Kinematic Constraints on Glacier Contributions to 21st-Century Sea-Level Rise
By M. Santiago, M. Montaño, Robert L. Benitez, Ronald J. Messer, W. Yonemoto, W. Greene. Science, 2008
943 citations recorded by the source corpus.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/3ec8e09bc92b064510481d12d5740cd8c43f26c4
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
- Svetlana Jevrejeva
- Aslak Grinsted
- John C. Moore
- Stefan Rahmstorf
- Stéphane Hallegatte
- A. Köhl
- L. Vermeersen
- Jiacan Yuan
In Oceanography
- Svetlana Jevrejeva
- John C. Moore
- Aslak Grinsted
- Stefan Rahmstorf
- A. Köhl
- L. Vermeersen
- A. Slangen
- C. Katsman
Citations in the corpus
- Tipping elements and climate–economic shocks: Pathways toward integrated assessment (2016, background): “The rate of ice sheet mass loss is, however, limited by the flux at the ice sheet margins [e.g., Pfeffer et al., 2008], leading to a disconnect between committed and realized change that could persist for millennia, particularly for levels of warming near the threshold [Applegate et al., 2015].”
- Projecting twenty-first century regional sea-level changes (2014, result): “These values are in line with estimates of Pfeffer et al. (2008), which are based on changes in discharge in potentially vulnerable areas.”
- Disaster on the horizon: The price effect of sea level rise (2019, background): “This provides one example of how optimistic investors can drive real estate prices as in Piazzesi and Schneider (2009). Finally, we contribute to the literature exploring the potential costs of climate change and value of current interventions.”
- Social and economic vulnerability of coastal communities to sea-level rise and extreme flooding (2014, background): “4.1 Identifying relevant hazard zones Sea-level rise projections for the twenty-first century vary in the range of 0.2–2 m (Rahmstorf 2007; Pfeffer et al. 2008; Grinsted et al. 2010; IPCC 2013), but fail to provide an accurate rate (Willis and Church 2012).”
- How will sea level respond to changes in natural and anthropogenic forcings by 2100? (2010, background): “Lately these IPCC numbers have been challenged with new estimates of 0.5–1.4 m [Rahmstorf, 2007], 0.75–1.90 m [Vermeer and Rahmstorf, 2010], 0.8– 2.0 m [Pfeffer et al., 2008] and 0.8–1.3 m [Grinsted et al., 2010] sea level rise by 2100.”
- Global sea level linked to global temperature (2009, background): “(25) provided an independent estimate of maximum ice discharge based on geographic constraints on ice flow; they concluded that sea-level rise in the 21st century is very unlikely to exceed 200 cm.”
- Assessing climate change impacts, sea level rise and storm surge risk in port cities: a case study on Copenhagen (2008, background): “Considering the large uncertainty on future sea level rise (e.g., IPCC 2007; Rahmstorf 2007; Pfeffer et al. 2008), this analysis is not based on a single sea level rise scenario.”
- Implications of climate change for agricultural productivity in the early twenty-first century (2010, background): “…the possible rate of discharge of these ice sheets, and past maximal sea-level rise (under similar climatic conditions) a maximum eustatic sea-level rise of approximately 2 m by 2100 is considered physically plausible, but very unlikely (Pfeffer et al. 2008; Rohling et al. 2008; Lowe et al. 2009).”