4.5 Article

The transient sensitivity of sea level rise

期刊

OCEAN SCIENCE
卷 17, 期 1, 页码 181-186

出版社

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/os-17-181-2021

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资金

  1. Villum experiment Old Noble grant [28024]
  2. Villum Investigator Project IceFlow [16572]
  3. European Union under the Horizon 2020, the EUCP project [776613]

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Recent assessments suggest that global mean sea level may not rise more than 1.1 meters within this century, but will continue to increase beyond 2100. Some studies indicate greater sea level rise is possible, with experts assigning a higher likelihood of such a future. Analyzing the relationship between sea level change rate and global mean surface temperature has led to the concept of transient sea level sensitivity.
Recent assessments from the Intergovernmental Panel on Climate Change (IPCC) imply that global mean sea level is unlikely to rise more than about 1.1 m within this century but will increase further beyond 2100. Even within the most intensive future anthropogenic greenhouse gas emission scenarios, higher levels are assessed to be unlikely. However, some studies conclude that considerably greater sea level rise could be realized, and a number of experts assign a substantially higher likelihood of such a future. To understand this discrepancy, it would be useful to have scenario-independent metrics that can be compared between different approaches. The concept of a transient climate sensitivity has proven to be useful to compare the global mean temperature response of climate models to specific radiative forcing scenarios. Here, we introduce a similar metric for sea level response. By analyzing the mean rate of change in sea level (not sea level itself), we identify a nearly linear relationship with global mean surface temperature (and therefore accumulated carbon dioxide emissions) both in model projections and in observations on a century scale. This motivates us to define the transient sea level sensitivity as the increase in the sea level rate associated with a given warming in units of meters per century per kelvin. We find that future projections estimated on climate model responses fall below extrapolation based on recent observational records. This comparison suggests that the likely upper level of sea level projections in recent IPCC reports would be too low.

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