cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.18739/a2kw57k0t
title: Seasonal soil temperatures from a Circumarctic Active Layer Monitoring (CALM) grid, Barrow, Alaska, 2016

description: Seasonal soil temperature measurements were collected during the 2016 growing season at each Circumarctic Active Layer Monitoring (CALM) grid subset plot (30) in Utqiaġvik (formerly Barrow), Alaska. At each plot one temperature measurement was acquired, the date, start and end times, and the people present were also recorded. Soil temperature measurements were taken outside of every plot on the northeastern most corner in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales.
DOI: 10.6084/m9.figshare.27888912.v1
title: Supplementary Material for: Diabetic striatopathy (hyperglycemic hemichorea-hemiballismus syndrome) in a young patient with type 1 diabetes mellitus in Dar es Salaam, Tanzania: a case report

description: Introduction:
Diabetic striatopathy, or nonketotic hyperglycemic hemichorea-hemiballismus syndrome, is a rare movement disorder linked to poorly controlled diabetes mellitus. It predominantly affects older women with type 2 diabetes mellitus and presents with characteristic basal ganglia abnormalities on CT and MRI. Even rarer is the presentation in a young patient, which may pose diagnostic and management challenges.

Case Presentation:
We report a 17-year-old male with poorly controlled type 1 diabetes mellitus presenting with left-sided hemichorea-hemiballismus of acute onset associated with hyperglycemia without ketoacidosis. Brain imaging revealed increased attenuation in the right caudate and putamen on CT and hyperintensity on T1-weighted MRI, consistent with diabetic striatopathy. The abnormal movements abated after one month through dietary counseling, increased insulin dosage, and anti-chorea therapy.

Conclusion:
Diabetic striatopathy may occur in young patients with type 1 diabetes mellitus. In resource-limited settings, its management can be challenging. There is a need for increased awareness among physicians of this potentially reversible condition, especially when seeing atypical patient populations. Strict glycemic control is an essential part of treatment.
DOI: 10.18739/a2g737474
title: Seasonal soil temperatures from a Mobile Instrumented System Platform (MISP) grid, Atqasuk, Alaska, 2016

description: Seasonal soil temperature measurements were collected during the 2016 growing season at each Mobile Instrumented System Platform (MISP) grid meter in Atqasuk, Alaska. At each meter one soil temperature measurement was acquired, the date, start and end times, and the people present were also recorded. Soil temperature measurements were taken on the north side of the grid in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales.
DOI: 10.18739/a2bg2hb4g
title: Seasonal soil moisture measurements from a Mobile Instrumented System Platform (MISP) grid, Atqasuk, Alaska, 2016

description: Seasonal soil moisture measurements were collected during the 2016 growing season at each Mobile Instrumented System Platform (MISP) grid meter in Atqasuk, Alaska. At each meter one soil moisture measurement was acquired, the date, start and end times, and the people present were also recorded. Soil moisture measurements were taken on the north side of the grid between the matted trail and each white board in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales.
DOI: 10.18739/a26q1sj0b
title: Seasonal soil active layer measurements from a Circumarctic Active Layer Monitoring (CALM) grid, Barrow, Alaska, 2016

description: Seasonal active layer depth measurements were collected during the 2016 growing season at each Circumarctic Active Layer Monitoring (CALM) grid subset plot (30) in Utqiaġvik (formerly Barrow) Alaska. At each plot two depth measurements were acquired, the date, start and end times, and the people present were also recorded. Depth measurements were taken outside of every plot on the northeastern most corner in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales.
DOI: 10.18739/a22z12q6z
title: Seasonal active layer depth from a Mobile Instrumented System Platform (MISP) grid, Atqasuk, Alaska, 2016

description: Seasonal active layer depth measurements were collected during the 2016 growing season at each Mobile Instrumented System Platform (MISP) grid meter in Atqasuk, Alaska. At each meter two depth measurements were acquired, the date, start and end times, and the people present were also recorded. Depth measurements were taken on the north side of the grid in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales.
DOI: 10.18739/a2z60c319
title: Seasonal soil active layer measurements from a Mobile Instrumented System Platform (MISP) grid, Barrow, Alaska, 2016

description: Seasonal active layer depth measurements were collected during the 2016 growing season at each Mobile Instrumented System Platform (MISP) grid meter in Utqiaġvik (formerly Barrow) Alaska. At each meter two depth measurements were acquired, the date, start and end times, and the people present were also recorded. Depth measurements were taken on the north side of the grid in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales.
DOI: 10.18739/a2td9n870
title: Seasonal soil moisture measurements from a Mobile Instrumented System Platform (MISP) grid, Barrow, Alaska, 2016

description: Seasonal soil moisture measurements were collected during the 2016 growing season at each Mobile Instrumented System Platform (MISP) grid meter in Utqiaġvik (formerly Barrow), Alaska. At each meter one soil moisture measurement was acquired, the date, start and end times, and the people present were also recorded. Soil moisture measurements were taken on the north side of the grid in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales.
DOI: 10.18739/a2d795b84
title: Meteorological, Soil, Runoff, and Snowpack Data from Thermokarst Study Sites at Goldstream Creek, near Fairbanks, Alaska, 2015-2019

description: This project aims to define processes within the hydrology-permafrost-methane system at the lake- to watershed scale across the seasonal to millennial time scales. The study domain, Goldstream Valley, Interior Alaska, United States of America, offers a platform for process-oriented insights that are applicable for landscapes with discontinuous permafrost and thaw lakes, which are common in the sub-arctic region. One of the topics we are investigating is how and why the extent of permafrost has varied since the last ice age up until today and especially how the flow and storage of water has controlled (and been controlled by) permafrost. This dataset consists of meteorological, soil, runoff, and snowpack data from 2015 to 2019 from several hydro-meteorological stations within the Goldstream watershed.
DOI: 10.18739/a28g8fj40
title: Surface and underwater irradiance timeseries from the Stefansson Sound, Beaufort Sea, Alaska, 1984-2018.

description: In the nearshore Alaskan Beaufort Sea, discrete, isolated rocky habitats harbor biological communities that are unusually diverse for the region, with markedly different fauna and flora than found in the surrounding soft sediment areas. The boulder fields also support tightly linked food webs, with connections to higher trophic levels such as fishes and seals. These systems are highly vulnerable to disturbances, including sedimentation from human activities and coastal erosion, fluctuations in salinity from seasonal river discharge, and temperature increases from heat influx originating at lower latitudes and from atmospheric warming. Spatial isolation of these boulder fields and the slow development of benthic communities limit ecosystem recovery from disturbance. To assess the possible ecological effects of such environmental disturbances, this field program undertook an investigation of the biological communities and environmental conditions across the Stefansson Sound Boulder Patch, the largest of the Beaufort Sea nearshore boulder fields. 
 The overlying objectives of this program were to: 1) monitor incident and in situ photosynthetically active radiation (PAR), salinity, temperature, currents, and pH to define the spatial variability in annual kelp productivity and biomass; 2) characterize benthic community structure changes across environmental gradients in the Boulder Patch and 3) collect annual measurements of kelp growth in the Boulder Patch to provide a nearly continuous record of kelp growth since 1976. Within and in addition to these objectives, individual research projects were completed, using experimental approaches, timeseries analysis and historical data to gain an in depth understanding of mechanisms (past and present) that resulted in the Boulder Patch community we see today and how this community may vary in future conditions.
 These datasets here result from ecosystem studies and monitoring that took place from 1976 to 2018 at multiple site in Stefansson Sound, Alaska.
 To understand spatiotemporal variability in underwater light environment, photosyntheically active radiation (PAR, 400-700 nanometers) was measured from moorings on the benthos at multiple locations in Stefansson Sound, Alaska using LICOR spherical quantum sensors, and at an adjacent site on land for incident PAR using LICOR cosine sensors. The overall dataset spans from 1984 to 2018, though there are gaps that vary from days to multiple years, depending on the location.
DOI: 10.18739/a24q7qr0v
title: Arctic Nearshore Impact Monitoring in the Development Area (ANIMIDA) III: The Boulder Patch and other Kelp Communities in the Development Area. Ecosystem monitoring data collected from the Boulder Patch, Stefansson Sound, Alaska (1976-2018).

description: In the nearshore Alaskan Beaufort Sea, discrete, isolated rocky habitats harbor biological communities that are unusually diverse for the region, with markedly different fauna and flora than found in the surrounding soft sediment areas. The boulder fields also support tightly linked food webs, with connections to higher trophic levels such as fishes and seals. These systems are highly vulnerable to disturbances, including sedimentation from human activities and coastal erosion, fluctuations in salinity from seasonal river discharge, and temperature increases from heat influx originating at lower latitudes and from atmospheric warming. Spatial isolation of these boulder fields and the slow development of benthic communities limit ecosystem recovery from disturbance. To assess the possible ecological effects of such environmental disturbances, this field program undertook an investigation of the biological communities and environmental conditions across the Stefansson Sound Boulder Patch, the largest of the Beaufort Sea nearshore boulder fields. 
 The overlying objectives of this program were to: 1) monitor incident and in situ photosynthetically active radiation (PAR), salinity, temperature, currents, and pH to define the spatial variability in annual kelp productivity and biomass; 2) characterize benthic community structure changes across environmental gradients in the Boulder Patch and 3) collect annual measurements of kelp growth in the Boulder Patch to provide a nearly continuous record of kelp growth since 1976. Within and in addition to these objectives, individual research projects were completed, using experimental approaches, timeseries analysis and historical data to gain an in depth understanding of mechanisms (past and present) that resulted in the Boulder Patch community we see today and how this community may vary in future conditions.
 These datasets here result from ecosystem studies and monitoring that took place from 1976 to 2018 at multiple site in Stefansson Sound, Alaska.
DOI: 10.18739/a23r0pv05
title: North Slope Alaska Ancient Megafauna Bones, Willow and Stratigraphic Data 2014-2018

description: These data are a comprehensive collection from the Pleistocene in Beringia in northern Alaska. The carbon-14 (14C) dates and isotopic data from megafaunal bones, willow and stratigraphic samples allow a reconstruction of the climate, zoological and botanical history of the region during the last 40,000 years. We have used these data in published manuscripts:
 Gaglioti, B.V., Mann, D.H., Groves, P., Kunz, M.L., Farquharson, L.M., Reanier, R.E., Jones, B.M., Wooller, M.J., 2018. Aeolian stratigraphy describes ice-age paleoenvironments in unglaciated Arctic Alaska. Quat Sci Rev 182, 175-190.
 Gaglioti, B.V., Mann, D.H., Wooller, M.J., Jones, B.M., Wiles, G.C., Groves, P., Kunz, M.L., Baughman, C.A., Reanier, R.E., 2017. Younger-Dryas cooling and sea-ice feedbacks were prominent features of the Pleistocene-Holocene transition in Arctic Alaska. Quat Sci Rev 169, 330-343.
 Mann, D.H., Groves, P., Reanier, R.E., Gaglioti, B.V., Kunz, M.L., Shapiro, B., 2015. Life and extinction of megafauna in the ice-age Arctic. Proc. Natl. Acad. Sci. USA 112, 14301-14306.
 After developing a statistical approach to remove the age artifacts caused by radiocarbon calibration from a large series of dated megafaunal bones, we compared the temporal patterns of bone abundance with climate records. Megafaunal abundance tracked ice age climate, peaking during transitions from cold to warm periods. We used the oxygen isotope values of wood cellulose in living and sub-fossil willow shrubs (d18Owc) (Salix spp.) that have been radiocarbon-dated (14C) to produce a multi-millennial record of climatic change on Alaska's North Slope during the Pleistocene-Holocene transition. We described the stratigraphy and sedimentology of a yedoma deposit in Arctic Alaska (the Carter Section) dating to between 37,000 and 9000 calibrated radiocarbon years BP (37e9 ka) and containing detailed records of loess and sand-sheet sedimentation, soil development, carbon storage, and permafrost dynamics.
DOI: 10.18739/a2pn8xg4b
title: Legacy Organochlorine Pesticides (OCPs) from East Asia to the Arctic Ocean in 2016 and 2017

description: To provide updated field data on the global fate of organochlorine pesticides (OCPs) in the high Arctic Ocean region undergoing rapid climate change, 7 legacy OCPs, including 4 hexachlorocyclohexanes (HCHs) and 3 dichlorodiphenyltrichloroethanes (DDTs), in the surface seawater and atmosphere from East Asia to the high Arctic Ocean were investigated during 2 Arctic Research Expedition cruises in 2017 and 2016. Both the atmospheric and surface seawater samples were collected in the situ by the High-volume Solid-phase Extraction method. The sampling transects were along with East Asia, Northwest Pacific Ocean, Bering Sea, Chukchi Sea, and the Arctic Ocean. These data should be the first updated investigation of OCPs along the North Pacific Ocean to the Arctic Ocean transect in the past decade.
DOI: 10.71687/avid.ksa.109
title: KMD Elev (2018-2022)

description: KMD Elev løser de administrative opgaver, der er omkring elevernes stam- og undervisningsoplysninger, samt de administrative opgaver der er med undervisningspligten, adressekontrol, plejebørn/udenbys børn, skoleregister, aktuelt elevtal, skoleindskrivning, skolebestyrelsesvalg, transport/buskort, søskendeoplysninger, forældreoplysninger, elevernes fravær, handleplan, skolefritidsordning, klasseoprykning, prøveafvikling samt ungdomsskoletilbud.

Indeholder:
Systemet indeholder følgende hovedfunktioner: 1) Registrering af elevernes stam- og undervisningsoplysninger, 2) Registrering af standpunktskarakterer samt karakterer fra afgangsprøver, og 3) Registrering af oplysninger om skolerne.
DOI: 10.18739/a20000151
title: Thule, Greenland, water vapor isotopes (δ18O, δ2H, d-excess) and meteorological data, August 2017 - August 2019

description: This dataset contains quality checked and calibrated water vapor isotopic ratios for oxygen (δ18O) and hydrogen (δ2H), as well as the secondary isotopic variable of deuterium-excess. The data were taken at Thule Air Base, Greenland, between August 2017 and August 2019, using a Picarro L-2130i cavity ring-down spectroscopy isotope analyzer with Standards Delivery Module. Data here have been calibrated for machine accuracy and precision errors related to changing humidity values. Original measurements are made approximately 1 per second, and later aggregated into 10 minute, hourly, and daily means. Meteorological observations made at the SMT site of Thule Air Base and THU airport are also included here at 10 minute, hourly, and daily means. Full SMT meteorological data available at https://doi.org/10.1594/PANGAEA.895059.
 These data were collected to better understand the environmental controls on water isotopic variability in the High Arctic, including sea ice extent, synoptic moisture transport, and mesoscale winds. Thule is also part of the Arctic Water Isotope Network, a group of nine sites located around the Arctic Basin that measure water vapor isotopes in real time to track changes in the Pan-Arctic hydroclimate.
DOI: 10.15468/dl.2upw9s
title: Occurrence Download

description: A dataset containing 35 species occurrences available in GBIF matching the query:
{
 "and" : [
 "HasGeospatialIssue is false",
 "HasCoordinate is true",
 "OccurrenceStatus is Present",
 {
 "not" : {
 "BasisOfRecord" : [
 "is one of (Fossil, Living Specimen)"
 ]
 }
 },
 "TaxonKey is one of (Notoseris triflora (Hemsl.) C.Shih)"
 ]
}

 The dataset includes 35 records from 5 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0027825-241107131044228/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.18739/a2m32nb3b
title: Ice structure (optical televiewer) from Jarvis Glacier, Alaska, 2017

description: Ice sheets and alpine glaciers discharge primarily though streaming flow, so the dynamics of that flow is central to the overall mass balance of the cryosphere. In glaciers and ice streams, the resistance to flow at the bed is important, but equally important is the internal viscous strength of the ice near the margins. In many cases, the lateral margins support greater than 50% of the resisting stress. At present, there is moderate to high uncertainty of the factors controlling the viscous strength of streaming ice under natural conditions. Although experiments suggest that variations in the intensity and orientation of the crystallographic fabric can result in up to a ten-fold difference in flow strength, in-situ observational studies of the microstructural architecture of streaming ice number in the low single digits. Most microstructural and in-situ rheological studies come from ice divides, near sites of paleoclimate coring. To complement that work and provide insight into the dynamic influence of streaming ice margins, our study documented both temperature and microstructure across a strain gradient at the lateral margin of Jarvis (Creek) Glacier and related those observations to modeled and observed 3D velocity structure.
 The dataset included here is one component of the larger project: optical televiewer images of five boreholes, collected in spring 2017. Holes were drilled along a transect from less to more sheared ice, with the goal being to reach bed in at least two locations within the time constraints of the drilling season. We attempted six holes. The first (JA) and fifth (JE) reached bed. Others were limited by debris. All holes were imaged with the exception of the fourth (JD), which met refusal at 4m. The images that constitute this dataset are "unwrapped" 360-degree views of the borehole wall, such that planes in real space appear as sinusoids in televiewer images. As labeled in the images, south is at the center and north is at the edges. The numbers on the y-axis indicate depth in meters. For background, we also include a location map and core log in this dataset.
DOI: 10.18739/a2gb1xh9k
title: Ice microstructure (electron backscatter diffraction) from Jarvis Glacier, Alaska, 2017-2020

description: Ice sheets and alpine glaciers discharge primarily though streaming flow, so the dynamics of that flow is central to the overall mass balance of the cryosphere. In glaciers and ice streams, the resistance to flow at the bed is important, but equally important is the internal viscous strength of the ice near the margins. In many cases, the lateral margins support greater than 50% of the resisting stress. At present, there is moderate to high uncertainty of the factors controlling the viscous strength of streaming ice under natural conditions. Although experiments suggest that variations in the intensity and orientation of the crystallographic fabric can result in up to a ten-fold difference in flow strength, in-situ observational studies of the microstructural architecture of streaming ice number in the low single digits. Most microstructural and in-situ rheological studies come from ice divides, near sites of paleoclimate coring. To complement that work and provide insight into the dynamic influence of streaming ice margins, our study documented both temperature and microstructure across a strain gradient at the lateral margin of Jarvis (Creek) Glacier and related those observations to modeled and observed 3D velocity structure.
 The dataset included here is one component of the larger project described above: electron backscatter diffraction raw and processed data from two ice cores collected in spring 2017. Holes were drilled along a transect from less to more sheared ice, with the goal being to reach bed in at least two locations within the time constraints of the drilling season. We attempted six holes. The first (JA; 63.4750˚N, 145.6753˚W, 1621 m elevation), and fifth (JE; 63.4743˚N, 145.6766˚W, 1625 m elevation) appear to have reached bed, and those are the ones represented in this dataset. Other cores were limited by debris. All data were collected at 60 degree tilt using an EDAX-TSL electron backscatter diffraction (EBSD) system on a Tescan Vega II electron microscope. Raw data files (in text format, with .ang extension) are not tilt-corrected. In addition to the raw data, we include products derived from the EBSD data: one-point-per-grain orientation lists, and orientation tensors for each sample. For background, we also include a location map and core log.