Changes
On October 22, 2024, 5:52:56 PM UTC,
-
Added resource LOCO2_10_MCTD_2656_3003m_raw.asc to Hydrography and velocity data from the Long-term Ocean Circulation Observations (LOCO) mooring in the central Irminger Sea: Deployment ten (LOCO2_10) August 2012 to July 2014
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| 2 | "author": null, | 2 | "author": null, | ||
| 3 | "author_email": null, | 3 | "author_email": null, | ||
| 4 | "code": "7b.b.ng", | 4 | "code": "7b.b.ng", | ||
| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "25cdedd0-cb90-4e47-bf9e-6215cafb2c2d", | 6 | "creator_user_id": "25cdedd0-cb90-4e47-bf9e-6215cafb2c2d", | ||
| 7 | "creators": "[{\"firstname\":\"Marieke Femke\",\"lastname\":\"de | 7 | "creators": "[{\"firstname\":\"Marieke Femke\",\"lastname\":\"de | ||
| 8 | Jong\",\"orcid\":\"0000-0001-5683-0570\",\"affiliation\":\"Royal | 8 | Jong\",\"orcid\":\"0000-0001-5683-0570\",\"affiliation\":\"Royal | ||
| 9 | Netherlands Institute for Sea | 9 | Netherlands Institute for Sea | ||
| 10 | ingauthor\":true,\"contactemailaddress\":\"femke.de.jong@nioz.nl\"}]", | 10 | ingauthor\":true,\"contactemailaddress\":\"femke.de.jong@nioz.nl\"}]", | ||
| 11 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.ng", | 11 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.ng", | ||
| 12 | "dates": "[{\"datefrom\":\"2012-08-02 | 12 | "dates": "[{\"datefrom\":\"2012-08-02 | ||
| 13 | 00:00:00.000\",\"dateto\":\"2014-07-26 | 13 | 00:00:00.000\",\"dateto\":\"2014-07-26 | ||
| 14 | 00:00:00.000\",\"type\":\"collected\",\"information\":null}]", | 14 | 00:00:00.000\",\"type\":\"collected\",\"information\":null}]", | ||
| 15 | "deposit_date": "2023-12-01", | 15 | "deposit_date": "2023-12-01", | ||
| 16 | "depositor": "Femke de Jong", | 16 | "depositor": "Femke de Jong", | ||
| 17 | "distribution_date": "2023-12-01", | 17 | "distribution_date": "2023-12-01", | ||
| 18 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 18 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 19 | Institute for Sea Research)", | 19 | Institute for Sea Research)", | ||
| 20 | "doi_date_published": "2023-12-06", | 20 | "doi_date_published": "2023-12-06", | ||
| 21 | "funding_references": | 21 | "funding_references": | ||
| 22 | "[{\"name\":\"NWO\",\"awardnumber\":null,\"awardtitle\":\"Long-term | 22 | "[{\"name\":\"NWO\",\"awardnumber\":null,\"awardtitle\":\"Long-term | ||
| 23 | Ocean-Climate Observations (LOCO)\",\"formatted\":\"NWO - - Long-term | 23 | Ocean-Climate Observations (LOCO)\",\"formatted\":\"NWO - - Long-term | ||
| 24 | Ocean-Climate Observations | 24 | Ocean-Climate Observations | ||
| 25 | },{\"name\":\"EU\",\"awardnumber\":\"GA212643\",\"awardtitle\":\"THOR: | 25 | },{\"name\":\"EU\",\"awardnumber\":\"GA212643\",\"awardtitle\":\"THOR: | ||
| 26 | Thermohaline Overturning \u2013 at | 26 | Thermohaline Overturning \u2013 at | ||
| 27 | "awardnumber\":\"308299\",\"awardtitle\":\"NACLIM\",\"formatted\":\"EU | 27 | "awardnumber\":\"308299\",\"awardtitle\":\"NACLIM\",\"formatted\":\"EU | ||
| 28 | - 308299 - | 28 | - 308299 - | ||
| 29 | dnumber\":\"727852\",\"awardtitle\":\"Blue-Action\",\"formatted\":\"EU | 29 | dnumber\":\"727852\",\"awardtitle\":\"Blue-Action\",\"formatted\":\"EU | ||
| 30 | - 727852 - Blue-Action\"},{\"name\":\"Royal Netherlands Institute for | 30 | - 727852 - Blue-Action\"},{\"name\":\"Royal Netherlands Institute for | ||
| 31 | Sea Research | 31 | Sea Research | ||
| 32 | NIOZ)\",\"awardnumber\":null,\"awardtitle\":null,\"formatted\":\"Royal | 32 | NIOZ)\",\"awardnumber\":null,\"awardtitle\":null,\"formatted\":\"Royal | ||
| 33 | Netherlands Institute for Sea Research (NIOZ) - -\"}]", | 33 | Netherlands Institute for Sea Research (NIOZ) - -\"}]", | ||
| 34 | "groups": [], | 34 | "groups": [], | ||
| 35 | "id": "f7af813a-18d5-47d1-8c62-520c172de46f", | 35 | "id": "f7af813a-18d5-47d1-8c62-520c172de46f", | ||
| 36 | "isopen": false, | 36 | "isopen": false, | ||
| 37 | "license_title": null, | 37 | "license_title": null, | ||
| 38 | "maintainer": null, | 38 | "maintainer": null, | ||
| 39 | "maintainer_email": null, | 39 | "maintainer_email": null, | ||
| 40 | "metadata_created": "2024-10-22T17:52:29.596083", | 40 | "metadata_created": "2024-10-22T17:52:29.596083", | ||
| n | 41 | "metadata_modified": "2024-10-22T17:52:54.910405", | n | 41 | "metadata_modified": "2024-10-22T17:52:56.411035", |
| 42 | "name": "7bbng", | 42 | "name": "7bbng", | ||
| 43 | "notes": "The data set under this specific DOI contains data from | 43 | "notes": "The data set under this specific DOI contains data from | ||
| 44 | the tenth LOCO2 deployment (LOCO2_10), from 2 August 2012 to 26 July | 44 | the tenth LOCO2 deployment (LOCO2_10), from 2 August 2012 to 26 July | ||
| 45 | 2014.\nData from other deployments can be found through the related | 45 | 2014.\nData from other deployments can be found through the related | ||
| 46 | identifyers.\n\nThe LOCO2 mooring was started as part of the Dutch | 46 | identifyers.\n\nThe LOCO2 mooring was started as part of the Dutch | ||
| 47 | Long-term Ocean Circulation Observations project. LOCO2 was moored in | 47 | Long-term Ocean Circulation Observations project. LOCO2 was moored in | ||
| 48 | the central Irminger Sea at approximately 59.2N, 39.5W from summer | 48 | the central Irminger Sea at approximately 59.2N, 39.5W from summer | ||
| 49 | 2003 until summer 2018. It was equipped with Acoustic Doppler Current | 49 | 2003 until summer 2018. It was equipped with Acoustic Doppler Current | ||
| 50 | Profilers for the upper ocean (<400m) and deep ocean (>2500m) | 50 | Profilers for the upper ocean (<400m) and deep ocean (>2500m) | ||
| 51 | circulation, a near bottom SBE37 to record the temperature and | 51 | circulation, a near bottom SBE37 to record the temperature and | ||
| 52 | salinity of the Denmark Strait Overflow Water and (from the 10th | 52 | salinity of the Denmark Strait Overflow Water and (from the 10th | ||
| 53 | deployment onwards) another SBE37 at around 150m. A McLane Moored | 53 | deployment onwards) another SBE37 at around 150m. A McLane Moored | ||
| 54 | Profiler (MMP) equipped with a CTD was programmed to make profiles | 54 | Profiler (MMP) equipped with a CTD was programmed to make profiles | ||
| 55 | along the mooring cable between ~150m depth and ~2400m depth.\n\nLOCO2 | 55 | along the mooring cable between ~150m depth and ~2400m depth.\n\nLOCO2 | ||
| 56 | was positioned in the center of the Irminger Gyre, underneath the | 56 | was positioned in the center of the Irminger Gyre, underneath the | ||
| 57 | strong atmospheric forcing of the Greenland Tip Jet, in order to study | 57 | strong atmospheric forcing of the Greenland Tip Jet, in order to study | ||
| 58 | deep winter convection in the Irminger Sea. Data and results are | 58 | deep winter convection in the Irminger Sea. Data and results are | ||
| 59 | described in the following publications:\n- de Jong, M. F., van Aken, | 59 | described in the following publications:\n- de Jong, M. F., van Aken, | ||
| 60 | H. M., V\u00e5ge, K., and R. S. Pickart (2012). Convective mixing in | 60 | H. M., V\u00e5ge, K., and R. S. Pickart (2012). Convective mixing in | ||
| 61 | the central Irminger Sea: 2002-2010. Deep-Sea Research I, 63, 36-51. | 61 | the central Irminger Sea: 2002-2010. Deep-Sea Research I, 63, 36-51. | ||
| 62 | https://doi.org/10.1016/j.dsr.2012.01.003\n- van Aken, H. M., and M. | 62 | https://doi.org/10.1016/j.dsr.2012.01.003\n- van Aken, H. M., and M. | ||
| 63 | F. de Jong (2012). Hydrographic variability of Denmark Strait Overflow | 63 | F. de Jong (2012). Hydrographic variability of Denmark Strait Overflow | ||
| 64 | Water near Cape Farewell with multi-decadal to weakly time scales. | 64 | Water near Cape Farewell with multi-decadal to weakly time scales. | ||
| 65 | Deep-Sea Research I, 66, 41-50. | 65 | Deep-Sea Research I, 66, 41-50. | ||
| 66 | https://doi.org/10.1016/j.dsr.2012.04.004\n- de Jong, M. F. and L. de | 66 | https://doi.org/10.1016/j.dsr.2012.04.004\n- de Jong, M. F. and L. de | ||
| 67 | Steur (2016). Strong winter cooling over the Irminger Sea in winter | 67 | Steur (2016). Strong winter cooling over the Irminger Sea in winter | ||
| 68 | 2014-2015, exceptional deep convection, and the emergence of | 68 | 2014-2015, exceptional deep convection, and the emergence of | ||
| 69 | anomalously low SST. Geophysical Research Letters, 43, 13, 7106-7113. | 69 | anomalously low SST. Geophysical Research Letters, 43, 13, 7106-7113. | ||
| 70 | https://doi.org/10.1002/2016GL069596\n- de Jong, M.F., M. Oltmanns, J. | 70 | https://doi.org/10.1002/2016GL069596\n- de Jong, M.F., M. Oltmanns, J. | ||
| 71 | Karstensen, and L. de Steur (2018). Deep convection in the Irminger | 71 | Karstensen, and L. de Steur (2018). Deep convection in the Irminger | ||
| 72 | Sea observed with a dense mooring array. Oceanography | 72 | Sea observed with a dense mooring array. Oceanography | ||
| 73 | 31(1):50\u201359. https://doi.org/10.5670/oceanog.2018.109\n- de Jong, | 73 | 31(1):50\u201359. https://doi.org/10.5670/oceanog.2018.109\n- de Jong, | ||
| 74 | M.F., Fogaren, K.E., Le Bras, I., Trafford, L. and H. Palevsky | 74 | M.F., Fogaren, K.E., Le Bras, I., Trafford, L. and H. Palevsky | ||
| 75 | (submitted 2023). Convection in the central Irminger Sea; insights | 75 | (submitted 2023). Convection in the central Irminger Sea; insights | ||
| 76 | into variability and the roles of surface forcing and stratification | 76 | into variability and the roles of surface forcing and stratification | ||
| 77 | from 19 years of high resolution mooring data.", | 77 | from 19 years of high resolution mooring data.", | ||
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| 302 | Circulation Observations (LOCO) mooring in the central Irminger Sea: | 324 | Circulation Observations (LOCO) mooring in the central Irminger Sea: | ||
| 303 | Deployment ten (LOCO2_10) August 2012 to July 2014", | 325 | Deployment ten (LOCO2_10) August 2012 to July 2014", | ||
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