Dein Suchergebnis zum Thema: Model

Projecting Sea-​Level Rise: from Ice Sheets to Local Implications (PROTECT)

https://www.wsl.ch/de/projekte/projecting-sea-level-rise-from-ice-sheets-to-local-implications-protect/

The overarching scientific objective of PROTECT is to assess and project changes in the land-​based cryosphere with quantified uncertainties, to produce robust global, regional and local projections of SLR on a wide range of timescales.
The focus is on further model development, e.g. regarding ice-​flow dynamics and

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INSIghtForest: IN SItu tracking of water fluxes in Forest ecosystems through novel high-resolution monitoring of stable water isotopes

https://www.wsl.ch/de/projekte/insightforest-in-situ-tracking-of-water-fluxes-in-forest-ecosystems/

INSIghtForest will accompany the Cost Action WATSON „WATer isotopeS in the critical zONeproposes“ by establishing a unique data set of high frequency in-situ measured water isotopes located in a long-term irrigation experiment Pfynwald in the naturally dry valley of Valais, Switzerland.
assimilation approach using a newly Soil-Vegetation-Atmosphere Transfer (SVAT) model

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Dynamics of upstream-downstream drought characteristics in mountainous regions in current and future climates

https://www.wsl.ch/de/projekte/dynamics-of-upstream-downstream-drought-characteristics-in-mountainous-regions-in-current-and-future-climates-upxdown/

This project (upXdown) aims to enhance our understanding of the probability of spatio-temporally compounding winter droughts in upstream catchments followed by consecutive summer droughts in downstream catchments in the European Alps under continued global warming.
Daher werden in diesem Projekt mehrere SMILEs (Single Model Initial Conditioned Large

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AVAL-1D

https://www.wsl.ch/de/services-produkte/aval-1d/

Lawinengefahrenkarten werden von Ingenieuren und Raumplanern entwickelt. Die praktische Erfahrungen und Computer-Modelle nutzen, um die Auslaufdistanzen und Fliessgeschwindigkeiten von Lawinen zu berechnen.
Geschwindigkeit und Druck entlang der gesamten Lawinenbahn (analytisches Voellmy-Salm Model

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