[PDF] Top 20 Time-evolving mass loss of the Greenland Ice Sheet from satellite altimetry
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Time-evolving mass loss of the Greenland Ice Sheet from satellite altimetry
... data from two spaceborne al- timeters: (i) the RA-1 (Radar Altimeter) on ERS-2 and (ii) the Geoscience Laser Altimeter System (GLAS) on ICESat (Ice, Cloud, and land Elevation ...data from ERS-2 have ... See full document
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Satellite Remote Sensing of the Greenland Ice Sheet Ablation Zone: A Review
... surface. Satellite remote sensing data show an ablation zone expanded in size, its albedo and surface elevation lower in response to enhanced melting, and an ice sheet transition from steady ... See full document
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Compensating Changes in the Penetration Depth of Pulse Limited Radar Altimetry Over the Greenland Ice Sheet
... the Greenland ice sheet experienced surface melting as increased transport of warm air from the south created anomalously high temperatures [16], ...the satellite era ...the ice ... See full document
10
An ice sheet model validation framework for the Greenland ice sheet
... new ice sheet model validation framework – the Cryospheric Model Comparison Tool (CmCt) – that aims to fill this ...specified time frame, process and filter available spatially and temporally ... See full document
16
Spatially extensive estimates of annual accumulation in the dry snow zone of the Greenland Ice Sheet determined from radar altimetry
... of ice sheet elevation change, the methodology we present should prove particu- larly useful for improving the accuracy of mass balance es- timates of the ...returns from the mis- sion ... See full document
8
Towards a re-assessment of the surface mass balance of the Greenland ice sheet
... The Greenland ice sheet (GrIS) is the largest freshwater source in the Northern Hemisphere ...future mass balance of the GrIS [2, 3] and its contribution to sea level change [4, ...loosing ... See full document
6
Feasibility of GNSS-R Ice Sheet Altimetry in Greenland Using TDS-1
... these ice sheets were to ever melt [1,2]. Even under a partial loss of these enormous ice masses, coastal areas would suffer significant ...that mass loss from the ... See full document
16
Seasonal to decadal variability in ice discharge from the Greenland Ice Sheet
... D from daily 1 km 2 resolution SMB estimates obtained from ...fluxes from the ice-free tundra and peripheral ice caps, which are included in the GRACE signal, into the ice ... See full document
13
Reconstruction of the 1979–2006 Greenland ice sheet surface mass balance using the regional climate model MAR
... discharge from outlet glaciers (Rignot et ...the ice sheet in the Green- land interior (Krabill et ...whole ice sheet is losing mass (Velicogna and Wahr, 2005; Chen et ...annual ... See full document
20
Estimation of the Greenland ice sheet surface mass balance for the 20th and 21st centuries
... Results from a regional climate simulation (1970– 2006) over the Greenland ice sheet (GrIS) reveals that more than 97% of the interannual variability of the modelled Sur- face Mass ... See full document
13
On the importance of the albedo parameterization for the mass balance of the Greenland ice sheet in EC-Earth
... snow, ice mass loss by sublimation, surface melt and subsequent run- ...and time over the ice ...the ice-sheet SEB, and thus on the ...over ice sheets re- mains ... See full document
17
Coupled regional climate–ice-sheet simulation shows limited Greenland ice loss during the Eemian
... face mass balance (SMB), being the sum of snowfall, subli- mation and meltwater run-off ...derived from ice core ...fields from climate models can be used, such as what has been done ...with ... See full document
16
Greenland Ice Sheet seasonal and spatial mass variability from model simulations and GRACE (2003–2012)
... GRACE-LM mass change estimates are pro- vided for ∼ 100 × 100 km 2 mascon regions, on what is essen- tially an equal area grid (shown in ...derived from k-band range and range rate (KBRR) data for two ... See full document
19
Inferred basal friction and surface mass balance of the Northeast Greenland Ice Stream using data assimilation of ICESat (Ice Cloud and land Elevation Satellite) surface altimetry and ISSM (Ice Sheet (System Model)
... on time-dependent adjoint modeling (Heimbach, 2008; Gold- berg and Heimbach, 2013), which show great promise in potentially enabling sophisticated data assimilation of dis- parate data sets into ... See full document
17
An integrated view of Greenland Ice Sheet mass changes based on models and satellite observations
... a) Mass change time series for the entire GrIS generated by DTU (red) and TUDR ...b) Ice mass trends for 2007-2011 provided by DTU (left) and TUDR ...solutions from the ITSG-Grace2016 ... See full document
22
Improved GRACE regional mass balance estimates of the Greenland ice sheet cross-validated with the input–output method
... The satellite gravity observations from GRACE (Gravity Recovery and Climate Experiment) provide snapshots of the global gravity field at monthly time intervals, which can be converted to mass ... See full document
18
The effect of overshooting 1.5 °C global warming on the mass loss of the Greenland ice sheet
... the ice sheet still lack details compared to an ...forcing from a GCM implies different characteristics, like smoother gradients and a less-resolved geometry, compared to the ...SMB from SEMIC ... See full document
21
Greenland Ice Sheet solid ice discharge from 1986 through 2017
... fast-flowing ice (orange, greater than 100 m yr −1 ) and the gates for the top eight discharging glaciers ...ferent from the main ...regions from Mouginot and Rignot (2019) are designated by thicker ... See full document
18
Arctic sea ice and ocean topography from satellite altimetry
... ple, from ice drillings in the Eurasian sector o f the A rctic O cean during A ugust and Septem ber 1991, Eicken et a l [1995] arrived at a value o f ...8.48. From sim ilar w ork carried out in the ... See full document
201
Hindcasting to measure ice sheet model sensitivity to initial states
... We have not used all available observations. Additional observations that can be used for validation are, for example, spatially distributed mass loss estimates from GRACE (e.g. Luthcke et al., 2013) ... See full document
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