Revisiting the Earth's sea‐level and energy budgets from 1961 to 2008

@article{White2011RevisitingTE,
  title={Revisiting the Earth's sea‐level and energy budgets from 1961 to 2008},
  author={Neil White and L. F. Konikow and Catia M. Domingues and J. Graham Cogley and E. Rignot and Jonathan M. Gregory and Michiel van den Broeke and Andrew J. Monaghan and Isabella Velicogna},
  journal={Geophysical Research Letters},
  year={2011},
  volume={38}
}
We review the sea‐level and energy budgets together from 1961, using recent and updated estimates of all terms. From 1972 to 2008, the observed sea‐level rise (1.8 ± 0.2 mm yr−1 from tide gauges alone and 2.1 ± 0.2 mm yr−1 from a combination of tide gauges and altimeter observations) agrees well with the sum of contributions (1.8 ± 0.4 mm yr−1) in magnitude and with both having similar increases in the rate of rise during the period. The largest contributions come from ocean thermal expansion… 

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References

SHOWING 1-10 OF 74 REFERENCES

Sea-Level Rise from the Late 19th to the Early 21st Century

We estimate the rise in global average sea level from satellite altimeter data for 1993–2009 and from coastal and island sea-level measurements from 1880 to 2009. For 1993–2009 and after correcting

Sea-Level Rise from the Late 19 th to the Early 21 st Century

We estimate the rise in global average sea level from satellite altimeter data for 1993-2009 and from coastal and island sea-level measurements from 1880 to 2009. For 1993-2009 and after correcting

Overview and Assessment of Antarctic Ice-Sheet Mass Balance Estimates: 1992–2009

Mass balance estimates for the Antarctic Ice Sheet (AIS) in the 2007 report by the Intergovernmental Panel on Climate Change and in more recent reports lie between approximately +50 to −250 Gt/year

Contemporary sea level rise.

TLDR
The most recent progress made in quantifying the processes causing sea level change on timescales ranging from years to decades, i.e., thermal expansion of the oceans, land ice mass loss, and land water-storage change are discussed.

Closing the sea level rise budget with altimetry, Argo, and GRACE

An analysis of the steric and ocean mass components of sea level shows that the sea level rise budget for the period January 2004 to December 2007 can be closed. Using corrected and verified Jason‐1

Thermosteric sea level rise, 1955–2003

For the 1955–2003 period, the thermal expansion of the 0–700 m layer of the World Ocean contributed approximately 0.33 mm/year to global sea level rise. About half of this thermosteric trend is due

Observations: Oceanic Climate Change and Sea Level

The oceans are warming. Over the period 1961 to 2003, global ocean temperature has risen by 0.10°C from the surface to a depth of 700 m. Consistent with the Third Assessment Report (TAR), global

The historical global sea-level budget

Abstract We analyze the global sea-level budget since 1850. Good estimates of sea-level contributions from glaciers and small ice caps, the Greenland ice sheet and thermosteric sea level are

Contribution of global groundwater depletion since 1900 to sea‐level rise

Removal of water from terrestrial subsurface storage is a natural consequence of groundwater withdrawals, but global depletion is not well characterized. Cumulative groundwater depletion represents a

Increasing rates of ice mass loss from the Greenland and Antarctic ice sheets revealed by GRACE

We use monthly measurements of time‐variable gravity from the GRACE (Gravity Recovery and Climate Experiment) satellite gravity mission to determine the ice mass‐loss for the Greenland and Antarctic
...