54 parallel-processing-bioinformatics-"DIFFER" Fellowship positions at University of Oslo
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way. At our research environment, we seek to understanding the origins and processes governing stability and discontinuity of biological and geological systems at different levels of organization from
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the knowledge base for decision making through six key activities: assimilating rich Norwegian datasets into process-based models novel modelling of forest disturbances more robust modelling of soil accumulation
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understand the process that may later lead to societal benefits. We will analyse data from annual reports, project descriptions, and interviews to explore how different approaches to funding, collaboration
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obtaining and using data, how should individuals’ interests be balanced against this? How do concepts such as privacy, autonomy and bias apply in different AI contexts? Whose knowledge, and whose values feed
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and South-Eastern Norway Regional Health Authority are partners of ORGIMP. In collaboration with the partners, the project seeks to explore their portfolios to better understand the process that may
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well as the mantle’s viscous response to the unloading of deglaciated ice. As a result, spatial differences in ice texture can locally enhance or slow down ice flow, leading to some areas with faster than average ice
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professors, post-docs, researchers, technical, and administrative personnel, the Department has a total staff of 260 from more than 30 different countries. The Department aims to maintain high international
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across Europe. The aim of NorSink is to improve the knowledge base for decision making through six key activities: assimilating rich Norwegian datasets into process-based models novel modelling of forest
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administrative personnel, the Department has a total staff of 260 from more than 30 different countries. The Department aims to maintain high international standards within both research and teaching. The new
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flow of ice from ice divides to the sea, as well as the mantle’s viscous response to the unloading of deglaciated ice. As a result, spatial differences in ice texture can locally enhance or slow down ice