Use of Sentinel-1 radar observations to evaluate snowmelt dynamics in alpine regions

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Use of Sentinel-1 radar observations to evaluate snowmelt dynamics in alpine regions ; volume:14 ; number:3 ; year:2020 ; pages:935-956
The Cryosphere ; 14, Heft 3 (2020), 935-956

Creator: Marin, Carlo
Bertoldi, Giacomo
Premier, Valentina
Callegari, Mattia
Brida, Christian
Hürkamp, Kerstin
Tschiersch, Jochen
Zebisch, Marc
Notarnicola, Claudia

DOI: 10.5194/tc-14-935-2020

URN: urn:nbn:de:101:1-2020031904440460396462

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 14.08.2025, 10:54 AM CEST

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Associated

Marin, Carlo
Bertoldi, Giacomo
Premier, Valentina
Callegari, Mattia
Brida, Christian
Hürkamp, Kerstin
Tschiersch, Jochen
Zebisch, Marc
Notarnicola, Claudia

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Monitoring Large-Scale Inland Water Dynamics by Fusing Sentinel-1 SAR and Sentinel-3 Altimetry Data and by Analyzing Causal Effects of Snowmelt

Snowmelt Characterization from Optical and Synthetic Aperture Radar Observations in the Lajoie Basin, British Columbia

Using Radar Observations to Evaluate 3D Radar Echo Structure Simulated by a Global Model

Dual-frequency radar observations of snowmelt processes on Antarctic perennial sea ice by CFOSCAT and ASCAT

Flowering phenology in alpine grassland strongly responds to shifts in snowmelt but weakly to summer drought

Attribution of growing season evapotranspiration variability considering snowmelt and vegetation changes in the arid alpine basins

Alpine plant communities differ in their seed germination requirements along a snowmelt gradient in the Caucasus

Early snowmelt advances flowering phenology and disrupts the drivers of pollinator visitation in an alpine ecosystem

Increased spring freezing vulnerability for alpine shrubs under early snowmelt

Simulation of snowmelt - runoff in lowland and lower alpine regions of Switzerland

Simulation of the snowmelt runoff contributing area in a small alpine basin

Snowmelt runoff from northern alpine tundra hillslopes: major processes and methods of simulation

Monitoring Large-Scale Inland Water Dynamics by Fusing Sentinel-1 SAR and Sentinel-3 Altimetry Data and by Analyzing Causal Effects of Snowmelt

Snowmelt Characterization from Optical and Synthetic Aperture Radar Observations in the Lajoie Basin, British Columbia

Using Radar Observations to Evaluate 3D Radar Echo Structure Simulated by a Global Model

Dual-frequency radar observations of snowmelt processes on Antarctic perennial sea ice by CFOSCAT and ASCAT

Flowering phenology in alpine grassland strongly responds to shifts in snowmelt but weakly to summer drought

Attribution of growing season evapotranspiration variability considering snowmelt and vegetation changes in the arid alpine basins

Alpine plant communities differ in their seed germination requirements along a snowmelt gradient in the Caucasus

Early snowmelt advances flowering phenology and disrupts the drivers of pollinator visitation in an alpine ecosystem

Increased spring freezing vulnerability for alpine shrubs under early snowmelt

Simulation of snowmelt - runoff in lowland and lower alpine regions of Switzerland

Simulation of the snowmelt runoff contributing area in a small alpine basin

Snowmelt runoff from northern alpine tundra hillslopes: major processes and methods of simulation

Monitoring Large-Scale Inland Water Dynamics by Fusing Sentinel-1 SAR and Sentinel-3 Altimetry Data and by Analyzing Causal Effects of Snowmelt

Snowmelt Characterization from Optical and Synthetic Aperture Radar Observations in the Lajoie Basin, British Columbia

Using Radar Observations to Evaluate 3D Radar Echo Structure Simulated by a Global Model

Dual-frequency radar observations of snowmelt processes on Antarctic perennial sea ice by CFOSCAT and ASCAT

Flowering phenology in alpine grassland strongly responds to shifts in snowmelt but weakly to summer drought

Attribution of growing season evapotranspiration variability considering snowmelt and vegetation changes in the arid alpine basins

Alpine plant communities differ in their seed germination requirements along a snowmelt gradient in the Caucasus

Early snowmelt advances flowering phenology and disrupts the drivers of pollinator visitation in an alpine ecosystem

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Use of Sentinel-1 radar observations to evaluate snowmelt dynamics in alpine regions

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Other Objects (12)

Increased spring freezing vulnerability for alpine shrubs under early snowmelt

Simulation of snowmelt - runoff in lowland and lower alpine regions of Switzerland

Simulation of the snowmelt runoff contributing area in a small alpine basin

Snowmelt runoff from northern alpine tundra hillslopes: major processes and methods of simulation

Monitoring Large-Scale Inland Water Dynamics by Fusing Sentinel-1 SAR and Sentinel-3 Altimetry Data and by Analyzing Causal Effects of Snowmelt

Snowmelt Characterization from Optical and Synthetic Aperture Radar Observations in the Lajoie Basin, British Columbia

Using Radar Observations to Evaluate 3D Radar Echo Structure Simulated by a Global Model

Dual-frequency radar observations of snowmelt processes on Antarctic perennial sea ice by CFOSCAT and ASCAT

Flowering phenology in alpine grassland strongly responds to shifts in snowmelt but weakly to summer drought

Attribution of growing season evapotranspiration variability considering snowmelt and vegetation changes in the arid alpine basins

Alpine plant communities differ in their seed germination requirements along a snowmelt gradient in the Caucasus

Early snowmelt advances flowering phenology and disrupts the drivers of pollinator visitation in an alpine ecosystem

Increased spring freezing vulnerability for alpine shrubs under early snowmelt

Simulation of snowmelt - runoff in lowland and lower alpine regions of Switzerland

Simulation of the snowmelt runoff contributing area in a small alpine basin

Snowmelt runoff from northern alpine tundra hillslopes: major processes and methods of simulation

Monitoring Large-Scale Inland Water Dynamics by Fusing Sentinel-1 SAR and Sentinel-3 Altimetry Data and by Analyzing Causal Effects of Snowmelt

Snowmelt Characterization from Optical and Synthetic Aperture Radar Observations in the Lajoie Basin, British Columbia

Using Radar Observations to Evaluate 3D Radar Echo Structure Simulated by a Global Model

Dual-frequency radar observations of snowmelt processes on Antarctic perennial sea ice by CFOSCAT and ASCAT

Flowering phenology in alpine grassland strongly responds to shifts in snowmelt but weakly to summer drought

Attribution of growing season evapotranspiration variability considering snowmelt and vegetation changes in the arid alpine basins

Alpine plant communities differ in their seed germination requirements along a snowmelt gradient in the Caucasus

Early snowmelt advances flowering phenology and disrupts the drivers of pollinator visitation in an alpine ecosystem

Increased spring freezing vulnerability for alpine shrubs under early snowmelt

Simulation of snowmelt - runoff in lowland and lower alpine regions of Switzerland

Simulation of the snowmelt runoff contributing area in a small alpine basin

Snowmelt runoff from northern alpine tundra hillslopes: major processes and methods of simulation

Monitoring Large-Scale Inland Water Dynamics by Fusing Sentinel-1 SAR and Sentinel-3 Altimetry Data and by Analyzing Causal Effects of Snowmelt

Snowmelt Characterization from Optical and Synthetic Aperture Radar Observations in the Lajoie Basin, British Columbia

Using Radar Observations to Evaluate 3D Radar Echo Structure Simulated by a Global Model

Dual-frequency radar observations of snowmelt processes on Antarctic perennial sea ice by CFOSCAT and ASCAT

Flowering phenology in alpine grassland strongly responds to shifts in snowmelt but weakly to summer drought

Attribution of growing season evapotranspiration variability considering snowmelt and vegetation changes in the arid alpine basins

Alpine plant communities differ in their seed germination requirements along a snowmelt gradient in the Caucasus

Early snowmelt advances flowering phenology and disrupts the drivers of pollinator visitation in an alpine ecosystem

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