Changes
On November 6, 2021 at 1:04:47 PM CDT, Claire Herbert:
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Uploaded a new file to resource Response of biological communities to a seasonal freshwater gradient in southwestern Hudson Bay, Canada in BaySys Conference Posters & Presentations
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Removed the value of field
url_type
in resource Response of biological communities to a seasonal freshwater gradient in southwestern Hudson Bay, Canada in BaySys Conference Posters & Presentations
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5 | "creatorName": "BaySys", | 5 | "creatorName": "BaySys", | ||
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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", | ||
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21 | "descriptionType": "Abstract", | 21 | "descriptionType": "Abstract", | ||
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27 | "groups": [ | 27 | "groups": [ | ||
28 | { | 28 | { | ||
29 | "description": "The cryosphere encompasses all the parts of the | 29 | "description": "The cryosphere encompasses all the parts of the | ||
30 | Earth system where water is in solid form, including ice sheets, ice | 30 | Earth system where water is in solid form, including ice sheets, ice | ||
31 | shelves, glaciers, snow cover, permafrost (frozen ground), sea ice, | 31 | shelves, glaciers, snow cover, permafrost (frozen ground), sea ice, | ||
32 | and river and lake ice. The cryosphere exerts an important influence | 32 | and river and lake ice. The cryosphere exerts an important influence | ||
33 | on Earth\u2019s climate. Image and description from | 33 | on Earth\u2019s climate. Image and description from | ||
34 | https://climate.copernicus.eu.", | 34 | https://climate.copernicus.eu.", | ||
35 | "display_name": "Cryosphere", | 35 | "display_name": "Cryosphere", | ||
36 | "id": "3707ff10-6424-4858-9ec9-7d67b38831b3", | 36 | "id": "3707ff10-6424-4858-9ec9-7d67b38831b3", | ||
37 | "image_display_url": | 37 | "image_display_url": | ||
38 | loads/group/2021-11-01-152857.585996C3SindicatorscryosphereFig10.png", | 38 | loads/group/2021-11-01-152857.585996C3SindicatorscryosphereFig10.png", | ||
39 | "name": "cryosphere", | 39 | "name": "cryosphere", | ||
40 | "title": "Cryosphere" | 40 | "title": "Cryosphere" | ||
41 | }, | 41 | }, | ||
42 | { | 42 | { | ||
43 | "description": "Female Daphnia magna carrying a resting egg | 43 | "description": "Female Daphnia magna carrying a resting egg | ||
44 | (\"ephippium\"). The black ephippium is part of the carapace and | 44 | (\"ephippium\"). The black ephippium is part of the carapace and | ||
45 | contains usually two sexual eggs. Photo by Dieter Ebert, Basel, | 45 | contains usually two sexual eggs. Photo by Dieter Ebert, Basel, | ||
46 | Switzerland. \r\nCC BY-SA 4.0 Licence\r\n", | 46 | Switzerland. \r\nCC BY-SA 4.0 Licence\r\n", | ||
47 | "display_name": "Marine", | 47 | "display_name": "Marine", | ||
48 | "id": "98238b1c-5be8-41ad-8c6e-74cdc4f5f369", | 48 | "id": "98238b1c-5be8-41ad-8c6e-74cdc4f5f369", | ||
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50 | ata/uploads/group/2021-10-31-211516.365746ofinspireoceanographic.svg", | 50 | ata/uploads/group/2021-10-31-211516.365746ofinspireoceanographic.svg", | ||
51 | "name": "marine", | 51 | "name": "marine", | ||
52 | "title": "Marine" | 52 | "title": "Marine" | ||
53 | } | 53 | } | ||
54 | ], | 54 | ], | ||
55 | "id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 55 | "id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
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59 | "license_id": null, | 59 | "license_id": null, | ||
60 | "license_title": null, | 60 | "license_title": null, | ||
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63 | "metadata_created": "2021-11-05T22:27:09.195631", | 63 | "metadata_created": "2021-11-05T22:27:09.195631", | ||
n | 64 | "metadata_modified": "2021-11-06T17:58:47.677594", | n | 64 | "metadata_modified": "2021-11-06T18:04:47.007814", |
65 | "name": "baysys-conference-posters-presentations", | 65 | "name": "baysys-conference-posters-presentations", | ||
66 | "notes": "A collection of BaySys project conference posters and | 66 | "notes": "A collection of BaySys project conference posters and | ||
67 | presentations. These posters and presentations we delivered at | 67 | presentations. These posters and presentations we delivered at | ||
68 | national and international conferences by project HQP and grad | 68 | national and international conferences by project HQP and grad | ||
69 | students between 2016-2020.", | 69 | students between 2016-2020.", | ||
70 | "num_resources": 6, | 70 | "num_resources": 6, | ||
71 | "num_tags": 13, | 71 | "num_tags": 13, | ||
72 | "organization": { | 72 | "organization": { | ||
73 | "approval_status": "approved", | 73 | "approval_status": "approved", | ||
74 | "created": "2017-07-21T13:15:49.935872", | 74 | "created": "2017-07-21T13:15:49.935872", | ||
75 | "description": "The Centre for Earth Observation Science (CEOS) | 75 | "description": "The Centre for Earth Observation Science (CEOS) | ||
76 | was established in 1994 with a mandate to research, preserve and | 76 | was established in 1994 with a mandate to research, preserve and | ||
77 | communicate knowledge of Earth system processes using the technologies | 77 | communicate knowledge of Earth system processes using the technologies | ||
78 | of Earth Observation Science. Research is multidisciplinary and | 78 | of Earth Observation Science. Research is multidisciplinary and | ||
79 | collaborative seeking to understand the complex interrelationships | 79 | collaborative seeking to understand the complex interrelationships | ||
80 | between elements of Earth systems, and how these systems will likely | 80 | between elements of Earth systems, and how these systems will likely | ||
81 | respond to climate change. Although researchers have worked in many | 81 | respond to climate change. Although researchers have worked in many | ||
82 | regions, the Arctic marine system has always been a unifying focus of | 82 | regions, the Arctic marine system has always been a unifying focus of | ||
83 | activity.\r\n\r\nIn 2012, CEOS, along with the Greenland Climate | 83 | activity.\r\n\r\nIn 2012, CEOS, along with the Greenland Climate | ||
84 | Research Centre (GCRC, Nuuk, Greenland) and the Arctic Research Centre | 84 | Research Centre (GCRC, Nuuk, Greenland) and the Arctic Research Centre | ||
85 | (ARC, Aarhus, Denmark) established the Arctic Science Partnership, | 85 | (ARC, Aarhus, Denmark) established the Arctic Science Partnership, | ||
86 | thereby integrating academic and research initiatives.\r\n\r\nAreas of | 86 | thereby integrating academic and research initiatives.\r\n\r\nAreas of | ||
87 | existing research activity are divided among key themes:\r\n\r\nArctic | 87 | existing research activity are divided among key themes:\r\n\r\nArctic | ||
88 | Anthropology/Paleoclimatology: LiDAR scanning and digital site | 88 | Anthropology/Paleoclimatology: LiDAR scanning and digital site | ||
89 | preservation, archaeo-geophysics, permafrost degredation, lithic | 89 | preservation, archaeo-geophysics, permafrost degredation, lithic | ||
90 | morphometrics, zooarchaeology, proxy studies, paleodistribution of sea | 90 | morphometrics, zooarchaeology, proxy studies, paleodistribution of sea | ||
91 | ice, landscape learning, Paleo-Eskimo culture, Thule Inuit culture, | 91 | ice, landscape learning, Paleo-Eskimo culture, Thule Inuit culture, | ||
92 | ethnographic analogy, traditional knowledge, climate change and | 92 | ethnographic analogy, traditional knowledge, climate change and | ||
93 | northern heritage resource management.\r\n\r\nAtmospheric | 93 | northern heritage resource management.\r\n\r\nAtmospheric | ||
94 | Studies/Meteorology: Boundary layer, precipitation, clouds, storms and | 94 | Studies/Meteorology: Boundary layer, precipitation, clouds, storms and | ||
95 | extreme weather, circulation, eddy correlations, polar vortex, | 95 | extreme weather, circulation, eddy correlations, polar vortex, | ||
96 | climate, teleconnections, geophysical fluid dynamics, flux and energy | 96 | climate, teleconnections, geophysical fluid dynamics, flux and energy | ||
97 | budgets, ocean-sea ice-atmosphere interface, radiative transfer, ice | 97 | budgets, ocean-sea ice-atmosphere interface, radiative transfer, ice | ||
98 | albedo feedback, cloud radiative forcing, pCO2. | 98 | albedo feedback, cloud radiative forcing, pCO2. | ||
99 | \r\n\r\nBiogeochemistry: Organic carbon, greenhouse gases, bubbles, | 99 | \r\n\r\nBiogeochemistry: Organic carbon, greenhouse gases, bubbles, | ||
100 | Ikaite, carbonate chemistry, CO2 fluxes, mercury and other trace | 100 | Ikaite, carbonate chemistry, CO2 fluxes, mercury and other trace | ||
101 | metals, minerals, hydrocarbons, brine processes, otolith | 101 | metals, minerals, hydrocarbons, brine processes, otolith | ||
102 | microchemistry, sediments, biomarkers. \r\n\r\nContaminants: Mercury, | 102 | microchemistry, sediments, biomarkers. \r\n\r\nContaminants: Mercury, | ||
103 | trace metals, PAHs, source, transport, transformation, pathways, | 103 | trace metals, PAHs, source, transport, transformation, pathways, | ||
104 | bioaccumulations, marine ecosystems, marine chemistry. \r\nEarth | 104 | bioaccumulations, marine ecosystems, marine chemistry. \r\nEarth | ||
105 | Observation Science: Active and passive microwave, LiDAR, EM | 105 | Observation Science: Active and passive microwave, LiDAR, EM | ||
106 | induction, spatial-temporal analysis, forward and inverse scattering | 106 | induction, spatial-temporal analysis, forward and inverse scattering | ||
107 | models, complex permittivity, ocean colour, ocean surface roughness, | 107 | models, complex permittivity, ocean colour, ocean surface roughness, | ||
108 | NIR, TIR, satellite telemetry, GPS. Ice-Associated Biology: | 108 | NIR, TIR, satellite telemetry, GPS. Ice-Associated Biology: | ||
109 | Biophysical processes, primary production; ice algae, ice | 109 | Biophysical processes, primary production; ice algae, ice | ||
110 | microbiology, bio-optics, under-ice phytoplankton. \r\n\r\nInland | 110 | microbiology, bio-optics, under-ice phytoplankton. \r\n\r\nInland | ||
111 | Lakes and Waters: Hydrologic connectivity, watershed systems, sediment | 111 | Lakes and Waters: Hydrologic connectivity, watershed systems, sediment | ||
112 | transport, nutrient transport, contaminants, landscape processes, | 112 | transport, nutrient transport, contaminants, landscape processes, | ||
113 | remote sensing, freshwater-marine coupling. Marine Mammals: Seals, | 113 | remote sensing, freshwater-marine coupling. Marine Mammals: Seals, | ||
114 | whales, habitat, conservation, satellite telemetry, distribution, | 114 | whales, habitat, conservation, satellite telemetry, distribution, | ||
115 | population studies, prey behaviour, bioacoustics.\r\n\r\nModelling: | 115 | population studies, prey behaviour, bioacoustics.\r\n\r\nModelling: | ||
116 | Simulation of sea ice and oceanic regional processes, Nucleus for | 116 | Simulation of sea ice and oceanic regional processes, Nucleus for | ||
117 | European Modelling of the Ocean (NEMO), ice-ocean modelling and | 117 | European Modelling of the Ocean (NEMO), ice-ocean modelling and | ||
118 | interactions, hind cast simulations and projections for sea ice state | 118 | interactions, hind cast simulations and projections for sea ice state | ||
119 | and ocean variables based on CMIP5 scenarios and MIROC5 forcing, | 119 | and ocean variables based on CMIP5 scenarios and MIROC5 forcing, | ||
120 | validation.\r\n\r\nOceanography: Circulation, temperature, in-flow and | 120 | validation.\r\n\r\nOceanography: Circulation, temperature, in-flow and | ||
121 | out-flow shelves, water dynamics, microturbulence, Beaufort Gyre, eddy | 121 | out-flow shelves, water dynamics, microturbulence, Beaufort Gyre, eddy | ||
122 | correlations.\r\n\r\nSea Ice Geophysics:Thermodynamic and dynamic | 122 | correlations.\r\n\r\nSea Ice Geophysics:Thermodynamic and dynamic | ||
123 | processes, extreme ice features and hazards, snow, ridges, | 123 | processes, extreme ice features and hazards, snow, ridges, | ||
124 | polynyas.\r\n\r\nTraditional and Local Knowledge: Indigenous cultures, | 124 | polynyas.\r\n\r\nTraditional and Local Knowledge: Indigenous cultures, | ||
125 | Inuit, Inuvialuit, oral history, toponomy, mobility and settlement, | 125 | Inuit, Inuvialuit, oral history, toponomy, mobility and settlement, | ||
126 | hunting, food security, sea ice use, community-based research, | 126 | hunting, food security, sea ice use, community-based research, | ||
127 | community-based monitoring, two ways of knowing.", | 127 | community-based monitoring, two ways of knowing.", | ||
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132 | "name": "ceos2", | 132 | "name": "ceos2", | ||
133 | "state": "active", | 133 | "state": "active", | ||
134 | "title": "CEOS", | 134 | "title": "CEOS", | ||
135 | "type": "organization" | 135 | "type": "organization" | ||
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150 | "related_datasets": "[]", | 150 | "related_datasets": "[]", | ||
151 | "related_programs": "[\"504c728f-da7d-4da9-acab-8430ed5c47ea\"]", | 151 | "related_programs": "[\"504c728f-da7d-4da9-acab-8430ed5c47ea\"]", | ||
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158 | "created": "2021-11-05T22:30:23.661687", | 158 | "created": "2021-11-05T22:30:23.661687", | ||
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161 | "description": "The Nelson/Hayes River (NHR), located in the | 161 | "description": "The Nelson/Hayes River (NHR), located in the | ||
162 | southwestern edge of the Hudson Bay (HB) (Canada) (Fig. 1) contributed | 162 | southwestern edge of the Hudson Bay (HB) (Canada) (Fig. 1) contributed | ||
163 | approximately 47% of the mean annual discharge of the western HB | 163 | approximately 47% of the mean annual discharge of the western HB | ||
164 | during the period 1964-2013 (D\u00e9ry et al, 2016). This voluminous | 164 | during the period 1964-2013 (D\u00e9ry et al, 2016). This voluminous | ||
165 | freshwater input controls the ocean processes in the south western to | 165 | freshwater input controls the ocean processes in the south western to | ||
166 | southern HB. Moreover hydroelectric regulation of the Nelson River has | 166 | southern HB. Moreover hydroelectric regulation of the Nelson River has | ||
167 | modified the discharge resulting in an increased winter discharge and | 167 | modified the discharge resulting in an increased winter discharge and | ||
168 | flattened summer hydrograph . This called for a need to investigate | 168 | flattened summer hydrograph . This called for a need to investigate | ||
169 | the revised seasonal signals of the river runoff in a spatio-temporal | 169 | the revised seasonal signals of the river runoff in a spatio-temporal | ||
170 | scale. Ocean color remote sensing approach provides a convenient way | 170 | scale. Ocean color remote sensing approach provides a convenient way | ||
171 | to study the mixed layer processes within the photic depth limit | 171 | to study the mixed layer processes within the photic depth limit | ||
172 | (Wozniak et al, 2010). This study has attempted to detect the NHR | 172 | (Wozniak et al, 2010). This study has attempted to detect the NHR | ||
173 | plume dispersion limit using color dissolved organic matter (CDOM) as | 173 | plume dispersion limit using color dissolved organic matter (CDOM) as | ||
174 | the ocean color proxy for terrestrial discharge, (Fichot et al, | 174 | the ocean color proxy for terrestrial discharge, (Fichot et al, | ||
175 | 2013).\r\n", | 175 | 2013).\r\n", | ||
176 | "format": "PDF", | 176 | "format": "PDF", | ||
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183 | "name": "An optical assessment of the nelson/hayes river plume | 183 | "name": "An optical assessment of the nelson/hayes river plume | ||
184 | dispersion extent in hudson bay (canada)", | 184 | dispersion extent in hudson bay (canada)", | ||
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192 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36104?show=full", | 192 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36104?show=full", | ||
193 | "url_type": "" | 193 | "url_type": "" | ||
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201 | "description": "The aim of this study is to examine the role of | 201 | "description": "The aim of this study is to examine the role of | ||
202 | regulated rivers on bottom ice algal communities and phytoplankton by | 202 | regulated rivers on bottom ice algal communities and phytoplankton by | ||
203 | investigating the following objectives along a salinity gradient: 1. | 203 | investigating the following objectives along a salinity gradient: 1. | ||
204 | Examine the influence of the river plume on ice algal and | 204 | Examine the influence of the river plume on ice algal and | ||
205 | phytoplankton production from the estuary to the marine system 2. | 205 | phytoplankton production from the estuary to the marine system 2. | ||
206 | Examine the variability in ice algal biomass and nutrient availability | 206 | Examine the variability in ice algal biomass and nutrient availability | ||
207 | 3. Investigate the influence of the river output on taxonomic | 207 | 3. Investigate the influence of the river output on taxonomic | ||
208 | composition.", | 208 | composition.", | ||
209 | "format": "PDF", | 209 | "format": "PDF", | ||
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214 | "mimetype": "application/pdf", | 214 | "mimetype": null, | ||
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216 | "name": "Response of biological communities to a seasonal | 216 | "name": "Response of biological communities to a seasonal | ||
217 | freshwater gradient in southwestern Hudson Bay, Canada\t", | 217 | freshwater gradient in southwestern Hudson Bay, Canada\t", | ||
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t | 225 | rce/aeb6b641-7a8e-40f4-abb4-509905234bc9/download/dalman_igs2019.pdf", | t | 225 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36105?show=full", |
226 | "url_type": "upload" | 226 | "url_type": "" | ||
227 | }, | 227 | }, | ||
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234 | "description": "**Motivation** \r\n\r\n- Sediments are | 234 | "description": "**Motivation** \r\n\r\n- Sediments are | ||
235 | hypothesized to enhance the rate of sea ice surface melt by decreasing | 235 | hypothesized to enhance the rate of sea ice surface melt by decreasing | ||
236 | surface albedo \r\n\r\n- Enhanced surface melt influences the sea ice | 236 | surface albedo \r\n\r\n- Enhanced surface melt influences the sea ice | ||
237 | surface topography/roughness, as well as increasing surface wetness | 237 | surface topography/roughness, as well as increasing surface wetness | ||
238 | \r\n\r\n- As a result, sediment presence on the ice surface could | 238 | \r\n\r\n- As a result, sediment presence on the ice surface could | ||
239 | impact both optical and radiometric satellite-borne measurements | 239 | impact both optical and radiometric satellite-borne measurements | ||
240 | (through changes in albedo and surface wetness, respectively)\r\n", | 240 | (through changes in albedo and surface wetness, respectively)\r\n", | ||
241 | "format": "PDF", | 241 | "format": "PDF", | ||
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245 | "metadata_modified": "2021-11-06T17:26:20.351253", | 245 | "metadata_modified": "2021-11-06T17:26:20.351253", | ||
246 | "mimetype": null, | 246 | "mimetype": null, | ||
247 | "mimetype_inner": null, | 247 | "mimetype_inner": null, | ||
248 | "name": "Sediments and sea ice deformation: UAV observations of | 248 | "name": "Sediments and sea ice deformation: UAV observations of | ||
249 | sea ice topography evolution throughout the melt season", | 249 | sea ice topography evolution throughout the melt season", | ||
250 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 250 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
251 | "position": 2, | 251 | "position": 2, | ||
252 | "resCategory": "documents", | 252 | "resCategory": "documents", | ||
253 | "resource_type": null, | 253 | "resource_type": null, | ||
254 | "size": null, | 254 | "size": null, | ||
255 | "state": "active", | 255 | "state": "active", | ||
256 | "url": | 256 | "url": | ||
257 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36106", | 257 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36106", | ||
258 | "url_type": null | 258 | "url_type": null | ||
259 | }, | 259 | }, | ||
260 | { | 260 | { | ||
261 | "cache_last_updated": null, | 261 | "cache_last_updated": null, | ||
262 | "cache_url": null, | 262 | "cache_url": null, | ||
263 | "created": "2021-11-05T22:36:14.383206", | 263 | "created": "2021-11-05T22:36:14.383206", | ||
264 | "datastore_active": false, | 264 | "datastore_active": false, | ||
265 | "datastore_contains_all_records_of_source_file": false, | 265 | "datastore_contains_all_records_of_source_file": false, | ||
266 | "description": "Diel vertical migration (DVM) of zooplanktonis a | 266 | "description": "Diel vertical migration (DVM) of zooplanktonis a | ||
267 | process of synchronized movement of the organisms from the mesopelagic | 267 | process of synchronized movement of the organisms from the mesopelagic | ||
268 | zone up to the epipelagic zone at night and returning back during the | 268 | zone up to the epipelagic zone at night and returning back during the | ||
269 | day. DVM is considered to be the largest synchronized diel movement of | 269 | day. DVM is considered to be the largest synchronized diel movement of | ||
270 | biomasson the planet. It also acts as a biological pump in | 270 | biomasson the planet. It also acts as a biological pump in | ||
271 | transferring organic carbon from the surface of the ocean to | 271 | transferring organic carbon from the surface of the ocean to | ||
272 | depth.\r\n", | 272 | depth.\r\n", | ||
273 | "format": "PDF", | 273 | "format": "PDF", | ||
274 | "hash": "", | 274 | "hash": "", | ||
275 | "id": "52a5859f-0bdd-4e8b-890c-7deea173f460", | 275 | "id": "52a5859f-0bdd-4e8b-890c-7deea173f460", | ||
276 | "last_modified": null, | 276 | "last_modified": null, | ||
277 | "metadata_modified": "2021-11-05T22:36:14.611228", | 277 | "metadata_modified": "2021-11-05T22:36:14.611228", | ||
278 | "mimetype": null, | 278 | "mimetype": null, | ||
279 | "mimetype_inner": null, | 279 | "mimetype_inner": null, | ||
280 | "name": "Impact of ice covers on diel vertical migration of | 280 | "name": "Impact of ice covers on diel vertical migration of | ||
281 | zooplankton in the Arctic marine environment", | 281 | zooplankton in the Arctic marine environment", | ||
282 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 282 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
283 | "position": 3, | 283 | "position": 3, | ||
284 | "resCategory": "documents", | 284 | "resCategory": "documents", | ||
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286 | "size": null, | 286 | "size": null, | ||
287 | "state": "active", | 287 | "state": "active", | ||
288 | "url": | 288 | "url": | ||
289 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36107", | 289 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36107", | ||
290 | "url_type": null | 290 | "url_type": null | ||
291 | }, | 291 | }, | ||
292 | { | 292 | { | ||
293 | "cache_last_updated": null, | 293 | "cache_last_updated": null, | ||
294 | "cache_url": null, | 294 | "cache_url": null, | ||
295 | "created": "2021-11-06T14:15:22.791448", | 295 | "created": "2021-11-06T14:15:22.791448", | ||
296 | "datastore_active": false, | 296 | "datastore_active": false, | ||
297 | "datastore_contains_all_records_of_source_file": false, | 297 | "datastore_contains_all_records_of_source_file": false, | ||
298 | "description": "Little information exists concerning the | 298 | "description": "Little information exists concerning the | ||
299 | riverine supply of inorganic nutrients and its consequences on primary | 299 | riverine supply of inorganic nutrients and its consequences on primary | ||
300 | production in the Hudson Bay system (HB), a large subarctic inland sea | 300 | production in the Hudson Bay system (HB), a large subarctic inland sea | ||
301 | that is impacted by rapid climate change and anthropogenic | 301 | that is impacted by rapid climate change and anthropogenic | ||
302 | disturbance. In order to provide a reference point by which future | 302 | disturbance. In order to provide a reference point by which future | ||
303 | changes can be evaluated, we estimated fluxes of nitrate (N), | 303 | changes can be evaluated, we estimated fluxes of nitrate (N), | ||
304 | phosphate (P) and silicate (Si) using contemporary and historical | 304 | phosphate (P) and silicate (Si) using contemporary and historical | ||
305 | nutrient data in conjunction with discharge rates generated by 3 | 305 | nutrient data in conjunction with discharge rates generated by 3 | ||
306 | different global climate models. Several key points can be | 306 | different global climate models. Several key points can be | ||
307 | highlighted. Firstly, the N:P and Si:N molar ratios of river nutrient | 307 | highlighted. Firstly, the N:P and Si:N molar ratios of river nutrient | ||
308 | fluxes exhibit large contrasts between different sectors of HB, which | 308 | fluxes exhibit large contrasts between different sectors of HB, which | ||
309 | is attributed to variable geological settings in the watersheds. | 309 | is attributed to variable geological settings in the watersheds. | ||
310 | Generally, low N:P and high Si:N ratios imply that river waters are | 310 | Generally, low N:P and high Si:N ratios imply that river waters are | ||
311 | characterized by a severe deficit of nitrate with respect to the needs | 311 | characterized by a severe deficit of nitrate with respect to the needs | ||
312 | of primary producers. Secondly, seasonality in nutrient concentrations | 312 | of primary producers. Secondly, seasonality in nutrient concentrations | ||
313 | and ratios were apparent in the sampled rivers at different times of | 313 | and ratios were apparent in the sampled rivers at different times of | ||
314 | years. While the regulation of river flow in the Nelson and La Grande | 314 | years. While the regulation of river flow in the Nelson and La Grande | ||
315 | rivers had no discernible impact on nutrient concentrations and | 315 | rivers had no discernible impact on nutrient concentrations and | ||
316 | ratios, it clearly shifted nutrient transports toward the winter when | 316 | ratios, it clearly shifted nutrient transports toward the winter when | ||
317 | biological activity in the estuaries is reduced. Thirdly, the | 317 | biological activity in the estuaries is reduced. Thirdly, the | ||
318 | southwestern rivers made the largest contributions of each nutrient | 318 | southwestern rivers made the largest contributions of each nutrient | ||
319 | flux to the total annual nutrient deliveries, with the modest | 319 | flux to the total annual nutrient deliveries, with the modest | ||
320 | contributions from the south and east rivers, and with the lowest | 320 | contributions from the south and east rivers, and with the lowest | ||
321 | contributions from the northwestern rivers. Finally, the combined | 321 | contributions from the northwestern rivers. Finally, the combined | ||
322 | nitrate input by all rivers was nearly two orders of magnitude (ca. | 322 | nitrate input by all rivers was nearly two orders of magnitude (ca. | ||
323 | 2.0 \u00d7 10^10 g N) lower than the estimated vertical re-supply of | 323 | 2.0 \u00d7 10^10 g N) lower than the estimated vertical re-supply of | ||
324 | nitrate to the surface during winter in offshore waters of HB (ca. 1.2 | 324 | nitrate to the surface during winter in offshore waters of HB (ca. 1.2 | ||
325 | \u00d7 10^12 g N). The potential contribution of river nutrients to | 325 | \u00d7 10^12 g N). The potential contribution of river nutrients to | ||
326 | new primary production is therefore small at HB scale but can be | 326 | new primary production is therefore small at HB scale but can be | ||
327 | significant locally.", | 327 | significant locally.", | ||
328 | "format": "PDF", | 328 | "format": "PDF", | ||
329 | "hash": "", | 329 | "hash": "", | ||
330 | "id": "d08f67a1-bad9-4081-9fb7-4ce0f7162195", | 330 | "id": "d08f67a1-bad9-4081-9fb7-4ce0f7162195", | ||
331 | "last_modified": null, | 331 | "last_modified": null, | ||
332 | "metadata_modified": "2021-11-06T14:16:06.382115", | 332 | "metadata_modified": "2021-11-06T14:16:06.382115", | ||
333 | "mimetype": null, | 333 | "mimetype": null, | ||
334 | "mimetype_inner": null, | 334 | "mimetype_inner": null, | ||
335 | "name": "Nutrient inputs from subarctic rivers into the Hudson | 335 | "name": "Nutrient inputs from subarctic rivers into the Hudson | ||
336 | Bay system", | 336 | Bay system", | ||
337 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 337 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
338 | "position": 4, | 338 | "position": 4, | ||
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342 | "state": "active", | 342 | "state": "active", | ||
343 | "url": | 343 | "url": | ||
344 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36108", | 344 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36108", | ||
345 | "url_type": null | 345 | "url_type": null | ||
346 | }, | 346 | }, | ||
347 | { | 347 | { | ||
348 | "cache_last_updated": null, | 348 | "cache_last_updated": null, | ||
349 | "cache_url": null, | 349 | "cache_url": null, | ||
350 | "created": "2021-11-06T17:33:15.579474", | 350 | "created": "2021-11-06T17:33:15.579474", | ||
351 | "datastore_active": false, | 351 | "datastore_active": false, | ||
352 | "datastore_contains_all_records_of_source_file": false, | 352 | "datastore_contains_all_records_of_source_file": false, | ||
353 | "description": "**Goals**\r\n\r\n- Present the first year-round | 353 | "description": "**Goals**\r\n\r\n- Present the first year-round | ||
354 | observations of the Hudson Strait inflow\r\n\r\n- Determine Hudson | 354 | observations of the Hudson Strait inflow\r\n\r\n- Determine Hudson | ||
355 | Strait inflow source waters\r\n\r\n- Estimate Hudson Strait inflow | 355 | Strait inflow source waters\r\n\r\n- Estimate Hudson Strait inflow | ||
356 | pathways within the Hudson Bay Complex\r\n", | 356 | pathways within the Hudson Bay Complex\r\n", | ||
357 | "format": "PPTX", | 357 | "format": "PPTX", | ||
358 | "hash": "", | 358 | "hash": "", | ||
359 | "id": "8048394d-a741-4091-bab1-98ac0fe2d2b2", | 359 | "id": "8048394d-a741-4091-bab1-98ac0fe2d2b2", | ||
360 | "last_modified": null, | 360 | "last_modified": null, | ||
361 | "metadata_modified": "2021-11-06T17:58:47.686467", | 361 | "metadata_modified": "2021-11-06T17:58:47.686467", | ||
362 | "mimetype": null, | 362 | "mimetype": null, | ||
363 | "mimetype_inner": null, | 363 | "mimetype_inner": null, | ||
364 | "name": "Hudson Strait Inflow: Structure and Variability", | 364 | "name": "Hudson Strait Inflow: Structure and Variability", | ||
365 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | 365 | "package_id": "51d3a499-75bd-4662-97e3-0d31d9fcb8dc", | ||
366 | "position": 5, | 366 | "position": 5, | ||
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370 | "state": "active", | 370 | "state": "active", | ||
371 | "url": | 371 | "url": | ||
372 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36111", | 372 | "https://mspace.lib.umanitoba.ca/xmlui/handle/1993/36111", | ||
373 | "url_type": null | 373 | "url_type": null | ||
374 | } | 374 | } | ||
375 | ], | 375 | ], | ||
376 | "rightsIdentifier": "CC-BY-4.0", | 376 | "rightsIdentifier": "CC-BY-4.0", | ||
377 | "rightsIdentifierScheme": "SPDX", | 377 | "rightsIdentifierScheme": "SPDX", | ||
378 | "rightsSchemeURI": "https://spdx.org/licenses", | 378 | "rightsSchemeURI": "https://spdx.org/licenses", | ||
379 | "rightsURI": "https://spdx.org/licenses/CC-BY-4.0.html", | 379 | "rightsURI": "https://spdx.org/licenses/CC-BY-4.0.html", | ||
380 | "schemeURI": "", | 380 | "schemeURI": "", | ||
381 | "state": "active", | 381 | "state": "active", | ||
382 | "subjectScheme": "", | 382 | "subjectScheme": "", | ||
383 | "tags": [ | 383 | "tags": [ | ||
384 | { | 384 | { | ||
385 | "display_name": "Albedo", | 385 | "display_name": "Albedo", | ||
386 | "id": "2f4d13d8-0144-46f5-9eb5-c7ae9e1d46b7", | 386 | "id": "2f4d13d8-0144-46f5-9eb5-c7ae9e1d46b7", | ||
387 | "name": "Albedo", | 387 | "name": "Albedo", | ||
388 | "state": "active", | 388 | "state": "active", | ||
389 | "vocabulary_id": null | 389 | "vocabulary_id": null | ||
390 | }, | 390 | }, | ||
391 | { | 391 | { | ||
392 | "display_name": "Climate change", | 392 | "display_name": "Climate change", | ||
393 | "id": "7a73cfd0-cc0f-4a58-93b8-c71202545a3e", | 393 | "id": "7a73cfd0-cc0f-4a58-93b8-c71202545a3e", | ||
394 | "name": "Climate change", | 394 | "name": "Climate change", | ||
395 | "state": "active", | 395 | "state": "active", | ||
396 | "vocabulary_id": null | 396 | "vocabulary_id": null | ||
397 | }, | 397 | }, | ||
398 | { | 398 | { | ||
399 | "display_name": "Hudson Bay", | 399 | "display_name": "Hudson Bay", | ||
400 | "id": "e8708f68-d619-4444-8951-96582b048848", | 400 | "id": "e8708f68-d619-4444-8951-96582b048848", | ||
401 | "name": "Hudson Bay", | 401 | "name": "Hudson Bay", | ||
402 | "state": "active", | 402 | "state": "active", | ||
403 | "vocabulary_id": null | 403 | "vocabulary_id": null | ||
404 | }, | 404 | }, | ||
405 | { | 405 | { | ||
406 | "display_name": "Hydrology", | 406 | "display_name": "Hydrology", | ||
407 | "id": "0b28b046-9102-4256-868b-17af1322f2f1", | 407 | "id": "0b28b046-9102-4256-868b-17af1322f2f1", | ||
408 | "name": "Hydrology", | 408 | "name": "Hydrology", | ||
409 | "state": "active", | 409 | "state": "active", | ||
410 | "vocabulary_id": null | 410 | "vocabulary_id": null | ||
411 | }, | 411 | }, | ||
412 | { | 412 | { | ||
413 | "display_name": "James Bay", | 413 | "display_name": "James Bay", | ||
414 | "id": "bb56cf12-bf82-4c14-93b0-fd31f4e0f6e2", | 414 | "id": "bb56cf12-bf82-4c14-93b0-fd31f4e0f6e2", | ||
415 | "name": "James Bay", | 415 | "name": "James Bay", | ||
416 | "state": "active", | 416 | "state": "active", | ||
417 | "vocabulary_id": null | 417 | "vocabulary_id": null | ||
418 | }, | 418 | }, | ||
419 | { | 419 | { | ||
420 | "display_name": "Modeling", | 420 | "display_name": "Modeling", | ||
421 | "id": "9f98c8ac-b485-4348-a112-1a57cc809e6d", | 421 | "id": "9f98c8ac-b485-4348-a112-1a57cc809e6d", | ||
422 | "name": "Modeling", | 422 | "name": "Modeling", | ||
423 | "state": "active", | 423 | "state": "active", | ||
424 | "vocabulary_id": null | 424 | "vocabulary_id": null | ||
425 | }, | 425 | }, | ||
426 | { | 426 | { | ||
427 | "display_name": "Nutrients", | 427 | "display_name": "Nutrients", | ||
428 | "id": "44265c2a-a639-4779-9481-478b0d6262ac", | 428 | "id": "44265c2a-a639-4779-9481-478b0d6262ac", | ||
429 | "name": "Nutrients", | 429 | "name": "Nutrients", | ||
430 | "state": "active", | 430 | "state": "active", | ||
431 | "vocabulary_id": null | 431 | "vocabulary_id": null | ||
432 | }, | 432 | }, | ||
433 | { | 433 | { | ||
434 | "display_name": "Ocean currents", | 434 | "display_name": "Ocean currents", | ||
435 | "id": "56242754-3dde-4386-bbf0-7ae74678361c", | 435 | "id": "56242754-3dde-4386-bbf0-7ae74678361c", | ||
436 | "name": "Ocean currents", | 436 | "name": "Ocean currents", | ||
437 | "state": "active", | 437 | "state": "active", | ||
438 | "vocabulary_id": null | 438 | "vocabulary_id": null | ||
439 | }, | 439 | }, | ||
440 | { | 440 | { | ||
441 | "display_name": "Primary production", | 441 | "display_name": "Primary production", | ||
442 | "id": "568c406b-0974-4083-a7e8-794d5a73fade", | 442 | "id": "568c406b-0974-4083-a7e8-794d5a73fade", | ||
443 | "name": "Primary production", | 443 | "name": "Primary production", | ||
444 | "state": "active", | 444 | "state": "active", | ||
445 | "vocabulary_id": null | 445 | "vocabulary_id": null | ||
446 | }, | 446 | }, | ||
447 | { | 447 | { | ||
448 | "display_name": "Rivers", | 448 | "display_name": "Rivers", | ||
449 | "id": "9e507343-6263-49ba-b1a4-e4fd2902d311", | 449 | "id": "9e507343-6263-49ba-b1a4-e4fd2902d311", | ||
450 | "name": "Rivers", | 450 | "name": "Rivers", | ||
451 | "state": "active", | 451 | "state": "active", | ||
452 | "vocabulary_id": null | 452 | "vocabulary_id": null | ||
453 | }, | 453 | }, | ||
454 | { | 454 | { | ||
455 | "display_name": "Satellite imagery", | 455 | "display_name": "Satellite imagery", | ||
456 | "id": "43456d7a-52ae-4390-acee-c0f0938d777c", | 456 | "id": "43456d7a-52ae-4390-acee-c0f0938d777c", | ||
457 | "name": "Satellite imagery", | 457 | "name": "Satellite imagery", | ||
458 | "state": "active", | 458 | "state": "active", | ||
459 | "vocabulary_id": null | 459 | "vocabulary_id": null | ||
460 | }, | 460 | }, | ||
461 | { | 461 | { | ||
462 | "display_name": "Sea ice", | 462 | "display_name": "Sea ice", | ||
463 | "id": "44971f11-ef93-4a43-9900-f32da30b84f7", | 463 | "id": "44971f11-ef93-4a43-9900-f32da30b84f7", | ||
464 | "name": "Sea ice", | 464 | "name": "Sea ice", | ||
465 | "state": "active", | 465 | "state": "active", | ||
466 | "vocabulary_id": null | 466 | "vocabulary_id": null | ||
467 | }, | 467 | }, | ||
468 | { | 468 | { | ||
469 | "display_name": "Sediments", | 469 | "display_name": "Sediments", | ||
470 | "id": "bc84fcae-7063-4f07-b8c2-08c5c9e7fadf", | 470 | "id": "bc84fcae-7063-4f07-b8c2-08c5c9e7fadf", | ||
471 | "name": "Sediments", | 471 | "name": "Sediments", | ||
472 | "state": "active", | 472 | "state": "active", | ||
473 | "vocabulary_id": null | 473 | "vocabulary_id": null | ||
474 | } | 474 | } | ||
475 | ], | 475 | ], | ||
476 | "theme": [ | 476 | "theme": [ | ||
477 | "3707ff10-6424-4858-9ec9-7d67b38831b3", | 477 | "3707ff10-6424-4858-9ec9-7d67b38831b3", | ||
478 | "8f8cd877-b037-4b1a-b928-f86d9e093741", | 478 | "8f8cd877-b037-4b1a-b928-f86d9e093741", | ||
479 | "98238b1c-5be8-41ad-8c6e-74cdc4f5f369" | 479 | "98238b1c-5be8-41ad-8c6e-74cdc4f5f369" | ||
480 | ], | 480 | ], | ||
481 | "title": "BaySys Conference Posters & Presentations", | 481 | "title": "BaySys Conference Posters & Presentations", | ||
482 | "type": "publication", | 482 | "type": "publication", | ||
483 | "url": null, | 483 | "url": null, | ||
484 | "version": "1.0" | 484 | "version": "1.0" | ||
485 | } | 485 | } |