	23
Jun 2013	3	9	0	12
Jul 2013	2	12	0	14
Aug 2013	10	4	0	14
Sep 2013	11	0	11
Oct 2013	6	11	0	17
Nov 2013	10	0	10
Dec 2013	3	8	1	12
Jan 2014	3	11	4	18
Feb 2014	4	10	4	18
Mar 2014	11	7	1	19
Apr 2014	2	9	0	11
May 2014	5	7	0	12
Jun 2014	2	6	2	10
Jul 2014	1	17	0	18
Aug 2014	2	14	1	17
Sep 2014	3	10	0	13
Oct 2014	1	13	2	16
Nov 2014	4	10	1	15
Dec 2014	2	15	1	18
Jan 2015	3	0	3
Feb 2015	6	3	0	9
Mar 2015	8	1	0	9
Apr 2015	10	1	1	12
May 2015	6	5	0	11
Jun 2015	23	5	0	28
Jul 2015	17	1	0	18
Aug 2015	4	7	0	11
Sep 2015	2	0	2
Oct 2015	10	0	10
Nov 2015	8	3	0	11
Dec 2015	2	3	0	5
Jan 2016	12	5	0	17
Feb 2016	5	7	0	12
Mar 2016	9	3	1	13
Apr 2016	7	2	0	9
May 2016	5	1	0	6
Jun 2016	4	1	0	5
Jul 2016	5	3	1	9
Aug 2016	5	3	0	8
Sep 2016	5	2	0	7
Oct 2016	3	0	3
Nov 2016	4	2	0	6
Dec 2016	3	3	0	6
Jan 2017	2	0	2
Feb 2017	5	1	0	6
Mar 2017	9	4	0	13
Apr 2017	9	9	1	19
May 2017	13	2	0	15
Jun 2017	13	2	0	15
Jul 2017	10	5	0	15
Aug 2017	4	3	2	9
Sep 2017	7	5	0	12
Oct 2017	4	3	0	7
Nov 2017	3	6	0	9
Dec 2017	10	6	3	19
Jan 2018	13	13	7	33
Feb 2018	10	6	2	18
Mar 2018	8	6	3	17
Apr 2018	8	8	4	20
May 2018	9	7	3	19
Jun 2018	10	8	4	22
Jul 2018	13	6	4	23
Aug 2018	11	4	2	17
Sep 2018	11	5	4	20
Oct 2018	10	10	4	24
Nov 2018	7	8	0	15
Dec 2018	7	3	1	11
Jan 2019	15	5	2	22
Feb 2019	15	6	2	23
Mar 2019	10	6	1	17
Apr 2019	9	6	1	16
May 2019	10	9	3	22
Jun 2019	4	6	1	11
Jul 2019	2	4	0	6
Aug 2019	1	2	0	3
Sep 2019	2	2	0	4
Oct 2019	1	2	0	3
Nov 2019	5	6	0	11
Dec 2019	1	10	0	11
Jan 2020	7	10	3	20
Feb 2020	2	3	0	5
Mar 2020	3	3	2	8
Apr 2020	2	5	0	7
May 2020	5	3	0	8
Jun 2020	12	11	0	23
Jul 2020	18	10	10	38
Aug 2020	7	5	5	17
Sep 2020	10	6	0	16
Oct 2020	10	11	1	22
Nov 2020	3	8	0	11
Dec 2020	9	6	0	15
Jan 2021	17	4	0	21
Feb 2021	7	4	0	11
Mar 2021	7	6	0	13
Apr 2021	3	5	0	8
May 2021	3	4	0	7
Jun 2021	4	2	0	6
Jul 2021	3	9	0	12
Aug 2021	2	1	0	3
Sep 2021	10	6	0	16
Oct 2021	4	18	0	22
Nov 2021	7	14	0	21
Dec 2021	8	5	0	13
Jan 2022	6	13	0	19
Feb 2022	4	6	1	11
Mar 2022	4	4	0	8
Apr 2022	1	4	0	5
May 2022	5	3	1	9
Jun 2022	3	2	1	6
Jul 2022	3	4	0	7
Aug 2022	7	3	0	10
Sep 2022	3	2	1	6
Oct 2022	4	1	0	5
Nov 2022	4	6	0	10
Dec 2022	6	5	0	11
Jan 2023	3	3	0	6
Feb 2023	8	6	0	14
Mar 2023	3	3	0	6
Apr 2023	3	1	0	4
May 2023	6	3	2	11
Jun 2023	2	2	0	4
Jul 2023	2	3	0	5
Aug 2023	6	4	1	11
Sep 2023	2	2	0	4
Oct 2023	4	2	0	6
Nov 2023	1	0	1
Dec 2023	6	1	0	7
Jan 2024	1	3	0	4
Feb 2024	3	5	0	8
Mar 2024	1	3	0	4
Apr 2024	7	2	2	11
May 2024	9	4	2	15
Jun 2024	35	6	2	43
Jul 2024	11	4	2	17
Aug 2024	35	3	3	41
Sep 2024	3	1	0	4

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Latest update: 10 Sep 2024

Upper stratospheric ozone decrease events due to a positive feedback between ozone and the ozone dissociation rate

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