Ocean Heat Content Anomalies in the North Atlantic based on mapping Argo data using local Gaussian processes defined over space
Monthly Ocean Heat Content Anomalies (OHCA) in the top 2000 dbar of the ocean are calculated (during 2005-2022, in the North Atlantic, north of 20N) subtracting the time mean over the period 2005-2021 from the monthly time series of OHC. OHC fields are mapped using a locally stationary Gaussian proc...
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ftzenodo:oai:zenodo.org:10183869 2024-09-15T18:22:24+00:00 Ocean Heat Content Anomalies in the North Atlantic based on mapping Argo data using local Gaussian processes defined over space Giglio, Donata Sukianto, Thea Kuusela, Mikael 2023-11-22 https://doi.org/10.5281/zenodo.10183869 unknown Zenodo https://doi.org/10.5281/zenodo.10183868 https://doi.org/10.5281/zenodo.10183869 oai:zenodo.org:10183869 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Ocean Heat Content Argo info:eu-repo/semantics/other 2023 ftzenodo https://doi.org/10.5281/zenodo.1018386910.5281/zenodo.10183868 2024-07-26T11:54:13Z Monthly Ocean Heat Content Anomalies (OHCA) in the top 2000 dbar of the ocean are calculated (during 2005-2022, in the North Atlantic, north of 20N) subtracting the time mean over the period 2005-2021 from the monthly time series of OHC. OHC fields are mapped using a locally stationary Gaussian process (defined over space) with data-driven decorrelation scales (Kuusela and Stein, 2018). A linear time trend was included in the estimate of the mean field (along with spatial terms and harmonics for the annual cycle). In this product, mapping is done in latitude and longitude with monthly subsets of data. Mapping is done separately for different vertical sections: 15-20 dbar, 15-300 dbar, 300-700 dbar, 700-1850 dbar, 1800-1850 dbar. The 15-20 dbar (1800-1850 dbar) section is used to estimate OHCA for 0-15 dbar (1850-2000 dbar), where observations are sparser. Different vertical sections are combined to estimate global OHCA for 0-2000 dbar. Regions of the ocean that are shallower than 300 m or are not sufficiently well sampled by the Argo array are not included. Other/Unknown Material North Atlantic Zenodo |
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Ocean Heat Content Argo |
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Ocean Heat Content Argo Giglio, Donata Sukianto, Thea Kuusela, Mikael Ocean Heat Content Anomalies in the North Atlantic based on mapping Argo data using local Gaussian processes defined over space |
topic_facet |
Ocean Heat Content Argo |
description |
Monthly Ocean Heat Content Anomalies (OHCA) in the top 2000 dbar of the ocean are calculated (during 2005-2022, in the North Atlantic, north of 20N) subtracting the time mean over the period 2005-2021 from the monthly time series of OHC. OHC fields are mapped using a locally stationary Gaussian process (defined over space) with data-driven decorrelation scales (Kuusela and Stein, 2018). A linear time trend was included in the estimate of the mean field (along with spatial terms and harmonics for the annual cycle). In this product, mapping is done in latitude and longitude with monthly subsets of data. Mapping is done separately for different vertical sections: 15-20 dbar, 15-300 dbar, 300-700 dbar, 700-1850 dbar, 1800-1850 dbar. The 15-20 dbar (1800-1850 dbar) section is used to estimate OHCA for 0-15 dbar (1850-2000 dbar), where observations are sparser. Different vertical sections are combined to estimate global OHCA for 0-2000 dbar. Regions of the ocean that are shallower than 300 m or are not sufficiently well sampled by the Argo array are not included. |
format |
Other/Unknown Material |
author |
Giglio, Donata Sukianto, Thea Kuusela, Mikael |
author_facet |
Giglio, Donata Sukianto, Thea Kuusela, Mikael |
author_sort |
Giglio, Donata |
title |
Ocean Heat Content Anomalies in the North Atlantic based on mapping Argo data using local Gaussian processes defined over space |
title_short |
Ocean Heat Content Anomalies in the North Atlantic based on mapping Argo data using local Gaussian processes defined over space |
title_full |
Ocean Heat Content Anomalies in the North Atlantic based on mapping Argo data using local Gaussian processes defined over space |
title_fullStr |
Ocean Heat Content Anomalies in the North Atlantic based on mapping Argo data using local Gaussian processes defined over space |
title_full_unstemmed |
Ocean Heat Content Anomalies in the North Atlantic based on mapping Argo data using local Gaussian processes defined over space |
title_sort |
ocean heat content anomalies in the north atlantic based on mapping argo data using local gaussian processes defined over space |
publisher |
Zenodo |
publishDate |
2023 |
url |
https://doi.org/10.5281/zenodo.10183869 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://doi.org/10.5281/zenodo.10183868 https://doi.org/10.5281/zenodo.10183869 oai:zenodo.org:10183869 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.1018386910.5281/zenodo.10183868 |
_version_ |
1810462187098996736 |