Migration Property List
Get a list of MigrationProperty objects.
GET /api/v3/migrationproperties/?format=api&offset=3800
{ "count": 5522, "next": "https://api.catalogue.ceda.ac.uk/api/v3/migrationproperties/?format=api&limit=100&offset=3900", "previous": "https://api.catalogue.ceda.ac.uk/api/v3/migrationproperties/?format=api&limit=100&offset=3700", "results": [ { "id": 8391, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8552 }, { "id": 8394, "key": "observation.content.citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\nLandmap; The GeoInformation Group. UK building classes, [Internet]. NERC Earth Observation Data Centre, 2014, <i>Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__ACTIVITY_c04941e6-29d2-11e4-98c5-00163e251233\r\n</div>", "modified": "2021-10-18", "ob_ref": 8552 }, { "id": 8399, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8556 }, { "id": 8400, "key": "observation.content.links", "value": "<div property=\"cedacat:links\">\r\n<div class=\"links\">Documentation and Links to further information and references</div>\r\n<p><b>Software</b></p>\r\n<p><a href=\"http://www.qgis.org/en/site/\">Quantum GIS (QGIS)</a> is a user friendly Open Source Geographic Information System (GIS) licensed under the GNU General Public License. QGIS is an official project of the Open Source Geospatial Foundation (OSGeo). It runs on Linux, Unix, Mac OSX, Windows and Android and supports numerous vector, raster, and database formats and functionalities.</p>\r\n\r\n<p><a href=\"http://udig.refractions.net/\">User-friendly Desktop Internet GIS (uDig)</a> is an open source (EPL and BSD) desktop application framework, built with Eclipse Rich Client (RCP) technology; that provides a Java solution for desktop GIS data access, editing, and viewing.</p>\r\n\r\n<p><b>Documentation</b></p>\r\n<ul>\r\n<li>Building classes <a href=\"http://www.geoinformationgroup.co.uk/wp-content/uploads/2011/05/Building-Class-Reference-Sheet-V4-May-11.pdf\">reference sheet</a></li>\r\n<li>The Cities Revealed buildings <a href=\"http://www.geoinformationgroup.co.uk/wp-content/uploads/2010/10/building_class_v6.pdf\">product guide</a></li>\r\n<li>The GeoInformation Group <a href=\"http://data.ceda.ac.uk/neodc/landmap/documents/Building_Class_Notes_2012.pdf\">guide to the building class dataset (link here)</a></li>\r\n</ul>\r\n\r\n<p><b>Links to further information</b></p>\r\n<ul>\r\n<li>The Landmap project <a href=\"http://www.landmap.ac.uk/index.php/Datasets/Building-Blocks/Building-Blocks\">building blocks</a> website, this website may be offline after 1st August 2014 due to a withdrawal of JISC (Joint Information Systems Committee) funding, see below for an archived version of the site</li>\r\n<li>An <a href=\"https://web.archive.org/web/20131106083649/http://www.landmap.ac.uk/index.php/Datasets/Building-Blocks/Building-Blocks\">archived</a> version of the Landmap project building blocks site, hosted by the <a href=\"https://archive.org/web/\">Internet Archive</a> project</li>\r\n<li><a href=\"http://www.geoinformationgroup.co.uk/\">The GeoInformation Group (TGG)</a> homepage</li>\r\n</ul>\r\n</div>\r\n\r\n\r\n", "modified": "2017-03-02", "ob_ref": 8556 }, { "id": 8401, "key": "observation.content.introduction", "value": "<div property=\"cedacat:introduction\">\r\n<div class=\"introduction\">Introduction</div>\r\n<p>This dataset is a combination of the <a href=\"http://www.geoinformationgroup.co.uk/\">The GeoInformation Groups' Cities Revealed</a> <a href=\"http://catalogue.ceda.ac.uk/uuid/e1449eac35108b49d3a0af26bb6d2060\">UK building heights</a> and <a href=\"http://catalogue.ceda.ac.uk/uuid/cf27c81e7f54c3701899017d1b810f81\">UK building classes</a> datasets, although height information is lacking for some buildings, so users may wish to check the <a href=\"http://catalogue.ceda.ac.uk/uuid/e1449eac35108b49d3a0af26bb6d2060\">UK building heights</a> database in these cases. This dataset provides outlines of building blocks with height information derived from the Cities Revealed <a href=\"http://catalogue.ceda.ac.uk/uuid/acfa8955414aef710105ef640802b9aa\">LiDAR surveys</a>, high-resolution <a href=\"http://catalogue.ceda.ac.uk/uuid/1999cc89208158c8616845f01ac93100\">aerial photography</a> and other height data sources combined with <a href=\"http://catalogue.ceda.ac.uk/uuid/cf27c81e7f54c3701899017d1b810f81\">UK building classes</a> data. The data were acquired by the <a href=\"http://catalogue.ceda.ac.uk/uuid/7f1280cf215da6f8001eae5c2f019fe8\">Landmap project</a> from <a href=\"http://www.geoinformationgroup.co.uk/\">The GeoInformation Group (TGG)</a>.</p> \r\n<p>The <a href=\"http://www.jisc.ac.uk/\">Joint Information Systems Committee (JISC)</a> funded <a href=\"http://catalogue.ceda.ac.uk/uuid/7f1280cf215da6f8001eae5c2f019fe8\">Landmap service</a> which ran from 2001 to July 2014 collected and hosted a large amount of earth observation data, such as thermal imagery, for the majority of the UK. After removal of <a href=\"http://www.jisc.ac.uk/\">JISC</a> funding in 2013, the <a href=\"http://catalogue.ceda.ac.uk/uuid/7f1280cf215da6f8001eae5c2f019fe8\">Landmap service</a> is no longer operational, with the data now held at the NEODC.</p> \r\n</div>\r\n\r\n", "modified": "2014-11-07", "ob_ref": 8556 }, { "id": 8402, "key": "observation.content.citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\nLandmap; The GeoInformation Group. UK building blocks, [Internet]. NERC Earth Observation Data Centre, 2014, <i>Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__ACTIVITY_cc3065e0-29df-11e4-8d25-00163e251233\r\n</div>\r\n", "modified": "2014-10-28", "ob_ref": 8556 }, { "id": 8403, "key": "observation.content.update", "value": "<div property=\"cedacat:update\">\r\n<div class=\"update\">Update Frequency</div>\r\nnotPlanned\r\n</div>", "modified": "2014-10-28", "ob_ref": 8556 }, { "id": 8404, "key": "observation.content.contact", "value": "<div property=\"cedacat:contact\">\r\n<div class=\"contact\">Who to contact</div>\r\n<p>If you have queries about these pages or about obtaining the Landmap building class data from the NEODC then you should contact the <a href=\"mailto:support@ceda.ac.uk\">NEODC Support team</a>. Your query should be answered within one working day. When follow-up work is required, the NEODC support team will carry out the work as quickly and efficiently as possible.</p>\r\n</div>\r\n\r\n", "modified": "2014-11-27", "ob_ref": 8556 }, { "id": 8405, "key": "observation.content.formats", "value": "<div property=\"cedacat:formats\">\r\n<div class=\"formats\">Data availability and file format</div>\r\n<p>Data are available as shapefiles, which comprise of .shp, .shx and .dbf files. \r\n</p><ul>\r\n<li>shp - shape format; the feature geometry itself</li>\r\n<li>shx - shape index format; a positional index of the feature geometry to allow seeking forwards and backwards quickly</li>\r\n<li>dbf - attribute format; columnar attributes for each shape, in dBase IV format</li>\r\n</ul>\r\n<p>Also provided are prj, sbn, sbx and xml files.\r\n<ul>\r\n<li>prj - projection format; the coordinate system and projection information, a plain text file describing the projection</li>\r\n<li>sbn and sbx - a spatial index of the features</li>\r\n<li>xml - location and other associated information</li>\r\n</ul></p>\r\n<p>Free software can be used to open shapefiles, such as <a href=\"http://www.qgis.org/en/site/\">Quantum GIS (QGIS)</a> or <a href=\"http://udig.refractions.net/\">User-friendly Desktop Internet GIS (uDig)</a>.</p>\r\n<p>The classifications attributes found in the attribute table (dbf files) of the shapefiles can be identified using this <a href=\"http://data.ceda.ac.uk/neodc/landmap/documents/Building_Class_Reference_Sheet_v6_Sep_12.pdf\">building class reference sheet</a>. There are 9 Age categories and 19 Type categories. Not all the Age/Type combinations are used, for example there are no Early and Middle Victorian very tall flats (point blocks) in the current edition of the classification (Version 6 September 2012). The current database for the UK does not contain Age categories 1 and 2 and only one type for Age 8. Also the type categories of Medium Height flats 5-6 storeys (3), Tall Terraces 3-4 storeys (5) and Very Large Detached Houses, Sometimes converted to flats (15) have been removed. These are all indicated by the DNU label in the classification sheet. More information can be found on in the The GeoInformation Group <a href=\"http://data.ceda.ac.uk/neodc/landmap/documents/Building_Class_Notes_2012.pdf\">guide to the building class dataset (link here)</a>. All building blocks have also have a height attribute, HGT, this value is the height of the building blocks from the base to the top of the building. In some cases this information is not supplied and presented as 0.</p>\r\n</div>\r\n\r\n\r\n", "modified": "2017-03-02", "ob_ref": 8556 }, { "id": 8407, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8560 }, { "id": 8410, "key": "observation.content.citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\nLandmap. Kinematic GPS (KGPS) data for UK roads, [Internet]. NERC Earth Observation Data Centre, 2014, <i>Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__ACTIVITY_975c0fce-29ec-11e4-a413-00163e251233\r\n</div>", "modified": "2021-10-18", "ob_ref": 8560 }, { "id": 8415, "key": "Instrument.content.contact", "value": "<div property=\"cedacat:contact\">\r\n<div class=\"contact\">Who to contact</div>\r\n<p>If you have queries about these pages or about obtaining the Landmap KGPS data from the NEODC then you should contact the <a href=\"mailto:neodc@rl.ac.uk\">NEODC Support team</a>. Your query should be answered within one working day. When follow-up work is required, the NEODC support team will carry out the work as quickly and efficiently as possible.</p>\r\n</div>", "modified": "2018-04-09", "ob_ref": 8562 }, { "id": 8416, "key": "Instrument.content.links", "value": "<div property=\"cedacat:links\">\r\n<div class=\"links\">Documentation and Links to further information and references</div>\r\n<p>\r\n</p><ul>\r\n<li><a href=\"http://www.leica-geosystems.co.uk/en/index.htm\">Leica Geosystems</a> website</li>\r\n</ul>\r\n<p />\r\n</div>\r\n\r\n\r\n", "modified": "2018-04-09", "ob_ref": 8562 }, { "id": 8417, "key": "Instrument.content.contact", "value": "<div property=\"cedacat:contact\">\r\n<div class=\"contact\">Who to contact</div>\r\n<p>If you have queries about these pages or about obtaining the Landmap KGPS data from the NEODC then you should contact the <a href=\"mailto:neodc@rl.ac.uk\">NEODC Support team</a>. Your query should be answered within one working day. When follow-up work is required, the NEODC support team will carry out the work as quickly and efficiently as possible.</p>\r\n</div>", "modified": "2018-04-09", "ob_ref": 8563 }, { "id": 8418, "key": "Instrument.content.links", "value": "<div property=\"cedacat:links\">\r\n<div class=\"links\">Documentation and Links to further information and references</div>\r\n<p>\r\n</p><ul>\r\n<li>The website for <a href=\"https://www.javad.com/\">JAVAD GNSS Inc.</a></li>\r\n</ul>\r\n<p />\r\n</div>\r\n\r\n\r\n", "modified": "2018-04-09", "ob_ref": 8563 }, { "id": 8419, "key": "Instrument.content.contact", "value": "<div property=\"cedacat:contact\">\r\n<div class=\"contact\">Who to contact</div>\r\n<p>If you have queries about these pages or about obtaining the Landmap KGPS data from the NEODC then you should contact the <a href=\"mailto:neodc@rl.ac.uk\">NEODC Support team</a>. Your query should be answered within one working day. When follow-up work is required, the NEODC support team will carry out the work as quickly and efficiently as possible.</p>\r\n</div>", "modified": "2018-04-09", "ob_ref": 8564 }, { "id": 8420, "key": "Instrument.content.links", "value": "<div property=\"cedacat:links\">\r\n<div class=\"links\">Documentation and Links to further information and references</div>\r\n<p>\r\n</p><ul>\r\n<li><a href=\"http://www.leica-geosystems.co.uk/en/index.htm\">Leica Geosystems</a> website</li>\r\n</ul>\r\n<p />\r\n</div>\r\n\r\n\r\n", "modified": "2018-04-09", "ob_ref": 8564 }, { "id": 8423, "key": "observation_collection.content.citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<ul>EUMETSAT. The Infrared Atmospheric Sounding Interferometer (IASI), [Internet]. NERC Earth Observation Data Centre, 2011, <i>Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__dataent_12417810458627666.\r\n</ul>\r\n</div>\r\n\r\n\r\n", "modified": "2016-06-27", "ob_ref": 8566 }, { "id": 8427, "key": "observation_collection.citation.publication_date", "value": "2009-12-10 03:17:43", "modified": "2014-09-28", "ob_ref": 8566 }, { "id": 8428, "key": "observation_collection.citation.revision_date", "value": "2014-06-11 14:57:04", "modified": "2014-09-28", "ob_ref": 8566 }, { "id": 8429, "key": "observation_collection.moles2_citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<ul>EUMETSAT. The Infrared Atmospheric Sounding Interferometer (IASI), [Internet]. NERC Earth Observation Data Centre, 2011, <i>Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__dataent_12417810458627666.\r\n</ul>\r\n</div>\r\n\r\n\r\n", "modified": "2016-06-27", "ob_ref": 8566 }, { "id": 8430, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8567 }, { "id": 8431, "key": "moles2.provider", "value": "badc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8572 }, { "id": 8432, "key": "observation_collection.content.links", "value": "<div property=\"cedacat:links\">\r\n<div class=\"links\">Documentation and Links to further information and references</div>\r\n<h3>Sensors</h3> \r\n<p>The Landsat TM sensor is a nadir-viewing, seven-band multi-spectral scanning radiometer capable of providing low to medium-resolution imaging information of the Earth's surface. The TM data are scanned simultaneously in seven spectral bands. Band 6 scans thermal (heat) infrared radiation. Spectral and spatial characteristics of these bands are shown in Table 1, below (For MSS details see <a href=\"http://www.neodc.rl.ac.uk/index.php?option=displaypage&Itemid=75&op=page&SubMenu=-1\">Landsat MSS 1-5 document</a>)</p>\r\n<table align=\"center\">\r\n <tbody><tr class=\"shadedarker\"> \r\n\t<th>Band no.</th>\r\n\t<th>Spectral range (µm)</th>\r\n\t<th>Ground resolution (m)</th>\r\n </tr>\r\n <tr> \r\n\t<th class=\"data\">1</th>\r\n\t<td class=\"data\">.450 to .520</td>\r\n\t<td class=\"data\">30</td>\r\n </tr>\r\n <tr class=\"shade\"> \r\n\t<th class=\"data\">2</th>\r\n\t<td class=\"data\">.520 to .600</td>\r\n\t<td class=\"data\">30</td>\r\n </tr>\r\n <tr> \r\n\t<th class=\"data\">3</th>\r\n\t<td class=\"data\">.630 to .690</td>\r\n\t<td class=\"data\">30</td>\r\n </tr>\r\n <tr class=\"shade\"> \r\n\t<th class=\"data\">4</th>\r\n\t<td class=\"data\">.775 to .900</td>\r\n\t<td class=\"data\">30</td>\r\n </tr>\r\n <tr> \r\n\t<th class=\"data\">5</th>\r\n\t<td class=\"data\">1.550 to 1.750</td>\r\n\t<td class=\"data\">30</td>\r\n </tr>\r\n <tr class=\"shade\"> \r\n\t<th class=\"data\">6</th>\r\n\t<td class=\"data\">10.40 to 12.50</td>\r\n\t<td class=\"data\">120</td>\r\n </tr>\r\n <tr> \r\n\t<th class=\"data\">7</th>\r\n\t<td class=\"data\">2.080 to 2.350</td>\r\n\t<td class=\"data\">30</td>\r\n </tr>\r\n</tbody>\r\n</table>\r\n\r\n<p><strong>Table 1</strong> LANDSAT-4 and 5 TM band characteristics.</p>\r\n\r\n<p>Landsat 5 information is also available on the web <a href=\"http://eros.usgs.gov/products/satellite/tm.html\">here</a>\r\n</p></div>", "modified": "2018-08-02", "ob_ref": 8577 }, { "id": 8434, "key": "observation_collection.content.citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<ul>National Aeronautics and Space Administration. Landsat 4/5 TM, [Internet]. NERC Earth Observation Data Centre, 2007, <i> Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__dataent_11793013743519809\r\n</ul>\r\n</div>", "modified": "2018-08-02", "ob_ref": 8577 }, { "id": 8436, "key": "observation_collection.content.formats", "value": "<div property=\"cedacat:formats\">\r\n<div class=\"formats\">Data availability and file format</div>\r\n<p> NEODC archive is available <a href=\"http://www.neodc.rl.ac.uk/datasearch/index.php?platform_type=satellite\" target=\"_blank\">here</a> to search NEODC holdings of Landsat 4 & 5 TM data or use the <a href=\"http://www.neodc.rl.ac.uk/maps/mapserver_neodc/dbox/neodc/neodc_coverage.html\">Interactive Map</a></p>\r\n\r\n<p>To browse the original data producer's archive click here: <a href=\"http://edcsns17.cr.usgs.gov/EarthExplorer/\">USGS Eros Data Centre</a>.</p>\r\n<p>Other suppliers are available here:</p>\r\n<ul>\r\n<li><a href=\"http://www.infoterra-global.com\">Infoterra</a></li>\r\n<li><a href=\"http://www.eurimage.com\">Eurimage</a></li>\r\n<li><a href=\"http://www.npagroup.com\">NPA Group</a></li>\r\n</ul>\r\n\r\n<p>The file format is ESA CEOS Landsat format - Details on how to open those types of files is available at <a href=\"http://geol.hu/data/online_help/Opening_External_Files.html\">http://geol.hu/data/online_help/Opening_External_Files.html</a>\r\n\r\n</p></div>", "modified": "2018-08-02", "ob_ref": 8577 }, { "id": 8438, "key": "observation_collection.citation.publication_date", "value": "2009-12-10 02:42:01", "modified": "2014-09-28", "ob_ref": 8577 }, { "id": 8439, "key": "observation_collection.citation.revision_date", "value": "2014-01-26 15:14:42", "modified": "2014-09-28", "ob_ref": 8577 }, { "id": 8440, "key": "observation_collection.moles2_citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<ul>National Aeronautics and Space Administration. Landsat 4/5 TM, [Internet]. NERC Earth Observation Data Centre, 2007, <i> Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__dataent_11793013743519809\r\n</ul>\r\n</div>", "modified": "2018-08-02", "ob_ref": 8577 }, { "id": 8441, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8578 }, { "id": 8448, "key": "observation_collection.citation.publication_date", "value": "2012-07-18 17:25:27", "modified": "2014-09-28", "ob_ref": 8584 }, { "id": 8449, "key": "observation_collection.citation.revision_date", "value": "2014-05-20 10:22:38", "modified": "2014-09-28", "ob_ref": 8584 }, { "id": 8450, "key": "observation_collection.moles2_citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<ul>Natural Environment Research Council, National Centre for Earth Observation, [Shepherd, A.;Sundal, A.]. Global 10 Year Monthly Climatology and Monthly Composites of Phytoplankton Size Class from SeaWiFS Analyses as part of the National Centre for Earth Observation (NCEO) Theme 2 Sub-theme 6, [Internet]. NCEO Earth Observation Data Centre, 2012, <i>Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__DE_2eb286d0-d0f5-11e1-bdb7-00163e251233.\r\n</ul>\r\n</div>\r\n\r\n\r\n", "modified": "2015-10-06", "ob_ref": 8584 }, { "id": 8451, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8585 }, { "id": 8452, "key": "moles2.spatial_resolution", "value": "9km SeaWiFS Level 3 Mapped data", "modified": "2014-09-28", "ob_ref": 8585 }, { "id": 8459, "key": "project.content.extra", "value": " <p><strong>Work description and methodology </strong>\r\n</p> <ul>\r\n<li>i) Partitioning the ocean organic carbon budget 10\r\n<ul>\r\n<li>a) Derive phytoplankton, detrital and dissolved components of the pelagic C-pool from IOP-OC data. \r\n</li><li>b) Develop statistical models linking organic C in various components to production and PFTs. \r\n</li><li>c) Determine seasonal, inter-annual, intra-decadal and regional variability in PFTs and their relationship to \r\nphysical-chemical drivers. \r\n</li></ul>\r\n</li><li>\r\nii) Improved estimates of marine PP and rate processes from OC data \r\n<ul>\r\n<li>\r\na) Develop new and export PP algorithms to quantify the transfer of C through the pelagic ecosystem and \r\n‘permanent’ sequestration from the atmosphere. \r\n</li><li>\r\nb) Quantify relationships between in situ PQE data and Chl & bio-optical indicators from EO data. \r\n</li><li>\r\nc) Use EO and in situ data to quantify the variability in PQE in phytoplankton communities (PFT estimates) \r\nand physical-chemical drivers (light, temperature, nutrients, stratification, turbulence). \r\n</li><li>\r\nd) Determine the PFT-specific P:R balance from EO estimates of PP and published data for respiration. \r\n</li><li>\r\ne) Apply EO estimates of global P:R balance to partition the ocean into regions dominated by autotrophic or \r\nheterotrophic processes. \r\n</li></ul>\r\n</li></ul>\r\n\r\n <p><strong>Deliverables </strong>\r\n</p> <ul>\r\n<li>\r\na) Global & regional (N Atlantic/shelf sea) climatologies of PFTs, coloured dissolved organic matter \r\n(CDOM), particulate-C and particle size concentration. \r\n</li><li>\r\nb) Quantified global & regional estimates of primary production (GPP, NPP, New-P, f-ratio) & C-export. \r\n</li><li>\r\nc) Global and regional climatologies of photosynthetic parameters (e.g. PQE). \r\n</li><li>\r\nd) Improved estimates of global and regional autotrophic/heterotrophic balance. \r\n</li></ul>\r\n <p>\r\n\r\n<strong>Key links to other programmes and organisations</strong>\r\n</p> <p>\r\n\r\nKT activities (DEFRA, EA, UKMO) include development of ecosystem monitoring products (e.g. CDOM in \r\nriver runoff, PFTs in relation to food for fish stocks, HABs and nuisance blooms, baseline maps and decadal \r\nchanges in phytoplankton composition). Obvious benefit to QUEST C-cycle modelling. Oceans 2025 (NERC \r\nMarine Centres research) is an associated project, providing in situ data (AMT; coastal observations). \r\n</p>", "modified": "2015-11-25", "ob_ref": 8587 }, { "id": 8460, "key": "project.moles2_activity_subtype", "value": "dgActivityDataProject", "modified": "2014-09-28", "ob_ref": 8587 }, { "id": 8461, "key": "Computation.content.extra", "value": " <p>\nA main characteristic of the model is that all the parameters that describe it have biological or optical interpretation. \n</p> <p>The three-population model performs better than the two-population model at retrieving total phytoplankton absorption. \n</p> <p>Accounting for the contributions of picophytoplankton and nanophytoplankton, rather than the combination of both as in the two-population model, improved significantly the retrieval of phytoplankton absorption at low chlorophyll-a concentrations. \n</p> <p>Class-dependent specific absorption of phytoplankton derived using the model compares well with previously published models.</p>", "modified": "2014-09-28", "ob_ref": 8588 }, { "id": 8462, "key": "Computation.content.all", "value": "Metadata document", "modified": "2014-09-28", "ob_ref": 8588 }, { "id": 8463, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8589 }, { "id": 8464, "key": "moles2.spatial_resolution", "value": "9km SeaWiFS Level 3 Mapped data", "modified": "2014-09-28", "ob_ref": 8589 }, { "id": 8474, "key": "observation_collection.content.citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<p /><ul>\r\nDudhia, A. Oxford MIPAS Atmospheric Profile Data, [Internet]. NERC Earth Observation Data Centre, 2010, <i>Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__DE_b5d9ea62-6e42-11df-92a9-00e081470264\r\n</ul>\r\n</div>", "modified": "2015-10-30", "ob_ref": 8591 }, { "id": 8478, "key": "observation_collection.citation.publication_date", "value": "2010-06-02 13:31:04", "modified": "2014-09-28", "ob_ref": 8591 }, { "id": 8479, "key": "observation_collection.citation.revision_date", "value": "2014-01-29 11:08:17", "modified": "2014-09-28", "ob_ref": 8591 }, { "id": 8480, "key": "observation_collection.moles2_citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<p /><ul>\r\nDudhia, A. Oxford MIPAS Atmospheric Profile Data, [Internet]. NERC Earth Observation Data Centre, 2010, <i>Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__DE_b5d9ea62-6e42-11df-92a9-00e081470264\r\n</ul>\r\n</div>", "modified": "2015-10-30", "ob_ref": 8591 }, { "id": 8481, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8592 }, { "id": 8482, "key": "project.moles2_activity_subtype", "value": "dgFundingProgram", "modified": "2014-09-28", "ob_ref": 8594 }, { "id": 8483, "key": "Computation.content.all", "value": "Metadata document ", "modified": "2014-09-28", "ob_ref": 8595 }, { "id": 8484, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8599 }, { "id": 8485, "key": "Computation.content.all", "value": "The Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) is one of the ten instruments onboard the Envisat satellite launched from Kourou (French Guyana) on the 28th February 2002 and operated by the European Space Agency (ESA). It operates as a Fourier transform spectrometer for the measurement of high-resolution gaseous emission spectra at the Earth's limb. It operates in the near- to mid-infrared, where many of the main atmospheric trace gases have important emission features. Its main objectives are to provide simultaneous and global measurements of the middle atmosphere dynamics, radiation budget and chemical composition (O3, H2O, CH4, N2O, HNO3, NO2), and to monitor stratospheric ozone and CFCs.", "modified": "2014-09-28", "ob_ref": 8601 }, { "id": 8486, "key": "Computation.content.all", "value": "Metadata document ", "modified": "2014-09-28", "ob_ref": 8601 }, { "id": 8487, "key": "Computation.content.all", "value": "Metadata document ", "modified": "2014-09-28", "ob_ref": 8602 }, { "id": 8488, "key": "Computation.content.contact", "value": "<div property=\"cedacat:contact\">\n<div class=\"contact\">Who to contact</div>\n<p>If you have queries about these pages then you should contact the <a href=\"http://www.ceda.ac.uk/contact/\">CEDA Support team</a>. Your query should be answered within one working day. When follow-up work is required, the CEDA support will carry out the work as quickly and efficiently as possible.</p>\n</div>\n\n", "modified": "2014-09-28", "ob_ref": 8602 }, { "id": 8489, "key": "Computation.content.links", "value": "<div property=\"cedacat:links\">\n<div class=\"operation\">Operational Details</div>\n<ol>\n<li>\n<div class=\"operationTitle\">Measurements taken by ENVISAT</div>\n<p>Envisat flies in a sun-synchronous polar orbit of about 800-km altitude. The repeat cycle of the reference orbit is 35 days, and for most sensors, being wide swath, it provides a complete coverage of the globe within one to three days. The Envisat satellite has a payload of 10 instruments.</p> \n</li>\n</ol>\n</div>", "modified": "2014-09-28", "ob_ref": 8602 }, { "id": 8493, "key": "observation_collection.content.citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<p>\r\n</p><ul>Natural Environment Research Council Airborne Research and Survey Facility . Airborne Research and Survey Facility (ARSF) Aerial Photography, Airborne Thematic Mapper (ATM), Light Detection and Ranging (LiDAR) and Compact Airborne Spectrographic Imager (CASI 2) data, [Internet]. NERC Earth Observation Data Centre, 2007, <i> Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__dataent_11716368890815055\r\n</ul></div>", "modified": "2020-01-08", "ob_ref": 8604 }, { "id": 8497, "key": "observation_collection.citation.publication_date", "value": "2009-12-10 03:01:43", "modified": "2014-09-28", "ob_ref": 8604 }, { "id": 8498, "key": "observation_collection.citation.revision_date", "value": "2013-12-10 17:04:49", "modified": "2014-09-28", "ob_ref": 8604 }, { "id": 8499, "key": "observation_collection.moles2_citation", "value": "<div property=\"cedacat:citation\">\r\n<div class=\"citation\">Citation</div>\r\n<p>\r\n</p><ul>Natural Environment Research Council Airborne Research and Survey Facility . Airborne Research and Survey Facility (ARSF) Aerial Photography, Airborne Thematic Mapper (ATM), Light Detection and Ranging (LiDAR) and Compact Airborne Spectrographic Imager (CASI 2) data, [Internet]. NERC Earth Observation Data Centre, 2007, <i> Date of citation</i>. Available from http://badc.nerc.ac.uk/view/neodc.nerc.ac.uk__ATOM__dataent_11716368890815055\r\n</ul></div>", "modified": "2020-01-08", "ob_ref": 8604 }, { "id": 8500, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8605 }, { "id": 8501, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8607 }, { "id": 8502, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8610 }, { "id": 8503, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8612 }, { "id": 8504, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8614 }, { "id": 8505, "key": "project.content.extra", "value": " <br />Ozone is a major participant in many atmospheric phenomena. It occurs as a natural component in the atmosphere. High levels of ozone in the troposphere are undesirable, as ozone is toxic to virtually all life on earth including man (WMO, 1992). Ozone advected to the troposphere is a potent greenhouse gas and may have a significant impact on these areas with enhanced response to climate change. Ozone abundance in the troposphere is thought to have increased by in excess of 100% in the last 100 years (Wayne, 1991). Although tropospheric ozone accounts for only ~10% of the total ozone present in the atmosphere, it is vital for the primary initiation of many oxidation chains that occur in the natural atmosphere. There is a clear increase in ozone abundance with increasing altitude (figure 1), and over the past 30 years ozone (both photochemical and background) has shown a significant increase in both the boundary layer and free troposphere (figure 2).", "modified": "2014-09-28", "ob_ref": 8616 }, { "id": 8506, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8616 }, { "id": 8507, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8618 }, { "id": 8508, "key": "project.content.extra", "value": " <br />LiDAR has been demonstrated to be an excellent mapping tool for identifying faults in forested terrain that pose a potential earthquake hazard. As part of an ongoing geophysical and geological investigation into earthquake hazards in Slovenia and the southeastern Alps region, we propose a LiDAR survey along two major fault systems in NW Slovenia to better document their geometry and recent activity. The Ravne Fault ruptured in 1998 (M=5.6) causing local landsliding and extensive damage and appears to be an active propagating fault, although its exact trace, length, and linkage with other faults is uncertain. The Idrija Fault forms a major topographic lineament and is believed to have ruptured in 1511 producing the largest historical earthquake (M=6.8) in the region. Both faults are believed to pose a major seismic hazard to large cities in the region where over 5 million people live including Trieste, Udine, Ljubljana, Villach, Klagenfurt, Rijeka, and Zagreb. LiDAR data should reveal the locations of paleaoseismic surface rupturing which will allow geologists to trench the sites, date previous events and most importantly, establish the earthquake recurrence interval.", "modified": "2014-09-28", "ob_ref": 8620 }, { "id": 8509, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8620 }, { "id": 8510, "key": "Instrument.content.all", "value": "The Optech 3033 is a high-resolution airborne laser scanner. Distances from the sensor to objects on the ground are calculated by recording the time taken for a pulse of laser energy emitted by the sensor to be reflected back. Half of this journey time multiplied by the speed of light gives the distance travelled by the pulse. The result is a highly detailed and highly accurate digital elevation model. Typical surveys involve collection of between one and four points per square metre although higher densities are possible. From a flying height of 1200 metres absolute accuracy is better than plus or minus 15 cm.\r\n\r\nThe system is complemented by a video recording system that can provide VHS playback of survey runs\r\n\r\nThe sensor (owned by ULM Cambridge) was deployed by ARSF from 2003 to 2008 on a development basis and is therefore not regarded as a core instrument.", "modified": "2017-01-30", "ob_ref": 8621 }, { "id": 8511, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8623 }, { "id": 8512, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8625 }, { "id": 8513, "key": "Instrument.content.extra", "value": " <h3>Airborne Thematic Mapper (ATM)</h3>\n <ul>\n<li><strong>ATM Background information:</strong><p> \n\n</p><p>The <a href=\"http://arsf.nerc.ac.uk/\">NERC Airborne Research and Survey Facility (ARSF)</a> has flown two ATM instruments over the period 1982 - present: the Daedalus 1268 was operated from 1982 until 1998. Since 1996 an upgraded version - the Azimuth Systems AZ-16 has been used, along with an improved data acquisition system.</p>\n<p>The eleven spectral channels of these instruments cover the visible and near-infrared (Chs: 1-8), shortwave infrared (SWIR - Chs: 9 & 10) and thermal infrared (TIR - Ch: 11) many of which closely match the seven channels of the Landsat Thematic Mapper satellite (see Fig.1 and Table 1):</p>\n<center><table align=\"center\">\n<tbody>\n<tr class=\"shadedarker\">\n<th class=\"data\">ATM Band</th>\n<th class=\"data\">Spectral range (μ m)</th>\n<th class=\"data\">Equivalent Landsat TM band</th></tr>\n<tr>\n<th class=\"data\">1</th>\n<td class=\"data\">0.42 - 0.45</td>\n<td class=\"data\" /></tr>\n<tr class=\"shade\">\n<th class=\"data\">2</th>\n<td class=\"data\">0.45 - 0.52</td>\n<td class=\"data\">1</td></tr>\n<tr>\n<th class=\"data\">3</th>\n<td class=\"data\">0.52 - 0.60</td>\n<td class=\"data\">2</td></tr>\n<tr class=\"shade\">\n<th class=\"data\">4</th>\n<td class=\"data\">0.605 - 0.625</td>\n<td class=\"data\" /></tr>\n<tr>\n<th class=\"data\">5</th>\n<td class=\"data\">0.63 - 0.69</td>\n<td class=\"data\">3</td></tr>\n<tr class=\"shade\">\n<th class=\"data\">6</th>\n<td class=\"data\">0.695 - 0.75</td>\n<td class=\"data\" /></tr>\n<tr>\n<th class=\"data\">7</th>\n<td class=\"data\">0.76 - 0.90</td>\n<td class=\"data\">4</td></tr>\n<tr class=\"shade\">\n<th class=\"data\">8</th>\n<td class=\"data\">0.91 - 1.05</td>\n<td class=\"data\" /></tr>\n<tr>\n<th class=\"data\">9</th>\n<td class=\"data\">1.55 - 1.75</td>\n<td class=\"data\">5</td></tr>\n<tr class=\"shade\">\n<th class=\"data\">10</th>\n<td class=\"data\">2.08 - 2.35</td>\n<td class=\"data\">7</td></tr>\n<tr>\n<th class=\"data\">11</th>\n<td class=\"data\">8.5 - 13.0#</td>\n<td class=\"data\">6</td></tr>\n<tr class=\"shade\">\n<th class=\"data\">12</th>\n<td class=\"data\">Spare thermal channel</td>\n<td class=\"data\" /></tr></tbody></table>\n</center>\n<center><p align=\"center\"><strong>Table 1.</strong> Band characteristics of the Daedalus 1268 Airborne Thematic Mapper instrument compared to those of the Landsat Thematic Mapper instrument. [# Thermal band broadened for aircraft operation.]</p>\n<p><img src=\"http://www.neodc.rl.ac.uk/images/data_pages/ATM_landsat_smaller.jpg\" /></p>\n<p align=\"center\"><strong>Figure 1.</strong> Comparison of ATM and LANDSAT-7 bands in the visible and near-infrared spectrum. ATM band 11 (not shown) is in the thermal infrared region, spanning 8400-11500 nm. Landsat-7 Band 8 (not shown) is a panchromatic band spanning the region 520-900 nm. </p>\n<p>Comparative Specifications of the Airborne Thematic Mapper - in its Daedalus 1268 and AZ-16 configurations?are provided in Table 2, below:</p>\n<table align=\"center\">\n<tbody>\n<tr class=\"shadedarker\">\n<th class=\"data\" />\n<th class=\"data\">Daedalus 1268</th>\n<th class=\"data\">AZ-16</th></tr>\n<tr>\n<th class=\"data\">Operational period</th>\n<td class=\"data\">1982-1985 \n</td><td class=\"data\">1996-present </td>\n</tr><tr class=\"shade\">\n<th class=\"data\" title=\"Instantaneous Field of View\">IFOV</th>\n<td class=\"data\">2.5 mrad</td>\n<td class=\"data\">2.5 mrad</td></tr>\n<tr>\n<th class=\"data\">Pixel swath</th>\n<td class=\"data\">716</td>\n<td class=\"data\">992/1984</td></tr>\n<tr class=\"shade\">\n<th class=\"data\" title=\"Digitised Field of View\">Digitised FOV</th>\n<td class=\"data\">86 °</td>\n<td class=\"data\">90 °</td></tr>\n<tr>\n<th class=\"data\">S-bend correction</th>\n<td class=\"data\">73 °</td>\n<td class=\"data\" /></tr>\n<tr class=\"shade\">\n<th class=\"data\">Scan rate</th>\n<td class=\"data\">12.5, 25, 50 Hz</td>\n<td class=\"data\">12.5, 25, 50 Hz</td></tr>\n<tr>\n<th class=\"data\">Roll correction</th>\n<td class=\"data\">+/-15 °</td>\n<td class=\"data\" /></tr>\n<tr class=\"shade\">\n<th class=\"data\">Resolution</th>\n<td class=\"data\">8-bit (0-255)</td>\n<td class=\"data\">16-bit (0-65535)</td></tr>\n<tr>\n<th class=\"data\">Thermal channel calibration</th>\n<td class=\"data\" colspan=\"2\">Two black bodies</td></tr></tbody></table>\n<p align=\"center\"><strong>Table 2.</strong> Comparison of Daedalus 1268 and AZ-16 systems.</p>\n<p>A fully automated Integrated Data System (IDS) was commissioned in late 1998/early 1999 and can now routinely provide geometrically registered, radiometrically calibrated data for both the multi-spectral ATM and the hyper-spectral CASI systems as operated by the NERC Airborne Research and Survey Facility.</p></center></li></ul>", "modified": "2014-09-28", "ob_ref": 8626 }, { "id": 8514, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8628 }, { "id": 8515, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8630 }, { "id": 8516, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8632 }, { "id": 8517, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8634 }, { "id": 8518, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8636 }, { "id": 8519, "key": "project.content.extra", "value": " <br />It is proposed to include in the Arctic Deployment 2003 of the Airborne Remote Sensing Facility a flight with the objective of obtaining Airborne Thematic Mapper (ATM) and Compact Airborne Spectrographic Imager (casi) data over sea-ice under predominantly clear-sky conditions. In summer, melt-ponds form on sea-ice, causing bias in microwave estimates of sea-ice concentration. With the data collected we will investigate the spectral signature of ponds at a high spatial resolution, at which individual melt ponds will be resolvable. This is with a view to routine use of lower-spatial-resolution space-based sensors to improve current estimates of summer sea-ice concentration in a multi-spectral retrieval.", "modified": "2014-09-28", "ob_ref": 8638 }, { "id": 8520, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8638 }, { "id": 8521, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8640 }, { "id": 8522, "key": "project.content.extra", "value": " <br />\nThe aim of this project is to examine spatial structure and diurnal variations of longwave flux from urban canopy using the techniques of remote sensing and thermal analysis in the context of understanding the current policies of urban design and the principles of design of a sustainable city where the adverse effects of UHI will be mitigated and positive effects will be used. The main advantage of remote sensing techniques is that a very large number of time-synchronised observations can be collected allowing the relations between thermal properties and types of both discrete urban surfaces and urban developments to be analysed in a way not possible with ground data alone in the extremely heterogeneous urban setting. Previous studies have demonstrated that emission of longwave radiation from urban canopies can be successfully measured using both satellite and airborne observations (Roth et al., 1989; Nichol, 1996; Lo et al., 1997; Quattrochi and Ridd, 1998; Voogt and Oke, 1997; 1998; Stone and Rodgers, 2001).", "modified": "2014-09-28", "ob_ref": 8642 }, { "id": 8523, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8642 }, { "id": 8524, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8644 }, { "id": 8525, "key": "project.content.extra", "value": " <br />The overall aim of this project, using the Sound of Eriskay as test site, is to develop algorithms for the simultaneous retrieval of depth and bottom reflectance and for the improvement in monitoring temperate coastal regions. Specific objectives are to:\n <ul>\n<li>To develop and test novel algebraic retrieval methods for the simultaneous derivation of bathymetry and bottom reflectance in heterogeneous sublittoral temperate regions\n</li><li>To infer the depth limits of water column attenuation properties on levels of discrimination of depth and bottom habitat types\n</li><li>To evaluate processed data for discriminating typical shallow water habitat types\n</li><li>To evaluate changes in bottom type characteristics induced by alterations to the hydrodynamics caused by causeway construction in the study site region\n</li><li>Evaluate the impacts of hydrodynamics on, and assess the potential for remote sensing of, seagrass health and productivity.\n</li></ul>", "modified": "2014-09-28", "ob_ref": 8646 }, { "id": 8526, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8646 }, { "id": 8527, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8648 }, { "id": 8528, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8650 }, { "id": 8529, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8652 }, { "id": 8530, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8654 }, { "id": 8531, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8656 }, { "id": 8532, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8658 }, { "id": 8533, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8660 }, { "id": 8534, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8662 }, { "id": 8535, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8664 }, { "id": 8536, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8666 }, { "id": 8537, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8668 }, { "id": 8538, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8670 }, { "id": 8539, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8672 }, { "id": 8540, "key": "project.moles2_activity_subtype", "value": "dgActivityDataCampaign", "modified": "2014-09-28", "ob_ref": 8674 }, { "id": 8541, "key": "moles2.provider", "value": "neodc.nerc.ac.uk", "modified": "2014-09-28", "ob_ref": 8676 } ] }
