eodag/resources/ext_product_types.json
152c152
<         "keywords": "arctic-analysisforecast-phy-tide-002-015,arctic-ocean,coastal-marine-environment,forecast,level-4,marine-resources,marine-safety,near-real-time,oceanographic-geographical-features,sea-surface-elevation,weather-climate-and-seasonal-forecasting,x-sea-water-velocity,y-sea-water-velocity",
---
>         "keywords": "arctic-analysisforecast-phy-tide-002-015,arctic-ocean,coastal-marine-environment,forecast,level-4,marine-resources,marine-safety,near-real-time,numerical-model,oceanographic-geographical-features,sea-surface-elevation,weather-climate-and-seasonal-forecasting,x-sea-water-velocity,y-sea-water-velocity",
4716c4716
<         "keywords": "baltic-sea,coastal-marine-environment,marine-resources,marine-safety,oceanographic-geographical-features,omi-climate-sl-europe-area-averaged-anomalies,sea-surface-height-above-sea-level,weather-climate-and-seasonal-forecasting",
---
>         "keywords": "baltic-sea,coastal-marine-environment,marine-resources,marine-safety,oceanographic-geographical-features,omi-climate-sl-europe-area-averaged-anomalies,satellite-observation,sea-surface-height-above-sea-level,weather-climate-and-seasonal-forecasting",
4791,4792c4791,4792
<         "abstract": null,
<         "doi": null,
---
>         "abstract": "**DEFINITION**\n\nThe ocean monitoring indicator on regional mean sea level is derived from the DUACS delayed-time (DT-2021 version, “my” (multi-year) dataset used when available, “myint” (multi-year interim) used after) sea level anomaly maps from satellite altimetry based on a stable number of altimeters (two) in the satellite constellation. These products are distributed by the Copernicus Climate Change Service and the Copernicus Marine Service (SEALEVEL_GLO_PHY_CLIMATE_L4_MY_008_057).\nThe time series of area averaged anomalies correspond to the area average of the maps in the Irish-Biscay-Iberian (IBI) Sea weighted by the cosine of the latitude (to consider the changing area in each grid with latitude) and by the proportion of ocean in each grid (to consider the coastal areas). The time series are corrected from global TOPEX-A instrumental drift (WCRP Global Sea Level Budget Group, 2018) and regional mean GIA correction (weighted GIA mean of a 27 ensemble model following Spada et Melini, 2019). The time series are adjusted for seasonal annual and semi-annual signals and low-pass filtered at 6 months. Then, the trends/accelerations are estimated on the time series using ordinary least square fit.The trend uncertainty is provided in a 90% confidence interval. It is calculated as the weighted mean uncertainties in the region from Prandi et al., 2021. This estimate only considers errors related to the altimeter observation system (i.e., orbit determination errors, geophysical correction errors and inter-mission bias correction errors). The presence of the interannual signal can strongly influence the trend estimation considering to the altimeter period considered (Wang et al., 2021; Cazenave et al., 2014). The uncertainty linked to this effect is not considered.\n\n**CONTEXT  **\n\nChange in mean sea level is an essential indicator of our evolving climate, as it reflects both the thermal expansion of the ocean in response to its warming and the increase in ocean mass due to the melting of ice sheets and glaciers (WCRP Global Sea Level Budget Group, 2018). At regional scale, sea level does not change homogenously. It is influenced by various other processes, with different spatial and temporal scales, such as local ocean dynamic, atmospheric forcing, Earth gravity and vertical land motion changes (IPCC WGI, 2021). The adverse effects of floods, storms and tropical cyclones, and the resulting losses and damage, have increased as a result of rising sea levels, increasing people and infrastructure vulnerability and food security risks, particularly in low-lying areas and island states (IPCC, 2022a). Adaptation and mitigation measures such as the restoration of mangroves and coastal wetlands, reduce the risks from sea level rise (IPCC, 2022b). \nIn IBI region, the RMSL trend is modulated by decadal variations. As observed over the global ocean, the main actors of the long-term RMSL trend are associated with anthropogenic global/regional warming. Decadal variability is mainly linked to the strengthening or weakening of the Atlantic Meridional Overturning Circulation (AMOC) (e.g. Chafik et al., 2019). The latest is driven by the North Atlantic Oscillation (NAO)  for decadal (20-30y) timescales (e.g. Delworth and Zeng, 2016). Along the European coast, the NAO also influences the along-slope winds dynamic which in return significantly contributes to the local sea level variability observed (Chafik et al., 2019).\n\n**KEY FINDINGS**\n\nOver the [1993/01/01, 2023/07/06] period, the area-averaged sea level in the IBI area rises at a rate of 4.00  0.80 mm/year with an acceleration of 0.14 0.06 mm/year2. This trend estimation is based on the altimeter measurements corrected from the Topex-A drift at the beginning of the time series (Legeais et al., 2020) and global GIA correction (Spada et Melini, 2019) to consider the ongoing movement of land. \n\n**DOI (product):** \nhttps://doi.org/10.48670/moi-00252\n\n**References:**\n\n* Cazenave, A., Dieng, H.-B., Meyssignac, B., von Schuckmann, K., Decharme, B., and Berthier, E.: The rate of sea-level rise, Nat. Clim. Change, 4, 358–361, https://doi.org/10.1038/nclimate2159, 2014.\n* Chafik, L., Nilsen, J. E. Ø., Dangendorf, S., Reverdin, G., and Frederikse, T.: North Atlantic Ocean Circulation and Decadal Sea Level Change During the Altimetry Era, Sci. Rep., 9, 1041, https://doi.org/10.1038/s41598-018-37603-6, 2019.\n* Delworth, T. L. and Zeng, F.: The Impact of the North Atlantic Oscillation on Climate through Its Influence on the Atlantic Meridional Overturning Circulation, J. Clim., 29, 941–962, https://doi.org/10.1175/JCLI-D-15-0396.1, 2016.\n* Horwath, M., Gutknecht, B. D., Cazenave, A., Palanisamy, H. K., Marti, F., Marzeion, B., Paul, F., Le Bris, R., Hogg, A. E., Otosaka, I., Shepherd, A., Döll, P., Cáceres, D., Müller Schmied, H., Johannessen, J. A., Nilsen, J. E. Ø., Raj, R. P., Forsberg, R., Sandberg Sørensen, L., Barletta, V. R., Simonsen, S. B., Knudsen, P., Andersen, O. B., Ranndal, H., Rose, S. K., Merchant, C. J., Macintosh, C. R., von Schuckmann, K., Novotny, K., Groh, A., Restano, M., and Benveniste, J.: Global sea-level budget and ocean-mass budget, with a focus on advanced data products and uncertainty characterisation, Earth Syst. Sci. Data, 14, 411–447, https://doi.org/10.5194/essd-14-411-2022, 2022.\n* IPCC: AR6 Synthesis Report: Climate Change 2022, 2022a.\n* IPCC: Summary for Policymakers [H.-O. Pörtner, D.C. Roberts, E.S. Poloczanska, K. Mintenbeck, M. Tignor, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem (eds.)]. In: Climate Change 2022: Impacts, Adaptation, and Vulnerability. Contribution of Working Group II to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [H.-O. Pörtner, D.C. Roberts, M. Tignor, E.S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)], 2022b.\n* IPCC: Summary for Policymakers. In: Climate Change 2022: Mitigation of Climate Change. Contribution of Working Group III to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [P.R. Shukla, J. Skea, R. Slade, A. Al Khourdajie, R. van Diemen, D. McCollum, M. Pathak, S. Some, P. Vyas, R. Fradera, M. Belkacemi, A. Hasija, G. Lisboa, S. Luz, J. Malley, (eds.)], , https://doi.org/10.1017/9781009157926.001, 2022c.\n* IPCC WGI: Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change, 2021.\n* IPCC WGII: Climate Change 2021: Impacts, Adaptation and Vulnerability; Summary for Policemakers. Contribution of Working Group II to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change, 2021.\n* Legeais, J. F., Llowel, W., Melet, A., and Meyssignac, B.: Evidence of the TOPEX-A altimeter instrumental anomaly and acceleration of the global mean sea level, Copernic. Mar. Serv. Ocean State Rep. Issue 4, 13, s77–s82, https://doi.org/10.1080/1755876X.2021.1946240, 2020.\n* Peltier, W. R.: GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE, Annu. Rev. Earth Planet. Sci., 32, 111–149, https://doi.org/10.1146/annurev.earth.32.082503.144359, 2004.\n* Prandi, P., Meyssignac, B., Ablain, M., Spada, G., Ribes, A., and Benveniste, J.: Local sea level trends, accelerations and uncertainties over 1993–2019, Sci. Data, 8, 1, https://doi.org/10.1038/s41597-020-00786-7, 2021.\n* Wang, J., Church, J. A., Zhang, X., and Chen, X.: Reconciling global mean and regional sea level change in projections and observations, Nat. Commun., 12, 990, https://doi.org/10.1038/s41467-021-21265-6, 2021.\n* WCRP Global Sea Level Budget Group: Global sea-level budget 1993–present, Earth Syst. Sci. Data, 10, 1551–1590, https://doi.org/10.5194/essd-10-1551-2018, 2018.\n",
>         "doi": "10.48670/moi-00252",
4794,4795c4794,4795
<         "keywords": ",omi-climate-sl-ibi-area-averaged-anomalies",
<         "license": null,
---
>         "keywords": "coastal-marine-environment,iberian-biscay-irish-seas,marine-resources,marine-safety,multi-year,oceanographic-geographical-features,omi-climate-sl-ibi-area-averaged-anomalies,satellite-observation,sea-surface-height-above-sea-level,weather-climate-and-seasonal-forecasting",
>         "license": "proprietary",
4800,4801c4800,4816
<         "providers": [],
<         "title": null
---
>         "providers": [
>           {
>             "name": "CLS (France)",
>             "roles": [
>               "producer"
>             ]
>           },
>           {
>             "name": "Copernicus Marine Service",
>             "roles": [
>               "host",
>               "processor"
>             ],
>             "url": "https://marine.copernicus.eu"
>           }
>         ],
>         "title": "Atlantic Iberian Biscay Mean Sea Level time series and trend from Observations Reprocessing"
6403c6418
<         "keywords": "black-sea,coastal-marine-environment,invariant,level-4,marine-resources,marine-safety,oceanographic-geographical-features,sea-surface-height-above-geoid,sealevel-blk-phy-mdt-l4-static-008-067,weather-climate-and-seasonal-forecasting",
---
>         "keywords": "black-sea,coastal-marine-environment,invariant,level-4,marine-resources,marine-safety,oceanographic-geographical-features,satellite-observation,sea-surface-height-above-geoid,sealevel-blk-phy-mdt-l4-static-008-067,weather-climate-and-seasonal-forecasting",
6683c6698
<         "keywords": "arctic-ocean,baltic-sea,coastal-marine-environment,global-ocean,iberian-biscay-irish-seas,invariant,level-4,marine-resources,marine-safety,north-west-shelf-seas,oceanographic-geographical-features,sea-surface-height-above-geoid,sealevel-glo-phy-mdt-008-063,weather-climate-and-seasonal-forecasting",
---
>         "keywords": "arctic-ocean,baltic-sea,coastal-marine-environment,global-ocean,iberian-biscay-irish-seas,invariant,level-4,marine-resources,marine-safety,north-west-shelf-seas,oceanographic-geographical-features,satellite-observation,sea-surface-height-above-geoid,sealevel-glo-phy-mdt-008-063,weather-climate-and-seasonal-forecasting",
6739c6754
<         "keywords": "coastal-marine-environment,invariant,level-4,marine-resources,marine-safety,mediterranean-sea,oceanographic-geographical-features,sea-surface-height-above-geoid,sealevel-med-phy-mdt-l4-static-008-066,weather-climate-and-seasonal-forecasting",
---
>         "keywords": "coastal-marine-environment,invariant,level-4,marine-resources,marine-safety,mediterranean-sea,oceanographic-geographical-features,satellite-observation,sea-surface-height-above-geoid,sealevel-med-phy-mdt-l4-static-008-066,weather-climate-and-seasonal-forecasting",
7495c7510
<         "keywords": "arctic-ocean,baltic-sea,black-sea,global-ocean,iberian-biscay-irish-seas,level-3,mediterranean-sea,north-west-shelf-seas,oceanographic-geographical-features,sea-surface-wave-from-direction-at-variance-spectral-density-maximum,sea-surface-wave-period-at-variance-spectral-density-maximum,sea-surface-wave-significant-height,wave-glo-phy-spc-l3-nrt-014-009,wave-spectrum",
---
>         "keywords": "arctic-ocean,baltic-sea,black-sea,global-ocean,iberian-biscay-irish-seas,level-3,mediterranean-sea,north-west-shelf-seas,oceanographic-geographical-features,satellite-observation,sea-surface-wave-from-direction-at-variance-spectral-density-maximum,sea-surface-wave-period-at-variance-spectral-density-maximum,sea-surface-wave-significant-height,wave-glo-phy-spc-l3-nrt-014-009,wave-spectrum",
7691c7706
<         "keywords": "eastward-wind,level-4,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,status-flag,time,wind-arc-phy-hr-l3-nrt-012-100,wind-speed,wind-to-direction",
---
>         "keywords": "arctic-ocean,eastward-wind,level-3,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,satellite-observation,status-flag,time,wind-arc-phy-hr-l3-nrt-012-100,wind-speed,wind-to-direction",
7696c7711
<         "processingLevel": "Level 4",
---
>         "processingLevel": "Level 3",
7719c7734
<         "keywords": "eastward-wind,level-3,near-real-time,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,status-flag,time,wind-atl-phy-hr-l3-nrt-012-101,wind-speed,wind-to-direction",
---
>         "keywords": "eastward-wind,iberian-biscay-irish-seas,level-3,near-real-time,north-west-shelf-seas,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,satellite-observation,status-flag,time,wind-atl-phy-hr-l3-nrt-012-101,wind-speed,wind-to-direction",
7747c7762
<         "keywords": "eastward-wind,level-3,near-real-time,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,status-flag,time,wind-bal-phy-hr-l3-nrt-012-102,wind-speed,wind-to-direction",
---
>         "keywords": "baltic-sea,eastward-wind,level-3,near-real-time,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,satellite-observation,status-flag,time,wind-bal-phy-hr-l3-nrt-012-102,wind-speed,wind-to-direction",
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<         "keywords": "eastward-wind,level-3,near-real-time,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,status-flag,time,wind-blk-phy-hr-l3-nrt-012-103,wind-speed,wind-to-direction",
---
>         "keywords": "black-sea,eastward-wind,level-3,near-real-time,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,satellite-observation,status-flag,time,wind-blk-phy-hr-l3-nrt-012-103,wind-speed,wind-to-direction",
7943c7958
<         "keywords": "eastward-wind,level-3,near-real-time,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,status-flag,time,wind-med-phy-hr-l3-nrt-012-104,wind-speed,wind-to-direction",
---
>         "keywords": "eastward-wind,level-3,mediterranean-sea,near-real-time,northward-wind,oceanographic-geographical-features,quality-flag,quality-flag-wind-speed,satellite-observation,status-flag,time,wind-med-phy-hr-l3-nrt-012-104,wind-speed,wind-to-direction",