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Aerosol–climate interactions in the Norwegian Earth System Model – NorESM1-M
Aerosol–climate Norwegian Earth System Model NorESM1-M
2014/12/17
The objective of this study is to document and evaluate recent changes and updates to the module for aerosols and aerosol–cloud–radiation interactions in the atmospheric module CAM4-Oslo of the core v...
Evaluation of the carbon cycle components in the Norwegian Earth System Model (NorESM)
the carbon cycle components Norwegian Earth System Model
2014/12/16
The recently developed Norwegian Earth System Model (NorESM) is employed for simulations contributing to the CMIP5 (Coupled Model Intercomparison Project phase 5) experiments and the fifth assessment ...
The Norwegian Earth System Model, NorESM1-M – Part 2: Climate response and scenario projections
Norwegian Earth System Model NorESM1-M – Part 2 Climate response scenario projections
2014/12/16
NorESM is a generic name of the Norwegian earth system model. The first version is named NorESM1, and has been applied with medium spatial resolution to provide results for CMIP5 (http://cmip-pcmdi.ll...
The Norwegian Earth System Model, NorESM1-M – Part 1: Description and basic evaluation of the physical climate
Norwegian Earth System Model Description and basic evaluation the physical climate
2014/12/12
The core version of the Norwegian Climate Center's Earth System Model, named NorESM1-M, is presented. The NorESM family of models are based on the Community Climate System Model version 4 (CCSM4) of t...
The Late Riphean Porsangerhalvøyan tectonometamorphic event in the North Norwegian Caledonides:a comment on nomenclature
tectonometamorphic event North Norwegian Caledonides comment nomenclature
2009/12/3
A case is presented for replacing the name 'Porsanger' in 'Porsanger orogeny', in the Kalak Nappe Complex of the Finnmark Caledonides, by the adjectival 'Porsangerhalvøyan'.Moreover, until prov...
Mesozoic mudstone compositions and the role of kaolinite weathering–a view from shallow cores in the Norwegian Sea (Møre to Troms)
Mesozoic mudstone compositions kaolinite weathering shallow cores
2009/12/3
Mineralogical data from Mesozoic fine clastic sediments in shallow cores offshore Møre to Troms are compiled. The purpose is to examine stratigraphic and geographic variations in rock compositi...
Metamorphic conditions across the Seve-Köli Nappe boundary,southeastern Trondheim region,Norwegian Caledonides:Comparison of garnet-biotite thermometry and amphibole chemistry
Metamorphic conditions Seve-Kö li Nappe boundary garnet-biotite thermometry amphibole chemistry
2009/12/3
Rocks of the lower Seve Nappe and overlying Köli Nappes are exposed by a domal structure in the Einunnfjellet-Savalen area, southeastern Trondheim region, south-central Norway. In a traverse acro...
From rifting to drifting:effects on the development of deep-water hydrocarbon reservoirs in a passive margin setting,Norwegian Sea
deep-water hydrocarbon reservoirs passive margin setting Norwegian Sea
2009/12/3
The Cretaceous to Eocene deep-water hydrocarbon reservoirs in the Norwegian Sea were deposited during four main tectonic stages from continental rifting to oceanic drift: 1) Late Jurassic/Early Cretac...
Buried sedimentary mounds in the Nyk High area,Mid-Norwegian margin:Are they Miocene-Pliocene cold-water coral mounds?
Buried sedimentary mounds Nyk High area Miocene-Pliocene cold-water coral mounds
2009/12/3
Buried sedimentary mounds in the Nyk High area,Mid-Norwegian continental margin, are described from a 3D-seismic dataset and discussed in relation to modern deep-water sedimentary mounds. The mounds a...
Polycyclic aromatic hydrocarbons (PAHs) in Norwegian and Russian Arctic marine sediments:concentrations,geographical distribution and sources
Polycyclic aromatic hydrocarbons Norwegian Russian Arctic marine sediments
2009/12/3
Polycyclic aromatic hydrocarbons (PAHs) are key contaminants of concern under the Arctic Environmental Monitoring Programme (AMAP) due to their carcinogenic potential. The concentration of the differe...
Depositional facies and reservoir quality of deep-marine sandstones in the Norwegian Sea
Depositional facies reservoir quality deep-marine sandstones Norwegian Sea
2009/12/3
During the Late Cretaceous and Early Paleocene, deep-water depositional systems deposited sandstones in the Norwegian Sea. The reservoir quality is variable and difficult to predict because of variati...
Frequency and triggering mechanisms of submarine landslides of the North Norwegian continental margin
Frequency triggering mechanisms submarine landslides North Norwegian continental margin
2009/12/3
The frequency of submarine landslides was investigated through the occurrence of sandy turbidites in a 16 m long piston core and a shorter gravity core from the abyssal plain of the Lofoten Basin, Nor...
Automatic detection of circular depressions in digital elevation data in the search for potential Norwegian impact structures
Automatic detection circular depressions digital elevation data potential Norwegian impact structures
2009/12/2
Presently, 174 impact craters are proven on Earth, and of these 10 are located in Finland, 6 in Sweden and only 2 in Norway (Gardnos and Mjølnir).A pattern matching algorithm (correlation) base...
The Molo Formation,deposited by coastal progradation on the inner Mid-Norwegian continental shelf,coeval with the Kai Formation to the west and the Utsira Formation in the North Sea
Molo Formation coastal progradation inner Mid-Norwegian continental shelf Kai Formation
2009/12/2
The Molo Formation represents a characteristic depositional unit on the inner Mid-Norwegian continental shelf and extends along the coast for about 500 km from Møre to Lofoten. It was deposited...
Fluid flow structures and processes;indications from the North Norwegian continental margin
Fluid flow structures and processes indications North Norwegian continental margin
2009/12/2
On the basis of multibeam echo-sounder bathymetric data and high-resolution seismic records about 285 pockmarks and 25 dome structures are mapped in the outer parts of Andfjorden, northern Norway. The...