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

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

3

Hydrology: Groundwater Hydrology, Oceanography: Physical: Sea Level: Variations And Mean (1222, 1225, 1641)

Scientific paper

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 transfer of mass from land to the oceans that contributes to sea-level rise. Depletion is directly calculated using calibrated groundwater models, analytical approaches, or volumetric budget analyses for multiple aquifer systems. Estimated global groundwater depletion during 1900-2008 totals ˜4,500 km3, equivalent to a sea-level rise of 12.6 mm (>6% of the total). Furthermore, the rate of groundwater depletion has increased markedly since about 1950, with maximum rates occurring during the most recent period (2000-2008), when it averaged ˜145 km3/yr (equivalent to 0.40 mm/yr of sea-level rise, or 13% of the reported rate of 3.1 mm/yr during this recent period).

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Contribution of global groundwater depletion since 1900 to sea-level rise does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Contribution of global groundwater depletion since 1900 to sea-level rise, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Contribution of global groundwater depletion since 1900 to sea-level rise will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1401579

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.