Regional acceleration in ice mass loss from Greenland and Antarctica using GRACE time‐variable gravity data
By Isabella Velicogna, Tyler Clark Sutterley, M. V. D. Broeke. 2014
343 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/496290a6e2ba942d1f0a95efb2fc57b3a3a2008c
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
- Eric J. M. Rignot
- Jeremie Mouginot
- Isabella Velicogna
- Bernd Scheuchl
- F. Landerer
- David Wiese
- Tyler Clark Sutterley
- Mathieu Morlighem
In Oceanography
- David Wiese
- F. Landerer
- Tyler Clark Sutterley
- Eric J. M. Rignot
- Jeremie Mouginot
- Shuang Yi
- N. Sneeuw
- Isabella Velicogna
Citations in the corpus
- Continuity of Ice Sheet Mass Loss in Greenland and Antarctica From the GRACE and GRACE Follow‐On Missions (2020, methodology): “All harmonics are smoothed with a 250 km radius Gaussian smoothing function (Velicogna et al., 2014).”
- Forty-six years of Greenland Ice Sheet mass balance from 1972 to 2018 (2019, methodology): “With the Gravity Recovery and Climate Experiment (GRACE), the loss of 280 ± 58 Gt/y for 2003–2013, with an acceleration of 254 ± 12 Gt/y per decade (8), matches our 274 ± 17 Gt/y estimate, with an acceleration of 249 ± 54 Gt/y per decade.”
- Filling the Data Gaps Within GRACE Missions Using Singular Spectrum Analysis (2021, background): “As the number of observations grows, it is suggested that the long-term melting trends may be accelerating (Velicogna et al., 2014) or intermittent (Talpe et al.”