Groundwater deeper than 500 m contributes less than 0.1% of global river discharge
At depths of over 500 m, deep groundwater has long residence times and likely contributes less than 0.1% to global streamflow and only sporadically connects with the surface terrestrial water cycle on geological timescales, according to estimates derived from the chloride mass balance approach.
Main Authors: | Grant Ferguson, Jennifer C. McIntosh, Scott Jasechko, Ji-Hyun Kim, James S. Famiglietti, Jeffrey J. McDonnell |
---|---|
Format: | Article |
Language: | English |
Published: |
Nature Portfolio
2023-02-01
|
Series: | Communications Earth & Environment |
Online Access: | https://doi.org/10.1038/s43247-023-00697-6 |
Similar Items
-
Competition for shrinking window of low salinity groundwater
by: Grant Ferguson, et al.
Published: (2018-01-01) -
Deeper than the dead /
by: 219708 Hoag, Tami
Published: (c200) -
Modern groundwater reaches deeper depths in heavily pumped aquifer systems
by: Melissa Thaw, et al.
Published: (2022-09-01) -
Deeper waters are changing less consistently than surface waters in a global analysis of 102 lakes
by: Rachel M. Pilla, et al.
Published: (2020-11-01) -
Variables which influence the neurodevelopment at 2 years of newborns born less than 32 weeks of gestational age or less than 1,500 g
by: Eugénia Matos, et al.
Published: (2019-04-01)