A 1/16° eddying simulation of the global NEMO sea-ice–ocean system

Iovino, Doroteaciro; Masina, Simona; Storto, Andrea; Cipollone, Andrea; Stepanov, Vladimir N.

doi:10.5194/gmd-9-2665-2016

Articles | Volume 9, issue 8

https://doi.org/10.5194/gmd-9-2665-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Nucleus for European Modelling of the Ocean - NEMO

https://doi.org/10.5194/gmd-9-2665-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 9, issue 8

Model evaluation paper

|

12 Aug 2016

Model evaluation paper |

| 12 Aug 2016

A 1/16° eddying simulation of the global NEMO sea-ice–ocean system

Doroteaciro Iovino, Simona Masina, Andrea Storto, Andrea Cipollone, and Vladimir N. Stepanov

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Views and downloads (calculated since 18 Jan 2016)

Month	HTML	PDF	XML	Total
Jan 2016	92	53	1	146
Feb 2016	34	64	2	100
Mar 2016	31	19	0	50
Apr 2016	22	7	0	29
May 2016	14	4	0	18
Jun 2016	6	12	0	18
Jul 2016	11	6	0	17
Aug 2016	63	167	2	232
Sep 2016	37	26	3	66
Oct 2016	23	27	4	54
Nov 2016	24	33	13	70
Dec 2016	24	28	12	64
Jan 2017	49	61	16	126
Feb 2017	29	31	12	72
Mar 2017	44	22	10	76
Apr 2017	48	31	18	97
May 2017	60	53	20	133
Jun 2017	49	30	15	94
Jul 2017	27	12	2	41
Aug 2017	11	14	1	26
Sep 2017	17	18	2	37
Oct 2017	19	15	0	34
Nov 2017	12	17	2	31
Dec 2017	12	17	1	30
Jan 2018	22	28	1	51
Feb 2018	33	27	1	61
Mar 2018	22	35	1	58
Apr 2018	11	30	0	41
May 2018	21	30	1	52
Jun 2018	18	31	0	49
Jul 2018	8	31	1	40
Aug 2018	20	36	0	56
Sep 2018	19	23	0	42
Oct 2018	19	31	1	51
Nov 2018	27	36	4	67
Dec 2018	15	27	1	43
Jan 2019	8	22	0	30
Feb 2019	7	13	0	20
Mar 2019	8	22	0	30
Apr 2019	12	29	1	42
May 2019	8	21	0	29
Jun 2019	11	40	0	51
Jul 2019	21	33	1	55
Aug 2019	15	26	0	41
Sep 2019	12	20	1	33
Oct 2019	13	18	0	31
Nov 2019	7	20	0	27
Dec 2019	7	20	2	29
Jan 2020	14	8	3	25
Feb 2020	14	8	0	22
Mar 2020	8	12	1	21
Apr 2020	6	8	0	14
May 2020	8	7	2	17
Jun 2020	16	14	2	32
Jul 2020	46	70	24	140
Aug 2020	7	6	0	13
Sep 2020	25	8	0	33
Oct 2020	10	6	2	18
Nov 2020	8	9	0	17
Dec 2020	16	12	0	28
Jan 2021	19	11	0	30
Feb 2021	15	12	0	27
Mar 2021	14	8	0	22
Apr 2021	13	15	1	29
May 2021	9	7	0	16
Jun 2021	10	8	0	18
Jul 2021	7	14	0	21
Aug 2021	15	10	1	26
Sep 2021	19	16	1	36
Oct 2021	8	38	0	46
Nov 2021	19	32	1	52
Dec 2021	14	8	1	23
Jan 2022	21	21	0	42
Feb 2022	15	14	1	30
Mar 2022	18	10	0	28
Apr 2022	37	8	2	47
May 2022	42	8	0	50
Jun 2022	48	14	0	62
Jul 2022	32	8	1	41
Aug 2022	45	13	2	60
Sep 2022	35	6	1	42
Oct 2022	43	5	1	49
Nov 2022	50	16	3	69
Dec 2022	45	17	4	66
Jan 2023	41	18	2	61
Feb 2023	48	31	4	83
Mar 2023	56	16	0	72
Apr 2023	47	12	0	59
May 2023	51	11	0	62
Jun 2023	64	7	1	72
Jul 2023	39	14	0	53
Aug 2023	40	10	2	52
Sep 2023	44	17	1	62
Oct 2023	104	10	3	117
Nov 2023	111	1	0	112
Dec 2023	50	9	2	61
Jan 2024	42	7	1	50
Feb 2024	40	9	2	51
Mar 2024	44	24	0	68
Apr 2024	56	11	7	74
May 2024	26	14	6	46
Jun 2024	15	14	1	30
Jul 2024	15	13	3	31
Aug 2024	30	4	3	37
Sep 2024	9	9	0	18
Oct 2024	13	8	0	21
Nov 2024	11	7	2	20
Dec 2024	23	18	1	42
Jan 2025	12	3	0	15
Feb 2025	32	19	5	56
Mar 2025	30	12	1	43
Apr 2025	24	13	0	37
May 2025	28	3	1	32
Jun 2025	36	33	2	71
Jul 2025	43	33	3	79
Aug 2025	21	30	3	54
Sep 2025	30	27	3	60
Oct 2025	39	25	4	68
Nov 2025	41	20	7	68

Cumulative views and downloads (calculated since 18 Jan 2016)

Month	HTML	PDF	XML	Total
Jan 2016	92	53	1	146
Feb 2016	34	64	2	100
Mar 2016	31	19	0	50
Apr 2016	22	7	0	29
May 2016	14	4	0	18
Jun 2016	6	12	0	18
Jul 2016	11	6	0	17
Aug 2016	63	167	2	232
Sep 2016	37	26	3	66
Oct 2016	23	27	4	54
Nov 2016	24	33	13	70
Dec 2016	24	28	12	64
Jan 2017	49	61	16	126
Feb 2017	29	31	12	72
Mar 2017	44	22	10	76
Apr 2017	48	31	18	97
May 2017	60	53	20	133
Jun 2017	49	30	15	94
Jul 2017	27	12	2	41
Aug 2017	11	14	1	26
Sep 2017	17	18	2	37
Oct 2017	19	15	0	34
Nov 2017	12	17	2	31
Dec 2017	12	17	1	30
Jan 2018	22	28	1	51
Feb 2018	33	27	1	61
Mar 2018	22	35	1	58
Apr 2018	11	30	0	41
May 2018	21	30	1	52
Jun 2018	18	31	0	49
Jul 2018	8	31	1	40
Aug 2018	20	36	0	56
Sep 2018	19	23	0	42
Oct 2018	19	31	1	51
Nov 2018	27	36	4	67
Dec 2018	15	27	1	43
Jan 2019	8	22	0	30
Feb 2019	7	13	0	20
Mar 2019	8	22	0	30
Apr 2019	12	29	1	42
May 2019	8	21	0	29
Jun 2019	11	40	0	51
Jul 2019	21	33	1	55
Aug 2019	15	26	0	41
Sep 2019	12	20	1	33
Oct 2019	13	18	0	31
Nov 2019	7	20	0	27
Dec 2019	7	20	2	29
Jan 2020	14	8	3	25
Feb 2020	14	8	0	22
Mar 2020	8	12	1	21
Apr 2020	6	8	0	14
May 2020	8	7	2	17
Jun 2020	16	14	2	32
Jul 2020	46	70	24	140
Aug 2020	7	6	0	13
Sep 2020	25	8	0	33
Oct 2020	10	6	2	18
Nov 2020	8	9	0	17
Dec 2020	16	12	0	28
Jan 2021	19	11	0	30
Feb 2021	15	12	0	27
Mar 2021	14	8	0	22
Apr 2021	13	15	1	29
May 2021	9	7	0	16
Jun 2021	10	8	0	18
Jul 2021	7	14	0	21
Aug 2021	15	10	1	26
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Oct 2021	8	38	0	46
Nov 2021	19	32	1	52
Dec 2021	14	8	1	23
Jan 2022	21	21	0	42
Feb 2022	15	14	1	30
Mar 2022	18	10	0	28
Apr 2022	37	8	2	47
May 2022	42	8	0	50
Jun 2022	48	14	0	62
Jul 2022	32	8	1	41
Aug 2022	45	13	2	60
Sep 2022	35	6	1	42
Oct 2022	43	5	1	49
Nov 2022	50	16	3	69
Dec 2022	45	17	4	66
Jan 2023	41	18	2	61
Feb 2023	48	31	4	83
Mar 2023	56	16	0	72
Apr 2023	47	12	0	59
May 2023	51	11	0	62
Jun 2023	64	7	1	72
Jul 2023	39	14	0	53
Aug 2023	40	10	2	52
Sep 2023	44	17	1	62
Oct 2023	104	10	3	117
Nov 2023	111	1	0	112
Dec 2023	50	9	2	61
Jan 2024	42	7	1	50
Feb 2024	40	9	2	51
Mar 2024	44	24	0	68
Apr 2024	56	11	7	74
May 2024	26	14	6	46
Jun 2024	15	14	1	30
Jul 2024	15	13	3	31
Aug 2024	30	4	3	37
Sep 2024	9	9	0	18
Oct 2024	13	8	0	21
Nov 2024	11	7	2	20
Dec 2024	23	18	1	42
Jan 2025	12	3	0	15
Feb 2025	32	19	5	56
Mar 2025	30	12	1	43
Apr 2025	24	13	0	37
May 2025	28	3	1	32
Jun 2025	36	33	2	71
Jul 2025	43	33	3	79
Aug 2025	21	30	3	54
Sep 2025	30	27	3	60
Oct 2025	39	25	4	68
Nov 2025	41	20	7	68

Latest update: 01 Dec 2025

Short summary

An 11-year simulation of a global eddying ocean (1/16) configuration is presented. Model performance is evaluated against observations and a twin 1/4 configuration. The model realistically represents the variability at upper and intermediate depths, the position and strength of the surface circulation, and exchanges of mass through key passages. Sea ice properties are close to satellite observations. This simulation constitutes the groundwork for future applications to short range ocean forecasting.