Changes
On November 6, 2021 at 12:29:35 PM CDT,
Claire Herbert:
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| 5 | "creatorName": "BaySys", | 5 | "creatorName": "BaySys", | ||
| 6 | "email": "", | 6 | "email": "", | ||
| 7 | "nameIdentifier": "", | 7 | "nameIdentifier": "", | ||
| 8 | "nameType": "Organizational" | 8 | "nameType": "Organizational" | ||
| 9 | } | 9 | } | ||
| 10 | ], | 10 | ], | ||
| 11 | "PublicationYear": "2021", | 11 | "PublicationYear": "2021", | ||
| 12 | "Publisher": "BaySys", | 12 | "Publisher": "BaySys", | ||
| 13 | "ResourceType": "presentations", | 13 | "ResourceType": "presentations", | ||
| 14 | "Rights": "Creative Commons Attribution 4.0 International", | 14 | "Rights": "Creative Commons Attribution 4.0 International", | ||
| 15 | "author": null, | 15 | "author": null, | ||
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| 21 | "descriptionType": "Abstract", | 21 | "descriptionType": "Abstract", | ||
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| 27 | "groups": [ | 27 | "groups": [ | ||
| 28 | { | 28 | { | ||
| 29 | "description": "Freshwater is...", | 29 | "description": "Freshwater is...", | ||
| 30 | "display_name": "Freshwater", | 30 | "display_name": "Freshwater", | ||
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| 32 | "image_display_url": | 32 | "image_display_url": | ||
| 33 | /data/uploads/group/2021-10-31-211937.658599hyinspirehydrography.svg", | 33 | /data/uploads/group/2021-10-31-211937.658599hyinspirehydrography.svg", | ||
| 34 | "name": "freshwater", | 34 | "name": "freshwater", | ||
| 35 | "title": "Freshwater" | 35 | "title": "Freshwater" | ||
| 36 | }, | 36 | }, | ||
| 37 | { | 37 | { | ||
| 38 | "description": "Female Daphnia magna carrying a resting egg | 38 | "description": "Female Daphnia magna carrying a resting egg | ||
| 39 | (\"ephippium\"). The black ephippium is part of the carapace and | 39 | (\"ephippium\"). The black ephippium is part of the carapace and | ||
| 40 | contains usually two sexual eggs. Photo by Dieter Ebert, Basel, | 40 | contains usually two sexual eggs. Photo by Dieter Ebert, Basel, | ||
| 41 | Switzerland. \r\nCC BY-SA 4.0 Licence\r\n", | 41 | Switzerland. \r\nCC BY-SA 4.0 Licence\r\n", | ||
| 42 | "display_name": "Marine", | 42 | "display_name": "Marine", | ||
| 43 | "id": "98238b1c-5be8-41ad-8c6e-74cdc4f5f369", | 43 | "id": "98238b1c-5be8-41ad-8c6e-74cdc4f5f369", | ||
| 44 | "image_display_url": | 44 | "image_display_url": | ||
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| 46 | "name": "marine", | 46 | "name": "marine", | ||
| 47 | "title": "Marine" | 47 | "title": "Marine" | ||
| 48 | } | 48 | } | ||
| 49 | ], | 49 | ], | ||
| 50 | "id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 50 | "id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
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| 52 | "language": "", | 52 | "language": "", | ||
| 53 | "licenceType": "", | 53 | "licenceType": "", | ||
| 54 | "license_id": null, | 54 | "license_id": null, | ||
| 55 | "license_title": null, | 55 | "license_title": null, | ||
| 56 | "maintainer": null, | 56 | "maintainer": null, | ||
| 57 | "maintainer_email": null, | 57 | "maintainer_email": null, | ||
| 58 | "metadata_created": "2021-11-05T22:27:09.195631", | 58 | "metadata_created": "2021-11-05T22:27:09.195631", | ||
| t | 59 | "metadata_modified": "2021-11-06T17:29:34.251376", | t | 59 | "metadata_modified": "2021-11-06T17:29:34.862284", |
| 60 | "name": "baysys-conference-posters-presentations", | 60 | "name": "baysys-conference-posters-presentations", | ||
| 61 | "notes": "A collection of BaySys project conference posters and | 61 | "notes": "A collection of BaySys project conference posters and | ||
| 62 | presentations. These posters and presentations we delivered at | 62 | presentations. These posters and presentations we delivered at | ||
| 63 | national and international conferences by project HQP and grad | 63 | national and international conferences by project HQP and grad | ||
| 64 | students between 2016-2020.", | 64 | students between 2016-2020.", | ||
| 65 | "num_resources": 5, | 65 | "num_resources": 5, | ||
| 66 | "num_tags": 9, | 66 | "num_tags": 9, | ||
| 67 | "organization": { | 67 | "organization": { | ||
| 68 | "approval_status": "approved", | 68 | "approval_status": "approved", | ||
| 69 | "created": "2017-07-21T13:15:49.935872", | 69 | "created": "2017-07-21T13:15:49.935872", | ||
| 70 | "description": "The Centre for Earth Observation Science (CEOS) | 70 | "description": "The Centre for Earth Observation Science (CEOS) | ||
| 71 | was established in 1994 with a mandate to research, preserve and | 71 | was established in 1994 with a mandate to research, preserve and | ||
| 72 | communicate knowledge of Earth system processes using the technologies | 72 | communicate knowledge of Earth system processes using the technologies | ||
| 73 | of Earth Observation Science. Research is multidisciplinary and | 73 | of Earth Observation Science. Research is multidisciplinary and | ||
| 74 | collaborative seeking to understand the complex interrelationships | 74 | collaborative seeking to understand the complex interrelationships | ||
| 75 | between elements of Earth systems, and how these systems will likely | 75 | between elements of Earth systems, and how these systems will likely | ||
| 76 | respond to climate change. Although researchers have worked in many | 76 | respond to climate change. Although researchers have worked in many | ||
| 77 | regions, the Arctic marine system has always been a unifying focus of | 77 | regions, the Arctic marine system has always been a unifying focus of | ||
| 78 | activity.\r\n\r\nIn 2012, CEOS, along with the Greenland Climate | 78 | activity.\r\n\r\nIn 2012, CEOS, along with the Greenland Climate | ||
| 79 | Research Centre (GCRC, Nuuk, Greenland) and the Arctic Research Centre | 79 | Research Centre (GCRC, Nuuk, Greenland) and the Arctic Research Centre | ||
| 80 | (ARC, Aarhus, Denmark) established the Arctic Science Partnership, | 80 | (ARC, Aarhus, Denmark) established the Arctic Science Partnership, | ||
| 81 | thereby integrating academic and research initiatives.\r\n\r\nAreas of | 81 | thereby integrating academic and research initiatives.\r\n\r\nAreas of | ||
| 82 | existing research activity are divided among key themes:\r\n\r\nArctic | 82 | existing research activity are divided among key themes:\r\n\r\nArctic | ||
| 83 | Anthropology/Paleoclimatology: LiDAR scanning and digital site | 83 | Anthropology/Paleoclimatology: LiDAR scanning and digital site | ||
| 84 | preservation, archaeo-geophysics, permafrost degredation, lithic | 84 | preservation, archaeo-geophysics, permafrost degredation, lithic | ||
| 85 | morphometrics, zooarchaeology, proxy studies, paleodistribution of sea | 85 | morphometrics, zooarchaeology, proxy studies, paleodistribution of sea | ||
| 86 | ice, landscape learning, Paleo-Eskimo culture, Thule Inuit culture, | 86 | ice, landscape learning, Paleo-Eskimo culture, Thule Inuit culture, | ||
| 87 | ethnographic analogy, traditional knowledge, climate change and | 87 | ethnographic analogy, traditional knowledge, climate change and | ||
| 88 | northern heritage resource management.\r\n\r\nAtmospheric | 88 | northern heritage resource management.\r\n\r\nAtmospheric | ||
| 89 | Studies/Meteorology: Boundary layer, precipitation, clouds, storms and | 89 | Studies/Meteorology: Boundary layer, precipitation, clouds, storms and | ||
| 90 | extreme weather, circulation, eddy correlations, polar vortex, | 90 | extreme weather, circulation, eddy correlations, polar vortex, | ||
| 91 | climate, teleconnections, geophysical fluid dynamics, flux and energy | 91 | climate, teleconnections, geophysical fluid dynamics, flux and energy | ||
| 92 | budgets, ocean-sea ice-atmosphere interface, radiative transfer, ice | 92 | budgets, ocean-sea ice-atmosphere interface, radiative transfer, ice | ||
| 93 | albedo feedback, cloud radiative forcing, pCO2. | 93 | albedo feedback, cloud radiative forcing, pCO2. | ||
| 94 | \r\n\r\nBiogeochemistry: Organic carbon, greenhouse gases, bubbles, | 94 | \r\n\r\nBiogeochemistry: Organic carbon, greenhouse gases, bubbles, | ||
| 95 | Ikaite, carbonate chemistry, CO2 fluxes, mercury and other trace | 95 | Ikaite, carbonate chemistry, CO2 fluxes, mercury and other trace | ||
| 96 | metals, minerals, hydrocarbons, brine processes, otolith | 96 | metals, minerals, hydrocarbons, brine processes, otolith | ||
| 97 | microchemistry, sediments, biomarkers. \r\n\r\nContaminants: Mercury, | 97 | microchemistry, sediments, biomarkers. \r\n\r\nContaminants: Mercury, | ||
| 98 | trace metals, PAHs, source, transport, transformation, pathways, | 98 | trace metals, PAHs, source, transport, transformation, pathways, | ||
| 99 | bioaccumulations, marine ecosystems, marine chemistry. \r\nEarth | 99 | bioaccumulations, marine ecosystems, marine chemistry. \r\nEarth | ||
| 100 | Observation Science: Active and passive microwave, LiDAR, EM | 100 | Observation Science: Active and passive microwave, LiDAR, EM | ||
| 101 | induction, spatial-temporal analysis, forward and inverse scattering | 101 | induction, spatial-temporal analysis, forward and inverse scattering | ||
| 102 | models, complex permittivity, ocean colour, ocean surface roughness, | 102 | models, complex permittivity, ocean colour, ocean surface roughness, | ||
| 103 | NIR, TIR, satellite telemetry, GPS. Ice-Associated Biology: | 103 | NIR, TIR, satellite telemetry, GPS. Ice-Associated Biology: | ||
| 104 | Biophysical processes, primary production; ice algae, ice | 104 | Biophysical processes, primary production; ice algae, ice | ||
| 105 | microbiology, bio-optics, under-ice phytoplankton. \r\n\r\nInland | 105 | microbiology, bio-optics, under-ice phytoplankton. \r\n\r\nInland | ||
| 106 | Lakes and Waters: Hydrologic connectivity, watershed systems, sediment | 106 | Lakes and Waters: Hydrologic connectivity, watershed systems, sediment | ||
| 107 | transport, nutrient transport, contaminants, landscape processes, | 107 | transport, nutrient transport, contaminants, landscape processes, | ||
| 108 | remote sensing, freshwater-marine coupling. Marine Mammals: Seals, | 108 | remote sensing, freshwater-marine coupling. Marine Mammals: Seals, | ||
| 109 | whales, habitat, conservation, satellite telemetry, distribution, | 109 | whales, habitat, conservation, satellite telemetry, distribution, | ||
| 110 | population studies, prey behaviour, bioacoustics.\r\n\r\nModelling: | 110 | population studies, prey behaviour, bioacoustics.\r\n\r\nModelling: | ||
| 111 | Simulation of sea ice and oceanic regional processes, Nucleus for | 111 | Simulation of sea ice and oceanic regional processes, Nucleus for | ||
| 112 | European Modelling of the Ocean (NEMO), ice-ocean modelling and | 112 | European Modelling of the Ocean (NEMO), ice-ocean modelling and | ||
| 113 | interactions, hind cast simulations and projections for sea ice state | 113 | interactions, hind cast simulations and projections for sea ice state | ||
| 114 | and ocean variables based on CMIP5 scenarios and MIROC5 forcing, | 114 | and ocean variables based on CMIP5 scenarios and MIROC5 forcing, | ||
| 115 | validation.\r\n\r\nOceanography: Circulation, temperature, in-flow and | 115 | validation.\r\n\r\nOceanography: Circulation, temperature, in-flow and | ||
| 116 | out-flow shelves, water dynamics, microturbulence, Beaufort Gyre, eddy | 116 | out-flow shelves, water dynamics, microturbulence, Beaufort Gyre, eddy | ||
| 117 | correlations.\r\n\r\nSea Ice Geophysics:Thermodynamic and dynamic | 117 | correlations.\r\n\r\nSea Ice Geophysics:Thermodynamic and dynamic | ||
| 118 | processes, extreme ice features and hazards, snow, ridges, | 118 | processes, extreme ice features and hazards, snow, ridges, | ||
| 119 | polynyas.\r\n\r\nTraditional and Local Knowledge: Indigenous cultures, | 119 | polynyas.\r\n\r\nTraditional and Local Knowledge: Indigenous cultures, | ||
| 120 | Inuit, Inuvialuit, oral history, toponomy, mobility and settlement, | 120 | Inuit, Inuvialuit, oral history, toponomy, mobility and settlement, | ||
| 121 | hunting, food security, sea ice use, community-based research, | 121 | hunting, food security, sea ice use, community-based research, | ||
| 122 | community-based monitoring, two ways of knowing.", | 122 | community-based monitoring, two ways of knowing.", | ||
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| 127 | "name": "ceos2", | 127 | "name": "ceos2", | ||
| 128 | "state": "active", | 128 | "state": "active", | ||
| 129 | "title": "CEOS", | 129 | "title": "CEOS", | ||
| 130 | "type": "organization" | 130 | "type": "organization" | ||
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| 144 | ], | 144 | ], | ||
| 145 | "related_datasets": "[]", | 145 | "related_datasets": "[]", | ||
| 146 | "related_programs": "[\"504c728f-da7d-4da9-acab-8430ed5c47ea\"]", | 146 | "related_programs": "[\"504c728f-da7d-4da9-acab-8430ed5c47ea\"]", | ||
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| 150 | { | 150 | { | ||
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| 153 | "created": "2021-11-05T22:30:23.661687", | 153 | "created": "2021-11-05T22:30:23.661687", | ||
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| 156 | "description": "The Nelson/Hayes River (NHR), located in the | 156 | "description": "The Nelson/Hayes River (NHR), located in the | ||
| 157 | southwestern edge of the Hudson Bay (HB) (Canada) (Fig. 1) contributed | 157 | southwestern edge of the Hudson Bay (HB) (Canada) (Fig. 1) contributed | ||
| 158 | approximately 47% of the mean annual discharge of the western HB | 158 | approximately 47% of the mean annual discharge of the western HB | ||
| 159 | during the period 1964-2013 (D\u00e9ry et al, 2016). This voluminous | 159 | during the period 1964-2013 (D\u00e9ry et al, 2016). This voluminous | ||
| 160 | freshwater input controls the ocean processes in the south western to | 160 | freshwater input controls the ocean processes in the south western to | ||
| 161 | southern HB. Moreover hydroelectric regulation of the Nelson River has | 161 | southern HB. Moreover hydroelectric regulation of the Nelson River has | ||
| 162 | modified the discharge resulting in an increased winter discharge and | 162 | modified the discharge resulting in an increased winter discharge and | ||
| 163 | flattened summer hydrograph . This called for a need to investigate | 163 | flattened summer hydrograph . This called for a need to investigate | ||
| 164 | the revised seasonal signals of the river runoff in a spatio-temporal | 164 | the revised seasonal signals of the river runoff in a spatio-temporal | ||
| 165 | scale. Ocean color remote sensing approach provides a convenient way | 165 | scale. Ocean color remote sensing approach provides a convenient way | ||
| 166 | to study the mixed layer processes within the photic depth limit | 166 | to study the mixed layer processes within the photic depth limit | ||
| 167 | (Wozniak et al, 2010). This study has attempted to detect the NHR | 167 | (Wozniak et al, 2010). This study has attempted to detect the NHR | ||
| 168 | plume dispersion limit using color dissolved organic matter (CDOM) as | 168 | plume dispersion limit using color dissolved organic matter (CDOM) as | ||
| 169 | the ocean color proxy for terrestrial discharge, (Fichot et al, | 169 | the ocean color proxy for terrestrial discharge, (Fichot et al, | ||
| 170 | 2013).\r\n", | 170 | 2013).\r\n", | ||
| 171 | "format": "PDF", | 171 | "format": "PDF", | ||
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| 178 | "name": "An optical assessment of the nelson/hayes river plume | 178 | "name": "An optical assessment of the nelson/hayes river plume | ||
| 179 | dispersion extent in hudson bay (canada)", | 179 | dispersion extent in hudson bay (canada)", | ||
| 180 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 180 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
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| 187 | ource/913f0783-1d97-4e18-b087-554732049a23/download/basu_igs2019.pdf", | 187 | ource/913f0783-1d97-4e18-b087-554732049a23/download/basu_igs2019.pdf", | ||
| 188 | "url_type": "upload" | 188 | "url_type": "upload" | ||
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| 193 | "created": "2021-11-05T22:34:50.364874", | 193 | "created": "2021-11-05T22:34:50.364874", | ||
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| 196 | "description": "The aim of this study is to examine the role of | 196 | "description": "The aim of this study is to examine the role of | ||
| 197 | regulated rivers on bottom ice algal communities and phytoplankton by | 197 | regulated rivers on bottom ice algal communities and phytoplankton by | ||
| 198 | investigating the following objectives along a salinity gradient: 1. | 198 | investigating the following objectives along a salinity gradient: 1. | ||
| 199 | Examine the influence of the river plume on ice algal and | 199 | Examine the influence of the river plume on ice algal and | ||
| 200 | phytoplankton production from the estuary to the marine system 2. | 200 | phytoplankton production from the estuary to the marine system 2. | ||
| 201 | Examine the variability in ice algal biomass and nutrient availability | 201 | Examine the variability in ice algal biomass and nutrient availability | ||
| 202 | 3. Investigate the influence of the river output on taxonomic | 202 | 3. Investigate the influence of the river output on taxonomic | ||
| 203 | composition.", | 203 | composition.", | ||
| 204 | "format": "PDF", | 204 | "format": "PDF", | ||
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| 207 | "last_modified": "2021-11-05T22:34:50.334176", | 207 | "last_modified": "2021-11-05T22:34:50.334176", | ||
| 208 | "metadata_modified": "2021-11-05T22:35:37.408740", | 208 | "metadata_modified": "2021-11-05T22:35:37.408740", | ||
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| 211 | "name": "Response of biological communities to a seasonal | 211 | "name": "Response of biological communities to a seasonal | ||
| 212 | freshwater gradient in southwestern Hudson Bay, Canada\t", | 212 | freshwater gradient in southwestern Hudson Bay, Canada\t", | ||
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| 229 | "description": "**Motivation** \r\n\r\n- Sediments are | 229 | "description": "**Motivation** \r\n\r\n- Sediments are | ||
| 230 | hypothesized to enhance the rate of sea ice surface melt by decreasing | 230 | hypothesized to enhance the rate of sea ice surface melt by decreasing | ||
| 231 | surface albedo \r\n\r\n- Enhanced surface melt influences the sea ice | 231 | surface albedo \r\n\r\n- Enhanced surface melt influences the sea ice | ||
| 232 | surface topography/roughness, as well as increasing surface wetness | 232 | surface topography/roughness, as well as increasing surface wetness | ||
| 233 | \r\n\r\n- As a result, sediment presence on the ice surface could | 233 | \r\n\r\n- As a result, sediment presence on the ice surface could | ||
| 234 | impact both optical and radiometric satellite-borne measurements | 234 | impact both optical and radiometric satellite-borne measurements | ||
| 235 | (through changes in albedo and surface wetness, respectively)\r\n", | 235 | (through changes in albedo and surface wetness, respectively)\r\n", | ||
| 236 | "format": "PDF", | 236 | "format": "PDF", | ||
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| 238 | "id": "dd21f17a-61f3-47fc-82fa-1f3478ffc565", | 238 | "id": "dd21f17a-61f3-47fc-82fa-1f3478ffc565", | ||
| 239 | "last_modified": null, | 239 | "last_modified": null, | ||
| 240 | "metadata_modified": "2021-11-06T17:26:20.351253", | 240 | "metadata_modified": "2021-11-06T17:26:20.351253", | ||
| 241 | "mimetype": null, | 241 | "mimetype": null, | ||
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| 243 | "name": "Sediments and sea ice deformation: UAV observations of | 243 | "name": "Sediments and sea ice deformation: UAV observations of | ||
| 244 | sea ice topography evolution throughout the melt season", | 244 | sea ice topography evolution throughout the melt season", | ||
| 245 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 245 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
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| 250 | "state": "active", | 250 | "state": "active", | ||
| 251 | "url": | 251 | "url": | ||
| 252 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36106", | 252 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36106", | ||
| 253 | "url_type": null | 253 | "url_type": null | ||
| 254 | }, | 254 | }, | ||
| 255 | { | 255 | { | ||
| 256 | "cache_last_updated": null, | 256 | "cache_last_updated": null, | ||
| 257 | "cache_url": null, | 257 | "cache_url": null, | ||
| 258 | "created": "2021-11-05T22:36:14.383206", | 258 | "created": "2021-11-05T22:36:14.383206", | ||
| 259 | "datastore_active": false, | 259 | "datastore_active": false, | ||
| 260 | "datastore_contains_all_records_of_source_file": false, | 260 | "datastore_contains_all_records_of_source_file": false, | ||
| 261 | "description": "Diel vertical migration (DVM) of zooplanktonis a | 261 | "description": "Diel vertical migration (DVM) of zooplanktonis a | ||
| 262 | process of synchronized movement of the organisms from the mesopelagic | 262 | process of synchronized movement of the organisms from the mesopelagic | ||
| 263 | zone up to the epipelagic zone at night and returning back during the | 263 | zone up to the epipelagic zone at night and returning back during the | ||
| 264 | day. DVM is considered to be the largest synchronized diel movement of | 264 | day. DVM is considered to be the largest synchronized diel movement of | ||
| 265 | biomasson the planet. It also acts as a biological pump in | 265 | biomasson the planet. It also acts as a biological pump in | ||
| 266 | transferring organic carbon from the surface of the ocean to | 266 | transferring organic carbon from the surface of the ocean to | ||
| 267 | depth.\r\n", | 267 | depth.\r\n", | ||
| 268 | "format": "PDF", | 268 | "format": "PDF", | ||
| 269 | "hash": "", | 269 | "hash": "", | ||
| 270 | "id": "52a5859f-0bdd-4e8b-890c-7deea173f460", | 270 | "id": "52a5859f-0bdd-4e8b-890c-7deea173f460", | ||
| 271 | "last_modified": null, | 271 | "last_modified": null, | ||
| 272 | "metadata_modified": "2021-11-05T22:36:14.611228", | 272 | "metadata_modified": "2021-11-05T22:36:14.611228", | ||
| 273 | "mimetype": null, | 273 | "mimetype": null, | ||
| 274 | "mimetype_inner": null, | 274 | "mimetype_inner": null, | ||
| 275 | "name": "Impact of ice covers on diel vertical migration of | 275 | "name": "Impact of ice covers on diel vertical migration of | ||
| 276 | zooplankton in the Arctic marine environment", | 276 | zooplankton in the Arctic marine environment", | ||
| 277 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 277 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
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| 283 | "url": | 283 | "url": | ||
| 284 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36107", | 284 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36107", | ||
| 285 | "url_type": null | 285 | "url_type": null | ||
| 286 | }, | 286 | }, | ||
| 287 | { | 287 | { | ||
| 288 | "cache_last_updated": null, | 288 | "cache_last_updated": null, | ||
| 289 | "cache_url": null, | 289 | "cache_url": null, | ||
| 290 | "created": "2021-11-06T14:15:22.791448", | 290 | "created": "2021-11-06T14:15:22.791448", | ||
| 291 | "datastore_active": false, | 291 | "datastore_active": false, | ||
| 292 | "datastore_contains_all_records_of_source_file": false, | 292 | "datastore_contains_all_records_of_source_file": false, | ||
| 293 | "description": "Little information exists concerning the | 293 | "description": "Little information exists concerning the | ||
| 294 | riverine supply of inorganic nutrients and its consequences on primary | 294 | riverine supply of inorganic nutrients and its consequences on primary | ||
| 295 | production in the Hudson Bay system (HB), a large subarctic inland sea | 295 | production in the Hudson Bay system (HB), a large subarctic inland sea | ||
| 296 | that is impacted by rapid climate change and anthropogenic | 296 | that is impacted by rapid climate change and anthropogenic | ||
| 297 | disturbance. In order to provide a reference point by which future | 297 | disturbance. In order to provide a reference point by which future | ||
| 298 | changes can be evaluated, we estimated fluxes of nitrate (N), | 298 | changes can be evaluated, we estimated fluxes of nitrate (N), | ||
| 299 | phosphate (P) and silicate (Si) using contemporary and historical | 299 | phosphate (P) and silicate (Si) using contemporary and historical | ||
| 300 | nutrient data in conjunction with discharge rates generated by 3 | 300 | nutrient data in conjunction with discharge rates generated by 3 | ||
| 301 | different global climate models. Several key points can be | 301 | different global climate models. Several key points can be | ||
| 302 | highlighted. Firstly, the N:P and Si:N molar ratios of river nutrient | 302 | highlighted. Firstly, the N:P and Si:N molar ratios of river nutrient | ||
| 303 | fluxes exhibit large contrasts between different sectors of HB, which | 303 | fluxes exhibit large contrasts between different sectors of HB, which | ||
| 304 | is attributed to variable geological settings in the watersheds. | 304 | is attributed to variable geological settings in the watersheds. | ||
| 305 | Generally, low N:P and high Si:N ratios imply that river waters are | 305 | Generally, low N:P and high Si:N ratios imply that river waters are | ||
| 306 | characterized by a severe deficit of nitrate with respect to the needs | 306 | characterized by a severe deficit of nitrate with respect to the needs | ||
| 307 | of primary producers. Secondly, seasonality in nutrient concentrations | 307 | of primary producers. Secondly, seasonality in nutrient concentrations | ||
| 308 | and ratios were apparent in the sampled rivers at different times of | 308 | and ratios were apparent in the sampled rivers at different times of | ||
| 309 | years. While the regulation of river flow in the Nelson and La Grande | 309 | years. While the regulation of river flow in the Nelson and La Grande | ||
| 310 | rivers had no discernible impact on nutrient concentrations and | 310 | rivers had no discernible impact on nutrient concentrations and | ||
| 311 | ratios, it clearly shifted nutrient transports toward the winter when | 311 | ratios, it clearly shifted nutrient transports toward the winter when | ||
| 312 | biological activity in the estuaries is reduced. Thirdly, the | 312 | biological activity in the estuaries is reduced. Thirdly, the | ||
| 313 | southwestern rivers made the largest contributions of each nutrient | 313 | southwestern rivers made the largest contributions of each nutrient | ||
| 314 | flux to the total annual nutrient deliveries, with the modest | 314 | flux to the total annual nutrient deliveries, with the modest | ||
| 315 | contributions from the south and east rivers, and with the lowest | 315 | contributions from the south and east rivers, and with the lowest | ||
| 316 | contributions from the northwestern rivers. Finally, the combined | 316 | contributions from the northwestern rivers. Finally, the combined | ||
| 317 | nitrate input by all rivers was nearly two orders of magnitude (ca. | 317 | nitrate input by all rivers was nearly two orders of magnitude (ca. | ||
| 318 | 2.0 \u00d7 10^10 g N) lower than the estimated vertical re-supply of | 318 | 2.0 \u00d7 10^10 g N) lower than the estimated vertical re-supply of | ||
| 319 | nitrate to the surface during winter in offshore waters of HB (ca. 1.2 | 319 | nitrate to the surface during winter in offshore waters of HB (ca. 1.2 | ||
| 320 | \u00d7 10^12 g N). The potential contribution of river nutrients to | 320 | \u00d7 10^12 g N). The potential contribution of river nutrients to | ||
| 321 | new primary production is therefore small at HB scale but can be | 321 | new primary production is therefore small at HB scale but can be | ||
| 322 | significant locally.", | 322 | significant locally.", | ||
| 323 | "format": "PDF", | 323 | "format": "PDF", | ||
| 324 | "hash": "", | 324 | "hash": "", | ||
| 325 | "id": "d08f67a1-bad9-4081-9fb7-4ce0f7162195", | 325 | "id": "d08f67a1-bad9-4081-9fb7-4ce0f7162195", | ||
| 326 | "last_modified": null, | 326 | "last_modified": null, | ||
| 327 | "metadata_modified": "2021-11-06T14:16:06.382115", | 327 | "metadata_modified": "2021-11-06T14:16:06.382115", | ||
| 328 | "mimetype": null, | 328 | "mimetype": null, | ||
| 329 | "mimetype_inner": null, | 329 | "mimetype_inner": null, | ||
| 330 | "name": "Nutrient inputs from subarctic rivers into the Hudson | 330 | "name": "Nutrient inputs from subarctic rivers into the Hudson | ||
| 331 | Bay system", | 331 | Bay system", | ||
| 332 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 332 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
| 333 | "position": 4, | 333 | "position": 4, | ||
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| 337 | "state": "active", | 337 | "state": "active", | ||
| 338 | "url": | 338 | "url": | ||
| 339 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36108", | 339 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36108", | ||
| 340 | "url_type": null | 340 | "url_type": null | ||
| 341 | } | 341 | } | ||
| 342 | ], | 342 | ], | ||
| 343 | "rightsIdentifier": "CC-BY-4.0", | 343 | "rightsIdentifier": "CC-BY-4.0", | ||
| 344 | "rightsIdentifierScheme": "SPDX", | 344 | "rightsIdentifierScheme": "SPDX", | ||
| 345 | "rightsSchemeURI": "https://spdx.org/licenses", | 345 | "rightsSchemeURI": "https://spdx.org/licenses", | ||
| 346 | "rightsURI": "https://spdx.org/licenses/CC-BY-4.0.html", | 346 | "rightsURI": "https://spdx.org/licenses/CC-BY-4.0.html", | ||
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| 348 | "state": "active", | 348 | "state": "active", | ||
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| 350 | "tags": [ | 350 | "tags": [ | ||
| 351 | { | 351 | { | ||
| 352 | "display_name": "Albedo", | 352 | "display_name": "Albedo", | ||
| 353 | "id": "2f4d13d8-0144-46f5-9eb5-c7ae9e1d46b7", | 353 | "id": "2f4d13d8-0144-46f5-9eb5-c7ae9e1d46b7", | ||
| 354 | "name": "Albedo", | 354 | "name": "Albedo", | ||
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| 356 | "vocabulary_id": null | 356 | "vocabulary_id": null | ||
| 357 | }, | 357 | }, | ||
| 358 | { | 358 | { | ||
| 359 | "display_name": "Climate change", | 359 | "display_name": "Climate change", | ||
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| 364 | }, | 364 | }, | ||
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| 371 | }, | 371 | }, | ||
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| 373 | "display_name": "Modeling", | 373 | "display_name": "Modeling", | ||
| 374 | "id": "9f98c8ac-b485-4348-a112-1a57cc809e6d", | 374 | "id": "9f98c8ac-b485-4348-a112-1a57cc809e6d", | ||
| 375 | "name": "Modeling", | 375 | "name": "Modeling", | ||
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| 377 | "vocabulary_id": null | 377 | "vocabulary_id": null | ||
| 378 | }, | 378 | }, | ||
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| 382 | "name": "Nutrients", | 382 | "name": "Nutrients", | ||
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| 385 | }, | 385 | }, | ||
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| 389 | "name": "Rivers", | 389 | "name": "Rivers", | ||
| 390 | "state": "active", | 390 | "state": "active", | ||
| 391 | "vocabulary_id": null | 391 | "vocabulary_id": null | ||
| 392 | }, | 392 | }, | ||
| 393 | { | 393 | { | ||
| 394 | "display_name": "Satellite imagery", | 394 | "display_name": "Satellite imagery", | ||
| 395 | "id": "43456d7a-52ae-4390-acee-c0f0938d777c", | 395 | "id": "43456d7a-52ae-4390-acee-c0f0938d777c", | ||
| 396 | "name": "Satellite imagery", | 396 | "name": "Satellite imagery", | ||
| 397 | "state": "active", | 397 | "state": "active", | ||
| 398 | "vocabulary_id": null | 398 | "vocabulary_id": null | ||
| 399 | }, | 399 | }, | ||
| 400 | { | 400 | { | ||
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| 402 | "id": "44971f11-ef93-4a43-9900-f32da30b84f7", | 402 | "id": "44971f11-ef93-4a43-9900-f32da30b84f7", | ||
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| 410 | "name": "Sediments", | 410 | "name": "Sediments", | ||
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| 413 | } | 413 | } | ||
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| 418 | ], | 418 | ], | ||
| 419 | "title": "BaySys Conference Posters & Presentations", | 419 | "title": "BaySys Conference Posters & Presentations", | ||
| 420 | "type": "publication", | 420 | "type": "publication", | ||
| 421 | "url": null, | 421 | "url": null, | ||
| 422 | "version": "1.0" | 422 | "version": "1.0" | ||
| 423 | } | 423 | } |