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Dating norway i hauknes

Parameter uncertainty analysis for an operational hydrological model using residual-based and limits of acceptability approaches. Hydrology and Earth System Sciences.

ISSN Geoscientific Dating norway i hauknes Development. ISSN X. Diagnosing the decline in climatic mass balance of glaciers in Svalbard over The Cryosphere.

The climatic mass balance of Svalbard glaciers: A year simulation with a coupled atmosphere-glacier mass balance model. Small-scale variation of snow in a regional permafrost model.

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Changes in winter warming events in the Nordic Arctic Region. Journal of Climate. Show summary In recent years extreme winter warming events have been reported in arctic areas. These events are characterized as extraordinarily warm weather episodes, occasionally combined with intense rainfall, causing ecological disturbance and challenges for arctic societies and infrastructure.

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Ground-ice formation due to winter rain or melting prevents ungulates from grazing, leads to vegetation browning, and impacts soil temperatures. The authors analyze changes in frequency and intensity of winter warming liknes singel in the Nordic arctic region—northern Norway, Sweden, and Finland, including the arctic islands Svalbard and JanMayen.

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This study identifies events in the longest available records of daily temperature and precipitation, as well as in future climate scenarios, and performs analyses of long-term trends for climate indices aimed to capture these individual events. Results show high frequencies of warm weather events during the s—30s and the past 15 years —14causing weak positive trends over the past 90 years — In contrast, strong positive trends in occurrence and intensity for all climate indices are found for the past 50 years with, for example, increased rates for number of melt days of up to 9.

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Regional projections for the twenty-first century indicate a significant enhancement of the frequency and intensity of winter warming events. For northern Scandinavia, the simulations indicate a doubling in the number of warming events, compared to —, while the projected frequencies for the arctic islands are up to 3 times higher. A comparison between simulated and observed surface energy balance at the Svalbard Archipelago.

Journal of Applied Meteorology and Climatology. Simulating the climatic mass balance of Svalbard glaciers from to with a high-resolution coupled atmosphere-glacier model.

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The Cryosphere Discussions. Mass-balance and runoff sensitivities of Norwegian glacier catchments to climate perturbations. Annals of Glaciology.

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CryoSat-2 delivers monthly and inter-annual surface elevation change for Arctic ice caps. A ground temperature map of the North Atlantic permafrost region based on remote sensing and reanalysis data. A statistical approach to represent small-scale variability of permafrost temperatures due to snow cover.

Contribution of snow and glacier melt to discharge for highly glacierised catchments in Norway. Meteorological conditions on an Arctic ice cap-8 years of automatic weather station data from Austfonna, Svalbard.

Academic Interests

International Journal of Climatology. Remote Sensing of Environment. Glacier mass balance of Norway — calculated by a temperature-index model. CryoGRID 1.

Permafrost and Periglacial Processes. Subglacial permafrost dynamics and erosion inside subglacial channels driven by surface events in Svalbard. Modelling the climatic mass balance of three glaciers in Norway along a continentality gradient, Sensing drifters as tool for glacial hydrology measurements.

Climate in Svalbard Norwegian Centre for Climate Services Reports.

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Full text in Research Dating norway i hauknes. Balancing between type I and type II errors in testing hydrological models as hypotheses of catchment behaviour. Ensemble-based uncertainty quantification and reduction in hydrological modelling and predictions.

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Application of machine learning emulators in parameter identification for a distributed hydrological model. Assimilation of MODIS fractional snow cover area into a hydrological model using fuzzy-logic based ensemble smoother data assimilation frameworks. Fuzzy-logic based ensemble smoother data assimilation frameworks for improving the informational value of the assimilated data. Snow data assimilation into a hydrological model using fuzzy logic based ensemble smoothers.

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Nå er isbreene fravristet noen av sine dypeste hemmeligheter. Towards high-resolution Bayesian snow reconstruction in permafrost regions. Stable and unstable glacier flows: Role of friction law and feedback mechanisms at the basal interface. The different dynamic personalities of two neighboring tidewater glaciers.

Parameter uncertainty analysis for a distributed hydrological model. A rate-and-state friction law for glaciers. Dating norway i hauknes subgrid snow data assimilation. The Evolution of a Snow Dune Field.

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The morphological evolution of a wind-shaped snow surface during a storm event at Finse, Norway. A network of instrumentation to keep track of snow distribution at Finse, Norway.

Multi-year surface velocities and sea-level rise contribution of the Basin-3 and Basin-2 surges, Austfonna, Svalbard. Parameterizing snow redistribution effect of topographic parameters in a conceptual hydrological model. A distributed and real-time wireless network of weather stations for wind-blown snow at Finse, Norway. Capturing snow depth distribution with a low cost and wireless weather station network. Weather stations for wind-blown snow at Finse, Norway: A distributed and real-time wireless network of.

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GlacierFlows: processes single lillehammer the glacier base and their significance for ice movement.

The surge must go on: extended surface velocity time series and frontal ablation estimates of Basin-3 and Basin-2NE-Svalbard.

Towards real-time snow products for Svalbard. Mapping the thermal state of permafrost through modeling and remote sensing. A surge of the Austfonna ice cap, Svalbard, promoted by a hydro-thermodynamic feedback to summer melt.

A probabilistic approach to represent small-scale variability of permafrost temperatures due to snow cover. Interaction of Svalbard glaciers and the ecosystem of the Barents Sea. Ground temperature mapping from space. Permafrost models and permafrost landscapes — is there a connection?. Large-scale monitoring of ground thermal conditions through data fusion of remote sensing products. Towards a spatial model of ground thermal regime for theSvalbard archipelago.

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Etzelmuller, Bernd; Christiansen, H. Observed and simulated surface energy budget at Ny-Ålesund, Svalbard. Observert og simulert bakke-energibalanse på Svalbard. On a major surge of Austfonna.

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Ground-based monitoring of snowcover, firn area and glacier facies of Austfonna, Svalbard, to validate and improve PolarWRF climate simulations. Relative age and Holocene distribution of permafrost in Norway. Considering orographic enhancement to downscale precipitation: resolving the accumulation asymmetry and deriving a 55 year accumulation history of Austfonna, Svalbard.

Published Dec.