Water and carbon

Subdecks (2)

Cards (67)

  • Flow / Transfer

    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 infiltration capacity 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 precipitation intercepted 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