Freshwater glossary

WISE Freshwater glossary presents a curated collection of essential terms related to freshwater studies, aimed at supporting scholars and practitioners in the fields of hydrology, ecology, and environmental science. Emphasizing scientific accuracy and clarity, it serves as a concise reference, illuminating the complex dynamics of freshwater systems and their pivotal role in sustaining ecological balance and human life.

Afforestation

Afforestation is the process of planting trees, either to replace those removed during forest harvesting or as a means of land use conversion. Afforestation is part of several natural water retention measures as it can contribute to a more natural and sustainable hydrologic cycle.

Agricultural practice

Agronomic practices which have the primary purpose of improvements to agriculture can, in some cases, contribute to the functioning of natural water retention measures. As such, they integrate sustainable and natural water management into current practices.

Appropriate design of roads and stream crossings

Appropriately designed roads and stream crossings can minimize the likelihood of erosion and sediment production that can be associated with forestry activities including final harvest. Poorly designed or built roads and stream crossings can cause some of the most negative effects of forestry on the landscape. Well-designed roads follow the contours of the landscape. Roads which run up and down (instead of across) hills can act as channels which focus runoff and can lead to increased erosion. Properly designed stream crossings permit the free movement of fish and aquatic invertebrates and will not restrict peak flows. Ensuring that stream crossings do not restrict peak flows will help to reduce localized flooding and can ultimately be more cost effective as they will not need to be rebuilt following high flow events - Based on Stella definitions, adapted by NWRM project experts and validated by the European Commission

Artificial groundwater recharge (AGR)

AGR stores large quantities of water in underground aquifers to increase the quantity of groundwater in times of shortage.ᅠ It results in a lowering of run-off from surrounding land, and in an enhanced natural condition of aquifers and water availability.ᅠ The natural cleaning process of water percolating through the soils when entering the AGR improves water quality. Mechanisms used to undertake the recharge should be highlighted. In this respect one can envisage:(i) surface structures to facilitate/augment recharge (such as soakways and infiltration basins);(ii) subsurface indirect recharge - artificial recharge is undertaken through wells drilled within the unsaturated zone;(iii) subsurface direct recharge - artificial recharge is undertaken through wells reaching the saturated zone. The regulatory approach to be adopted for each of the above three mechanisms could differ considerably, due to the fact that the level of natural protection to groundwater is vastly different for each of the mechanisms

Bank

The sloping side of any hollow in the ground, especially when bordering a river.

Basins and ponds

Basins and ponds store surface run-off.ᅠ Detention basins are free from water in dry weather flow conditions but ponds (e.g., retention ponds, flood storage reservoirs, shallow impoundments) contain water in dry weather, and are designed to hold more when it rains. - Based on Stella definitions, adapted by NWRM project experts and validated by the European Commission

Biophysical environment

The biophysical environment is the biotic and abiotic surrounding of an organism or population, and consequently includes the factors that have an influence in their survival, development and evolution. The biophysical environment can vary in scale from microscopic to global in extent. It can also be subdivided according to its attributes. Examples include the marine environment, the atmospheric environment and the terrestrial environment. The number of biophysical environments is countless, given that each living organism has its own environment. The symbiosis between the physical environment and the biological life forms within the environment includes all variables that comprise the Earth’s biosphere. The biophysical environment can be divided into two categories: the natural environment and the built environment with some overlap between the two. Following the industrial revolution the built environment has become an increasingly significant part of the Earth's environment. The scope of the biophysical environment is all that contained in the biosphere, which is that part of the Earth in which all life occurs. When narrowed down to the aquatic environment, and particularly in the context of the Water Framework Directive, these are often referred to as water quality, water quantity and hydromorphology.

Biophysical parameter

A biophysical parameter is a measurable characteristic that can help in defining a particular system. It can cover individual substances, groups of substances or be defined by its measurement method like turbidity or the mesurement of oxygen consumption like BOD5 or COD. It is generally expressed by a value and its unit.

Channels and rills

'Hard-edged' conveyance channels to move water between components in a SuDS 'train'.ᅠ Typically narrower than swales, but may also include vegetated aspects. - Based on Stella definitions, adapted by NWRM project experts and validated by the European Commission

Coarse woody debris

Coarse woody debris is a key stream habitat feature used by fish and other organisms. Coarse woody debris can also help to lower flow velocity in streams. - Based on Stella definitions, adapted by NWRM project experts and validated by the European Commission

Continuous cover forestry

Continuous cover forestry (CCF) is a broad term encompassing a wide variety of forest management practices. One key feature of is that biomass removal is based either on small clearcuts or selective harvesting. Smaller clearcuts may create less hydrological disturbance but some of the filtration benefits associated with forest soils may be lost as a result of the greater driving and road maintenance needed for continuous harvesting. - Based on Stella definitions, adapted by NWRM project experts and validated by the European Commission

Early sowing

Early sowing refers to sowing up to six weeks before the normal sowing season.ᅠ This allows for an earlier and quicker development of crops and of a root network that leads to soil protection.ᅠ The period in which the soil lies bare is shorter and, therefore, erosion and run-off are less significant and water infiltration is improved.ᅠ Early sowing can also help to mitigate the extreme ETP rates typical of Mediterranean summers.ᅠ However, early sown plants are frost sensitive; therefore farmers run the risk of losing the crops because of the low temperatures.ᅠ In northern countries, temperature in spring (March) can be adequate but the risk of frost is still serious until May.ᅠ Therefore, early sowing requires specific tools (plastic tunnel covers, onsite green house, etc.) and cannot be applied by any farmers for any crops. - Based on Stella definitions, adapted by NWRM project experts and validated by the European Commission

Economic cost

Sacrifice associated to the use of available resources to one means instead of another (so that any economic cost is indeed an opportunity cost) or of following one course of action instead of the best available alternative. As applied to NWRM, it refers to those negative impacts in terms of welfare, either direct or indirect, that may be linked to the implementation of any measure. The difference between explicit and implicit costs depends on whether there is an unequivocal monetary payment (or at least one which is straightforward to infer) or not. The term モdirect (economic) costヤ does actually refer to those costs that fall directly on the promoter of the NWRM. Hence, as opposed to direct costs, indirect costs are those incurred by others (those who are not under the direct scope of the NWRM implementation).

Elimination of riverbank protection

The suppression of lateral constraints consists in removing some bank protection in order to enhance lateral connection of the river, diversifying flows (depth, substrate, speed), diversify habitats but also capping floods in the mainstream. - Based on Stella definitions, adapted by NWRM project experts and validated by the European Commission

Environmental cost

Negative impacts connected with the actual or potential degradation of natural assets or environmental quality due to economic activities.

Equivalent annual cost

The cost per year of implementing a NWRM over its entire lifespan. EAC is used when comparing NWRMs of unequal lifespans. It is estimated through listing all capital expenditures and when they are incurred; calculating the net present value of expenditures, once discounted; and converting this net present value into an annuity

Externality

(either positive or negative). Third-party effect or welfare impact, which is both unilateral (i.e. one cannot decide neither whether to suffer it or not nor how much impact to bear), and non-compensated. In other words, an externality stemming from the implementation of a NWRM is a cost (if negative) or a benefit (if positive), which is not directly reflected in the direct costs or benefits of the NWRM but are one of its outcomes. It is a welfare variation expressed in monetary units.

Filter strips

Gently sloping vegetated strips of land that provide opportunities for slow conveyance and infiltration. Designed to accept runoff as overland flow from upstream and to slow the progress of this runoff. - Based on Stella definitions, adapted by NWRM project experts and validated by the European Commission

Financial cost

The (monetary) value of resources deployed for the implementation of any NWRM, which includes upfront capital expenditures, either from new investments or the replacement of assets in past investments; depreciation allowances (annualised cost or replacing the accounting value of existing assets in the future); operating expenditures (those incurred to keep the NWRM running in an efficient manner); maintenance expenditures (for preserving existing or new assets in good functioning order throughout their useful life); and decommissioning costs (those incurred at the end of the lifecycle of the NWRM).

Forest harvesting

Forest harvesting can cause severe disruptions to the hydrologic cycle. Clearcut areas are often subject to localized flooding due to reductions in evapotranspiration caused by removal of trees. Roads and other infrastructure needed to support forest harvesting can also be significant sources of sediment to surface waters. However, negative effects can be minimized when forest harvesting is performed in a water-sensitive manner and measures are taken to maintain the natural hydrological functioning of the landscape.