Abstract
Recent studies suggest that anthropogenic modification of land hydrology (e.g. through groundwater mining, dam building, irrigation, deforestation, wetlands drainage, and urbanization) could significantly impact sea-level rise, although the magnitude and sign of this effect have been widely debated. This paper attempts a comprehensive overview of the effects of human activities on land hydrology. Estimates are provided for the volumes of water associated with each of the major anthropogenic processes and the corresponding equivalent in sea level. Groundwater mining; and runoff from paved and built-up areas are two major sources of water added to the ocean. In contrast, storage of water behind dams, losses through percolation, and evapotranspiration from irrigated fields withhold water that would otherwise flow to the sea. The net effect of these processes holds back the equivalent of 0.8 +- 0.4 mm/yr from sea-level rise. This is a magnitude comparable to, but in the opposite direction from the currently observed sea-level rise of 1–2 mm/yr. These estimates are still preliminary, awaiting better documentation. Coupling of improved land hydrology models with GCMs will help in analysis of feedbacks, especially the partitioning of water among runoff, infiltration, and evaporation.
Keywords
Affiliated Institutions
Related Publications
Planetary Boundaries: Exploring the Safe Operating Space for Humanity
"Anthropogenic pressures on the Earth System have reached a scale where abrupt global environmental change can no longer be excluded. We propose a new approach to global sustain...
ERA5-Land: a state-of-the-art global reanalysis dataset for land applications
Abstract. Framed within the Copernicus Climate Change Service (C3S) of the European Commission, the European Centre for Medium-Range Weather Forecasts (ECMWF) is producing an en...
GEOCARB II; a revised model of atmospheric CO 2 over Phanerozoic time
Revision of the GEOCARB model (Berner, 1991, 1994) for paleolevels of atmospheric CO2, has been made with emphasis on factors affecting CO2 uptake by continental weathering. Thi...
Extension of New Zealand kauri (<i>Agathis australis</i>) tree‐ring chronologies into Oxygen Isotope Stage (OIS) 3
Abstract New Zealand kauri ( Agathis australis ) is both long‐lived and sensitive to climate so during the past two decades an extensive network of sites has been sampled for de...
Comparison of <sup>14</sup>C and U-Th Ages in Corals from IODP #310 Cores Offshore Tahiti
Shallow-water tropical corals can be used to calibrate the radiocarbon timescale. In this paper, we present a new data set based on the comparison between 14 C ages and U-Th age...
Publication Info
- Year
- 1997
- Type
- article
- Volume
- 14
- Issue
- 3-4
- Pages
- 147-161
- Citations
- 69
- Access
- Closed
External Links
Social Impact
Social media, news, blog, policy document mentions
Citation Metrics
Cite This
Identifiers
- DOI
- 10.1016/s0921-8181(96)00008-2