Extensive dynamic thinning on the margins of the Greenland and Antarctic ice sheets
By H. Pritchard, R. Arthern, D. Vaughan, Laura A. Edwards. Nature, 2009
1,003 citations recorded by the source corpus.
Subfields: Atmospheric Science, Pulmonary and Respiratory Medicine
View Paper: https://www.semanticscholar.org/paper/023aca60a32eb0b968d30edc229dbfeeacdd49e4
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- P. Whitehouse
- Isabella Velicogna
- John M. Wahr
- Ernst J. O. Schrama
- Srinivas V. Bettadpur
- Eric J. M. Rignot
- Jeremie Mouginot
- Erik Ivins
In Pulmonary and Respiratory Medicine
- Isabella Velicogna
- Jeremie Mouginot
- Eric J. M. Rignot
- Bernd Scheuchl
- T. Bartels-Rausch
- Antony J. Payne
- P. Whitehouse
- David D. Pollard
Citations in the corpus
- Dynamically and Kinematically Consistent Global Ocean Circulation and Ice State Estimates (2013, background): “…in Greenland and ice streams feeding vast ice shelves in Antarctica (e.g., Payne et al., 2004; Alley et al., 2005; Shepherd and Wingham, 2007; Pritchard et al., 2009; Rignot et al., 2011; Straneo et al., 2013) has led to inferences that much of the ice responsemay be due to regional oceanic…”
- Regional acceleration in ice mass loss from Greenland and Antarctica using GRACE time‐variable gravity data (2014, methodology): “In Antarctica, we distinguish five regions identified based on changes highlighted in prior studies [Rignot et al., 2008; Chen et al., 2009; Pritchard et al., 2009; Shepherd et al., 2012]: (1) the Amundsen Sea (AS) sector of West Antarctica, (2) the Antarctic Peninsula, (3) Queen Maud Land, (4) the…”
- A Reconciled Estimate of Ice-Sheet Mass Balance (2012, methodology): “75 times the interquartile range from the median over a radius of 25 km from each point and produced a smoothed, 5 km grid of the mean (77).”
- The ICESat-2 Laser Altimetry Mission (2010, background): “Basin-scale fields of ice thickness are therefore essential for improvements in our estimates of the seasonal and interannual variability in regional mass balance, the freshwater budget of the polar oceans, and the representation of these processes in regional and climate models.”
- Time‐variable gravity observations of ice sheet mass balance: Precision and limitations of the GRACE satellite data (2013, result): “This is consistent with recent analyses of ice volume changes from laser [Pritchard et al., 2009] and radar [Flament and Remy, 2012] altimetry, which reveal ice thinning along the glacier troughs, and mass budget calculations [Rignot et al., 2011].”
- Ice structures, patterns, and processes: A view across the icefields (2012, background): “Because of their tremendous mass, they react very slowly to environmental changes, with dynamic response times of up to 100 000 years for the West Antarctic ice sheet, but at the same time have a great potential to affect sea level (Vaughan, 2007).”