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767 results for “switzerland”
Investigation of the Effects of C-Mill (Hocoma AG, Switzerland) Treadmill Training on Trunk Balance in Patients with Spinal Cord Injury
ClinicalTrials.gov study NCT06872931. IPD Sharing: NO. Countries: 1. Publications: 0.
Real World Study With Benralizumab in Severe Asthma in Switzerland
ClinicalTrials.gov study NCT03907137. IPD Sharing: NO. Countries: 1. Publications: 0.
Influence of Hospital Volume on Mortality and Length of Hospital Stay After Pancreatic Resection in Switzerland
ClinicalTrials.gov study NCT07022639. IPD Sharing: NO. Countries: 1. Publications: 0.
Eardream Data Collection in Switzerland Supported by ADDF
ClinicalTrials.gov study NCT05320471. IPD Sharing: UNDECIDED. Countries: 1. Publications: 0.
Awareness, Care & Treatment In Obesity Management - An Observation in Switzerland
ClinicalTrials.gov study NCT05232786. IPD Sharing: YES. Countries: 1. Publications: 0.
Epidemiology, Identification Rate and Treatment Penetration of Osteoporotic Vertebral Fractures in Switzerland
ClinicalTrials.gov study NCT02234414. IPD Sharing: Not stated. Countries: 1. Publications: 0.
A Study to Assess Change in Disease State in Adult Participants With Acute Myeloid Leukemia (AML) Ineligible for Intensive Chemotherapy in Switzerland and Austria Receiving Oral Venetoclax Tablets
ClinicalTrials.gov study NCT05215639. IPD Sharing: UNDECIDED. Countries: 2. Publications: 0.
CKD-aP Among Adults on Dialysis in Switzerland
ClinicalTrials.gov study NCT05415969. IPD Sharing: UNDECIDED. Countries: 1. Publications: 0.
Complications in Minimally Invasive Aesthetic Dermatological Procedures in Switzerland
ClinicalTrials.gov study NCT06864871. IPD Sharing: Not stated. Countries: 1. Publications: 0.
Cultural Adaptation of Hap-pas-Hapi (Step-by-Step) for Albanian-speaking Immigrants in Switzerland and Germany
ClinicalTrials.gov study NCT04230135. IPD Sharing: Not stated. Countries: 2. Publications: 0.
A Research Study About Weight Loss and Treatment Patterns With the Use of Saxenda® in Adults in Real-life Settings in Switzerland
ClinicalTrials.gov study NCT05153590. IPD Sharing: YES. Countries: 1. Publications: 0.
Feasibility and Acceptability of PRISMA for Prisoners in Switzerland
ClinicalTrials.gov study NCT06404502. IPD Sharing: UNDECIDED. Countries: 1. Publications: 0.
Seroprevalence of Leptospirosis in Val Müstair, Switzerland
ClinicalTrials.gov study NCT05300425. IPD Sharing: Not stated. Countries: 1. Publications: 0.
Registry for Mitral Valve Surgery at Department of Cardiac Surgery University Hospital of Basel/ Switzerland
ClinicalTrials.gov study NCT03587688. IPD Sharing: Not stated. Countries: 1. Publications: 0.
App-based Psychosocial Intervention to Enhance Quality of Life in Arabic-speaking Refugees Residing in Switzerland
ClinicalTrials.gov study NCT05651737. IPD Sharing: NO. Countries: 1. Publications: 0.
Assisted Suicide in Switzerland
ClinicalTrials.gov study NCT04261088. IPD Sharing: Not stated. Countries: 1. Publications: 0.
Clinnova-MS: A Prospective Cohort Study of Patients With Multiple Sclerosis (Switzerland)
ClinicalTrials.gov study NCT06526364. IPD Sharing: Not stated. Countries: 1. Publications: 0.
Rock glaciers Gruben, Muragl and Murtel, Switzerland: Area-wide flow fields, Version 1
Besides their thermal and mechanical properties, rock glaciers are essentially defined by their kinematics. Knowledge of the permafrost flow field provides important information about the origin, morphology, development, dynamics and internal structure of creeping mountain permafrost. Monitoring permafrost behavior helps detecting climate signals. Aerial photogrammetry was used for determining digital terrain models (DTM) with high resolution.
Rock glaciers, Bernese Alps, western Switzerland, Version 1
This inventory has been established from the results of the interpretation of aerial photographs and field work between 1992 and 1994.The area investigated covers the entire Bernese Alps (western Switzerland), about 4200 km2, and is situated between 46 deg 10' and 46 deg 50' N and 7 deg 10' and 8 deg 30' E. The Bernese Alps are one of the main European watersheds, separating the catchment area of the Aare (draining into the North Sea via the Rhine) from that of the Rhone (which flows into the Mediterranean Sea). The lowest points of the study area are situated in the valley floors of the two rivers at about 500 m asl, whereas several summits exceed 4000 m asl (highest point-- Finsteraarhorn, 4273 m asl). The main structure of the Bernese Alps is the crystalline Aar massif striking WSW-ENE and culminating in the western part of the study area. To the north and the west, the massif is covered by thrust nappes consisting of sedimentary rocks mainly of Mesozoic and early Tertiary age (chiefly marine limestones, shales, and sandstones). Their summits are considerably lower (mostly between 2000 and 3500 m asl).According to their geographic situation between 46 deg and 47 deg N, the climate of the Bernese Alps is of temperate character typical for the zone of the westerlies. Because of the their horizontal and vertical extension, the Alps themselves have considerable influence on the climate. Based on climatic criteria, two main realms can be distinguished: the moist and quite oceanic part in the north of the main watershed and the slightly more continental part sloping south to the Rhone. The northern part, exposed to the westerlies, shows maximum precipitation during summer, with quite low variability, whereas the south is somewhat dryer, showing no distinct maximum but higher variability. Accordingly, mean cloudiness is higher in the north. This results in an increase in the height of the mean glacier elevation from about 2500 m asl in the northern part of the Bernese Alps to 2900 m asl in the south. Because of the high precipitation (locally exceeding 4000 mm per year) and their external situation, the Bernese Alps show a lower equilibrium line of the glaciers and are the mountain group showing the heaviest glacierization of the Alps, which leaves little space for periglacial phenomena (both the glacier showing the lowermost front and the largest glacier of the Alps are situated within the study site). However, this does not mean that permafrost is rare in the Bernese Alps; above 3300 m asl, permafrost can be considered as continuous. In fact, the bedrock of many of the higher mountains in the Bernese Alps is perennially frozen. The number of rock glaciers found in the Bernese Alps is relatively small compared with other Alpine regions. Furthermore, the objects are quite small. This can be explained with the stronger glacierization. Modelling shows that permafrost ground amounts to roughly half as much as the glacierized area (subglacial permafrost not included). (Imhof, 1996) These data are presented on the CAPS Version 1.0 CD-ROM, June 1998.
Rock glaciers, Entremont, Valais, Switzerland, Version 1
The Entremont area is 300 square km wide and located in the western part of the Swiss Alps between the Mont-Blanc Massif and the Valaisian Alps, slightly north of the main crest of the alpine range. Altitude varies between 4313 m above see level (asl) at the top of the Grand-Combin and 714 m asl for the outlet of the valleys system. The geological composition is essentially dominated by metamorphic rocks (gneiss, shale, quartzite), however some sedimentary layers (limestone, dolomite) are inserted. The mean annual air temperature is about 0 C at 2300 m asl and annual precipitation among ranges between 1000 and 1500 mm at 2000 m asl with a maximum value of about 2000 mm on the alpine crest (Grand-St-Bernard pass). Equilibrium line of glaciers is over 3000 m asl in the north-facing slopes, the timberline is at about 2100 m asl and permafrost creeping features exist between 2000 and 3000 m asl, what results in a great variety of mountain and morphological landscapes.Aerial photographs analyses and field morphological observations have been performed during summer 1995 in order to inventory and map (1 to 25000) 321 well-developed to embryonic rock glaciers and protalus lobes (coexisting features have been separated) of total area 10.4 square. km. Rock glacier activity classification results from interpretation of both geomorphological and environmental signs. Some geophysics (BTS measurements and DC resistivity soundings) have been performed between 1995 and 1997 on a few rock glaciers in order to confirm the initial interpretation. Data described in this file on the CAPS Version 1.0 CD-ROM, June 1998, are--1. Location (X, Y)-- Swiss coordinates near the center of the feature.2. Front elevation (Z)-- Elevation (m a.s.l.) at the foot of the front (accuracy: 10 m).3. Length-- Maximal distance (m) between front and roots (accuracy: 10 - 20%).4. Width-- Mean width (m) of the feature (accuracy: 10%). 5. Orientation-- Global exposition of the rock glacier.6. Activity-- Interpretation by field indicators observation, only in a few cases by geophysics.7. Surface (ha)-- Calculated by 1 to 25,000 numerical mapping (accuracy: 5 - 10%).8. Origin-- Talus or moraine (debris) derived rock glacier ?Other information such as lithology, spring temperature, vegetation cover, inclination, roots elevation are partly available, but not described in the present data set.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
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DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.