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    {
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      "affiliation": "",
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      "affiliation": "",
            
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      "creatorName": "Landry, David",
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      "creatorName": "Landry, David",
            
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      "email": "david.landry@umanitoba.ca",
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      "email": "david.landry@umanitoba.ca",
            
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      "nameIdentifier": "",
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      "nameIdentifier": "",
            
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      "nameType": "Personal"
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      "nameType": "Personal"
            
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    }
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  ],
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  ],
            
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  "PublicationYear": "2021",
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  "PublicationYear": "2021",
            
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  "Publisher": "BaySys",
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  "Publisher": "BaySys",
            
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  "ResourceType": "field logs",
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  "ResourceType": "field logs",
            
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  "Rights": "Creative Commons Attribution 4.0 International",
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  "Rights": "Creative Commons Attribution 4.0 International",
            
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  "creator_user_id": "c3ad971e-75e0-4e57-b825-8ed25f306937",
            
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  "descriptionType": "Abstract",
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  "descriptionType": "Abstract",
            
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  "groups": [
            
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    {
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    {
            
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      "description": "The cryosphere encompasses all the parts of the 
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      "description": "The cryosphere encompasses all the parts of the 
            
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Earth system where water is in solid form, including ice sheets, ice 
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Earth system where water is in solid form, including ice sheets, ice 
            
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shelves, glaciers, snow cover, permafrost (frozen ground), sea ice, 
31
shelves, glaciers, snow cover, permafrost (frozen ground), sea ice, 
            
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and river and lake ice. The cryosphere exerts an important influence 
32
and river and lake ice. The cryosphere exerts an important influence 
            
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on Earth\u2019s climate. Image and description from 
33
on Earth\u2019s climate. Image and description from 
            
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https://climate.copernicus.eu.",
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https://climate.copernicus.eu.",
            
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      "display_name": "Cryosphere",
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      "display_name": "Cryosphere",
            
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      "id": "3707ff10-6424-4858-9ec9-7d67b38831b3",
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      "id": "3707ff10-6424-4858-9ec9-7d67b38831b3",
            
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      "image_display_url": 
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      "image_display_url": 
            
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loads/group/2021-11-01-152857.585996C3SindicatorscryosphereFig10.png",
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loads/group/2021-11-01-152857.585996C3SindicatorscryosphereFig10.png",
            
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      "name": "cryosphere",
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      "name": "cryosphere",
            
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      "title": "Cryosphere"
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      "title": "Cryosphere"
            
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    },
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    },
            
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    {
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    {
            
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      "description": "Female Daphnia magna carrying a resting egg 
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      "description": "Female Daphnia magna carrying a resting egg 
            
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(\"ephippium\"). The black ephippium is part of the carapace and 
44
(\"ephippium\"). The black ephippium is part of the carapace and 
            
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contains usually two sexual eggs. Photo by Dieter Ebert, Basel, 
45
contains usually two sexual eggs. Photo by Dieter Ebert, Basel, 
            
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Switzerland. \r\nCC BY-SA 4.0 Licence\r\n",
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Switzerland. \r\nCC BY-SA 4.0 Licence\r\n",
            
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      "display_name": "Marine",
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      "display_name": "Marine",
            
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      "id": "98238b1c-5be8-41ad-8c6e-74cdc4f5f369",
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      "image_display_url": 
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ata/uploads/group/2021-10-31-211516.365746ofinspireoceanographic.svg",
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ata/uploads/group/2021-10-31-211516.365746ofinspireoceanographic.svg",
            
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      "name": "marine",
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      "name": "marine",
            
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      "title": "Marine"
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      "title": "Marine"
            
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    }
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  "metadata_modified": "2021-11-04T22:53:47.746297",
            
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  "name": "baysys-field-rep",
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  "name": "baysys-field-rep",
            
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  "notes": "Field reports for the BaySys project over the years 2016 
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  "notes": "Field reports for the BaySys project over the years 2016 
            
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to 2018. ",
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to 2018. ",
            
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  "organization": {
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  "organization": {
            
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    "approval_status": "approved",
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    "approval_status": "approved",
            
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    "created": "2017-07-21T13:15:49.935872",
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    "created": "2017-07-21T13:15:49.935872",
            
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    "description": "The Centre for Earth Observation Science (CEOS) 
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    "description": "The Centre for Earth Observation Science (CEOS) 
            
74
was established in 1994 with a mandate to research, preserve and 
74
was established in 1994 with a mandate to research, preserve and 
            
75
communicate knowledge of Earth system processes using the technologies 
75
communicate knowledge of Earth system processes using the technologies 
            
76
of Earth Observation Science. Research is multidisciplinary and 
76
of Earth Observation Science. Research is multidisciplinary and 
            
77
collaborative seeking to understand the complex interrelationships 
77
collaborative seeking to understand the complex interrelationships 
            
78
between elements of Earth systems, and how these systems will likely 
78
between elements of Earth systems, and how these systems will likely 
            
79
respond to climate change. Although researchers have worked in many 
79
respond to climate change. Although researchers have worked in many 
            
80
regions, the Arctic marine system has always been a unifying focus of 
80
regions, the Arctic marine system has always been a unifying focus of 
            
81
activity.\r\n\r\nIn 2012, CEOS, along with the Greenland Climate 
81
activity.\r\n\r\nIn 2012, CEOS, along with the Greenland Climate 
            
82
Research Centre (GCRC, Nuuk, Greenland) and the Arctic Research Centre 
82
Research Centre (GCRC, Nuuk, Greenland) and the Arctic Research Centre 
            
83
(ARC, Aarhus, Denmark) established the Arctic Science Partnership, 
83
(ARC, Aarhus, Denmark) established the Arctic Science Partnership, 
            
84
thereby integrating academic and research initiatives.\r\n\r\nAreas of 
84
thereby integrating academic and research initiatives.\r\n\r\nAreas of 
            
85
existing research activity are divided among key themes:\r\n\r\nArctic 
85
existing research activity are divided among key themes:\r\n\r\nArctic 
            
86
Anthropology/Paleoclimatology: LiDAR scanning and digital site 
86
Anthropology/Paleoclimatology: LiDAR scanning and digital site 
            
87
preservation, archaeo-geophysics, permafrost degredation, lithic 
87
preservation, archaeo-geophysics, permafrost degredation, lithic 
            
88
morphometrics, zooarchaeology, proxy studies, paleodistribution of sea 
88
morphometrics, zooarchaeology, proxy studies, paleodistribution of sea 
            
89
ice, landscape learning, Paleo-Eskimo culture, Thule Inuit culture, 
89
ice, landscape learning, Paleo-Eskimo culture, Thule Inuit culture, 
            
90
ethnographic analogy, traditional knowledge, climate change and 
90
ethnographic analogy, traditional knowledge, climate change and 
            
91
northern heritage resource management.\r\n\r\nAtmospheric 
91
northern heritage resource management.\r\n\r\nAtmospheric 
            
92
Studies/Meteorology: Boundary layer, precipitation, clouds, storms and 
92
Studies/Meteorology: Boundary layer, precipitation, clouds, storms and 
            
93
extreme weather, circulation, eddy correlations, polar vortex, 
93
extreme weather, circulation, eddy correlations, polar vortex, 
            
94
climate, teleconnections, geophysical fluid dynamics, flux and energy 
94
climate, teleconnections, geophysical fluid dynamics, flux and energy 
            
95
budgets, ocean-sea ice-atmosphere interface, radiative transfer, ice 
95
budgets, ocean-sea ice-atmosphere interface, radiative transfer, ice 
            
96
albedo feedback, cloud radiative forcing, pCO2. 
96
albedo feedback, cloud radiative forcing, pCO2. 
            
97
\r\n\r\nBiogeochemistry: Organic carbon, greenhouse gases, bubbles, 
97
\r\n\r\nBiogeochemistry: Organic carbon, greenhouse gases, bubbles, 
            
98
Ikaite, carbonate chemistry, CO2 fluxes, mercury and other trace 
98
Ikaite, carbonate chemistry, CO2 fluxes, mercury and other trace 
            
99
metals, minerals, hydrocarbons, brine processes, otolith 
99
metals, minerals, hydrocarbons, brine processes, otolith 
            
100
microchemistry, sediments, biomarkers. \r\n\r\nContaminants: Mercury, 
100
microchemistry, sediments, biomarkers. \r\n\r\nContaminants: Mercury, 
            
101
trace metals, PAHs, source, transport, transformation, pathways, 
101
trace metals, PAHs, source, transport, transformation, pathways, 
            
102
bioaccumulations, marine ecosystems, marine chemistry. \r\nEarth 
102
bioaccumulations, marine ecosystems, marine chemistry. \r\nEarth 
            
103
Observation Science: Active and passive microwave, LiDAR, EM 
103
Observation Science: Active and passive microwave, LiDAR, EM 
            
104
induction, spatial-temporal analysis, forward and inverse scattering 
104
induction, spatial-temporal analysis, forward and inverse scattering 
            
105
models, complex permittivity, ocean colour, ocean surface roughness, 
105
models, complex permittivity, ocean colour, ocean surface roughness, 
            
106
NIR, TIR, satellite telemetry, GPS. Ice-Associated Biology: 
106
NIR, TIR, satellite telemetry, GPS. Ice-Associated Biology: 
            
107
Biophysical processes, primary production; ice algae, ice 
107
Biophysical processes, primary production; ice algae, ice 
            
108
microbiology, bio-optics, under-ice phytoplankton. \r\n\r\nInland 
108
microbiology, bio-optics, under-ice phytoplankton. \r\n\r\nInland 
            
109
Lakes and Waters: Hydrologic connectivity, watershed systems, sediment 
109
Lakes and Waters: Hydrologic connectivity, watershed systems, sediment 
            
110
transport, nutrient transport, contaminants, landscape processes, 
110
transport, nutrient transport, contaminants, landscape processes, 
            
111
remote sensing, freshwater-marine coupling. Marine Mammals: Seals, 
111
remote sensing, freshwater-marine coupling. Marine Mammals: Seals, 
            
112
whales, habitat, conservation, satellite telemetry, distribution, 
112
whales, habitat, conservation, satellite telemetry, distribution, 
            
113
population studies, prey behaviour, bioacoustics.\r\n\r\nModelling: 
113
population studies, prey behaviour, bioacoustics.\r\n\r\nModelling: 
            
114
Simulation of sea ice and oceanic regional processes, Nucleus for 
114
Simulation of sea ice and oceanic regional processes, Nucleus for 
            
115
European Modelling of the Ocean (NEMO), ice-ocean modelling and 
115
European Modelling of the Ocean (NEMO), ice-ocean modelling and 
            
116
interactions, hind cast simulations and projections for sea ice state 
116
interactions, hind cast simulations and projections for sea ice state 
            
117
and ocean variables based on CMIP5 scenarios and MIROC5 forcing, 
117
and ocean variables based on CMIP5 scenarios and MIROC5 forcing, 
            
118
validation.\r\n\r\nOceanography: Circulation, temperature, in-flow and 
118
validation.\r\n\r\nOceanography: Circulation, temperature, in-flow and 
            
119
out-flow shelves, water dynamics, microturbulence, Beaufort Gyre, eddy 
119
out-flow shelves, water dynamics, microturbulence, Beaufort Gyre, eddy 
            
120
correlations.\r\n\r\nSea Ice Geophysics:Thermodynamic and dynamic 
120
correlations.\r\n\r\nSea Ice Geophysics:Thermodynamic and dynamic 
            
121
processes, extreme ice features and hazards, snow, ridges, 
121
processes, extreme ice features and hazards, snow, ridges, 
            
122
polynyas.\r\n\r\nTraditional and Local Knowledge: Indigenous cultures, 
122
polynyas.\r\n\r\nTraditional and Local Knowledge: Indigenous cultures, 
            
123
Inuit, Inuvialuit, oral history, toponomy, mobility and settlement, 
123
Inuit, Inuvialuit, oral history, toponomy, mobility and settlement, 
            
124
hunting, food security, sea ice use, community-based research, 
124
hunting, food security, sea ice use, community-based research, 
            
125
community-based monitoring, two ways of knowing.",
125
community-based monitoring, two ways of knowing.",
            
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      "description": "Report on the  2016  mooring  field  program  
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      "description": "Report on the  2016  mooring  field  program  
            
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took  place  in  southern  Hudson  Bay  from  September  26 
160
took  place  in  southern  Hudson  Bay  from  September  26 
            
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(Churchill)  to  October  4  (Kujjaurapik) ",
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(Churchill)  to  October  4  (Kujjaurapik) ",
            
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      "name": "BaySys - Des Groseilliers Cruise Report 2016",
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      "name": "BaySys - Des Groseilliers Cruise Report 2016",
            
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80e21361f326/download/baysys-des-groseilliers-cruise-report-2016.pdf",
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      "description": "In late September 2016, five oceanographic 
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      "description": "In late September 2016, five oceanographic 
            
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moorings were deployed in the eastern Hudson Bay and at the entrance 
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moorings were deployed in the eastern Hudson Bay and at the entrance 
            
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to James Bay (Figure 1). These moorings were supposed to be recovered 
188
to James Bay (Figure 1). These moorings were supposed to be recovered 
            
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in summer 2017 during the BaySys cruise onboard CCGS Amundsen or White 
189
in summer 2017 during the BaySys cruise onboard CCGS Amundsen or White 
            
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Diamond - a vessel refurnished in 2017 for the Churchill Marine 
190
Diamond - a vessel refurnished in 2017 for the Churchill Marine 
            
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Observatory. Later, a decision on turning the moorings from White 
191
Observatory. Later, a decision on turning the moorings from White 
            
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Diamond instead of recovery was made. Unfortunately, the slow progress 
192
Diamond instead of recovery was made. Unfortunately, the slow progress 
            
193
of ship\u2019s inspection from Transport Canada caused multiple delays 
193
of ship\u2019s inspection from Transport Canada caused multiple delays 
            
194
of ship\u2019s departure from Prince Edward Island and the 2017 cruise 
194
of ship\u2019s departure from Prince Edward Island and the 2017 cruise 
            
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was cancelled. Because of the critical role of these moorings for the 
195
was cancelled. Because of the critical role of these moorings for the 
            
196
scientific objectives of oncoming Amundsen cruise in spring 2018, the 
196
scientific objectives of oncoming Amundsen cruise in spring 2018, the 
            
197
opportunistic cruise onboard CCGS Henry Larsen was conducted in 
197
opportunistic cruise onboard CCGS Henry Larsen was conducted in 
            
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October 26 \u2013 November 1, 2017 in order to maintain the 
198
October 26 \u2013 November 1, 2017 in order to maintain the 
            
199
uninterrupted measurements. The goals for this short cruise were to 
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uninterrupted measurements. The goals for this short cruise were to 
            
200
retrieve and re-deploy as many BaySys moorings as possible accompanied 
200
retrieve and re-deploy as many BaySys moorings as possible accompanied 
            
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with the concurrent CTD and water sampling.\r\n",
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with the concurrent CTD and water sampling.\r\n",
            
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      "description": "Churchill River and mobile ice survey, February 
            
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1 to February 15, 2017 in Churchill Manitoba.",
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1 to February 15, 2017 in Churchill Manitoba.",
            
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      "name": "BaySys - Churchill Field Report 2017",
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      "name": "BaySys - Churchill Field Report 2017",
            
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      "description": "To investigate the nature of sediment, organic 
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      "description": "To investigate the nature of sediment, organic 
            
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matter, and mercury contributions over time to lakes in theNelson 
253
matter, and mercury contributions over time to lakes in theNelson 
            
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River system, the goal of this \feld program was to collect sediment 
254
River system, the goal of this \feld program was to collect sediment 
            
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cores and water samples from 2sites within the pre- and 
255
cores and water samples from 2sites within the pre- and 
            
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post-impoundment waterbody extents at 5 lakes in the Nelson River 
256
post-impoundment waterbody extents at 5 lakes in the Nelson River 
            
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watershed:\r\n\r\nOn- System\r\n-Stephens Lake\r\n-Threepoint 
257
watershed:\r\n\r\nOn- System\r\n-Stephens Lake\r\n-Threepoint 
            
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Lake\r\n-Split Lake\r\n\r\nOff System\r\n-Leftrook lake\r\n-Assean 
258
Lake\r\n-Split Lake\r\n\r\nOff System\r\n-Leftrook lake\r\n-Assean 
            
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lake",
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lake",
            
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      "name": "Sediment Coring and Water Quality Fieldwork Summary- 
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      "name": "Sediment Coring and Water Quality Fieldwork Summary- 
            
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March 1-6 and April 2-5",
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March 1-6 and April 2-5",
            
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in southwestern Hudson Bay, near the mouth of the Nelson Estuary. The 
            
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program was based out of the Nanuk Polar Bear Lodge, which is located 
            
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near the shore of Hudson Bay between the mouth of the Nelson River and 
            
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Cape Tatnam. The seasonal ice cover that forms annually within Hudson 
            
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Bay is composed of both mobile pack ice and landfast ice that forms a 
            
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narrow band of stationary ice in the near shore areas of Hudson Bay. 
            
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In southwestern Hudson Bay the landfast ice provided an excellent 
            
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opportunity to study the freshwater-marine coupling near the mouth of 
            
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the Nelson River. The area is typically ice covered from November to 
            
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June, though the landfast ice cover typically becomes unstable is 
            
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      "name": "Rivers",
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  "title": "Baysys Field Reports",
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  "title": "Baysys Field Reports",
            
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