A form of linkage between one store/component and another that involves movement of energy or mass
Input
The addition of matter and/or energy into a system
Store / Component
A part of the system where energy/mass is stored or transformed
System
A set of interrelated components working together towards some kind of process
Elements
The things that make up the system of interest
Attributes
The perceived characteristics of the elements
Relationships
Descriptions of how the various elements (and their attributes) work together to carry out some kind of process
Isolated systems
These have no interactions with anything outside system boundary. There is no input or output of energy or matter
Closed systems
These have transfers of energy both into and beyond the system boundary but not transfer of matter
Open systems
These are where matter and energy can be transferred from the system across the boundary into the surrounding environment. Most ecosystems are examples of open systems
Dynamic equilibrium
When there is a balance between the inputs and outputs. This means that the stores stay the same.
Positive feedback
Where the effects of an action are amplified or multiplied by subsequent knock-on or secondary effects
Negative feedback
Where the effects of an action are nullified by its subsequent knock-on effect
Atmospheric water
Water found in the atmosphere; mainly water vapour with some liquid water (cloud and rain droplets) and ice crystals
Cryospheric water
The water locked up on the Earth's surface as ice
Hydrosphere
A discountinuous layer of water at or near the Earth's surface. It includes all liquid and frozen surface waters, groundwater geld in soil and rock and atmospheric water vapour
Oceanic water
The water contained in the Earth's oceans and seas but not including such inland seas as the Caspian Sea.
Terrestrial water
This consists of groundwater, soil moisture, lakes, wetlands and rivers
Sea Ice
When water in the oceans is cooled to temperatures below freezing.
Ice Sheets
Mass of glacial land ice extending more than 50,000km2
Ice caps
Thick layers of ice on land that are smaller than 50,000km2
Alpine glaciers
Thick masses of ice found in deep valleys or in upland hollows
Permafrost
Ground that remains at or below 0oc for at least 2 consecutive years
Rivers
Act as both a store and a transfer of water. Streams of water within a defined channel
Lakes
Collections of fresh water found in hollows on the land surface. Larger than 2 hectares in area
Wetlands
An area of marsh, fen, peatland or water, weather natural or artificial, permanent or temporary, with water that is static or flowing where there is a dominance by vegetation.
Groundwater
Water that collects underground in the pore spaces of rock.
Soil water
Held together with air in unsaturated upper weathered layers of the Earth
Biological water
Constitutes the water stored in all the biomass
Atmospheric water
Water that is found in the atmosphere, most commonly as a gas, such as water vapour
Evaporation
Occurs when solar radiation hits the surface of water or land and causes liquid water to change state from a liquid to a gas (water vapour)
Condensation
Air cools and holds less water vapour. This means that if it cools sufficiently then it will get to a temperature at which it becomes saturated (dew point temperature). Excess water in the air will then be converted to liquid water.
Interception storage
The precipitation that falls on the vegetation surfaces (canopy) or human-made cover and is temporarily stored on these surfaces. This type of water can be evaporated directly to the atmosphere, absorbed by the canopy surfaces or ultimately transmitted to the ground surfaces
Overland flow
The tendency of water to flow horizontally across land surfaces when rainfall has exceeded the infiltrationcapacity of the soil and all surface stores are full to overflowing
Percolation
The downward movement of water within the rock under the soil surface. Rate vary depending on the nature of the rock.
Run-off
All the water that enters a river channel and eventually flows out of the drainage basin
Saturated
This applies to any water store that has reached its maximum capacity
Stemflow
The portion of precipitationintercepted by the canopy that reaches the ground by flowing down stems, stalks or tree trunk
Transpiration
The loss of water from vegetation through pores (stomata) on their surfaces
Storm & rainfall event
An individual storm is defined as a rainfall period separated by dry intervals of at least 24 hours and an individual rainfall event is defined as a rainfall period separated by dry intervals of at least 4 hours