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Household water use is generally calculated from the estimated or measured total public water supply and can either include or exclude leakage losses in the distribution system
Source-oriented approaches
The rate of change of the 'meteorological water balance', expressed in m3 ha-1 y-1 The map provides an estimate of the increase (red in the map) or decrease (blue in the map) of the volume of water required from irrigation in order to ensure that crop growth is not limited by water stress.
Left: relative difference in water available for runoff
Number of river monitoring stations included in analysis noted in brackets
In order to have a visually uninterrupted hydrographic network WISE Large rivers and large lakes should be used in combination with Transitional waters that resides along with the River basin district data.
Left: example of a forecast of topsoil moisture (15 July, 2008), right: subsoil available water capacity derived from modelling data.
Number of river monitoring stations included in analysis noted in brackets
This poster shows the dataset European River Catchments (ERC) and the water lines of EuroGlobalMap
The water level is measured relative to the present day tide, due to changes in atmospheric storminess, an increase in mean sea level and vertical land movements
Gross value added at market prices, constant 1990 prices; excluding Ireland; 1990 data for Germany do not include the former GDR
DE and NL have designated their whole territory as a sensitive area, but are not in conformity with the goal of 75% reduction of N
Projected river flow 2071-2100 (green line) and the observed river flow 1961-1990 (orange line)
For references, please go to https://www.eea.europa.eu/data-and-maps/find/global or scan the QR code.
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