When comparing the history of
hydrological changes in the region with artifacts from the Middle Stone Age, the researchers discovered a «striking correspondence between the archaeological record of South Africa and the timing of the abrupt climate change» as seen in the marine core, the study states.
Although the recent drought may have significant contributions from natural variability, it is notable that
hydrological changes in the region over the last 50 years can not be fully explained by natural variability, and instead show the signature of anthropogenic climate change.
Not exact matches
Taking factors such as sea surface temperature, greenhouse gases and natural aerosol particles into consideration, the researchers determined that
changes in the concentration of black carbon could be the primary driving force behind the observed alterations to the
hydrological cycle
in the
region.
That's a growing problem, because
in many places, finding water for energy isn't easy - and it's bound to get tougher as energy demands soar and climate
change alters
hydrological cycles
in already arid
regions.
In many regions, changing precipitation or melting snow and ice are altering hydrological systems, affecting water resources in terms of quantity and quality (medium confidence
In many
regions,
changing precipitation or melting snow and ice are altering
hydrological systems, affecting water resources
in terms of quantity and quality (medium confidence
in terms of quantity and quality (medium confidence).
Adaptation procedures and risk management practices for the water sector are being developed
in some countries and
regions that have recognised projected
hydrological changes with related uncertainties.
Adaptation procedures and risk management practices for the water sector are being developed
in some countries and
regions (e.g., Caribbean, Canada, Australia, Netherlands, UK, USA, Germany) that have recognised projected
hydrological changes with related uncertainties (very high confidence).
This study investigates a physical basis for heterogeneity
in hydrological changes, which suggests a greater detectability
in wet than dry
regions.
Although these
hydrological changes could potentially increase soil water availability
in previously snow - covered
regions during the cool low - ET season (34), this effect would likely be outweighed by the influence of warming temperatures (and decreased runoff) during the warm high - ET season (36, 38), as well as by the increasing occurrence of consecutive years with low precipitation and high temperature (Fig. 4A).
As noted
in the TAR (McAvaney et al., 2001), vegetation
change during the mid-Holocene likely triggered
changes in the
hydrological cycle, explaining the wet conditions that prevailed
in the Sahel
region that were further enhanced by ocean feedbacks (Ganopolski et al., 1998; Braconnot et al., 1999), although soil moisture may have counteracted some of these feedbacks (Levis et al., 2004).
PTI: Studies conducted by Geological Survey of India indicate some of the likely impacts of melting of glaciers on the
hydrological system
in form of
changes in the river hydrology, increased debris production and siltation of rivers
in downstream
region.