Water And Carbon Cycle Flashcards
System
A set of interrelated components working together towards some kind of process
Stores
A part of the system where energy/ mass is stored or transformed
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
Closed system
Energy is transferred into and out of the system. All matter is enclosed
Open system
Matter and energy can be transferred from the system into the surrounding environment
Dynamic equilibrium
The balanced state of a system. When opposing forces or inpupts and outputs are equal
Positive feedback
Occurs where the effects of an action are amplified by changes to the inputs/ outputs/ processes
(Process are enhance)
Negative feedback
Occurs where the effects of an action are nullified by changes to the input/outputs/ transfers
(Decelerates a process)
Drainage basin
The area of land surrounding a river, from which the river recieves water and subsequently drains this water
Precipitation
Rain, snow, hail and sleet
Infiltration
When water enters the ground
Interception
When water is caught by trees and plants
Stem flow
Water lands on plants and runs down their stems
Overland flow
Anywhere water flows over the land surface
Through flow
When water flows through the ground
Transpiration
When water vapour comes out of leaves
Evapotranspiration
Water rises as vapour from the ground or released from leaves
Ground water
Water deep in the ground
Soil water
Water held between soil particles
Ground water flow
The slow movement of groundwater
Percolation
Movement of water down through the ground
Surafce storage
Lakes, ponds and puddles
Ground water storage
Water stored underground in bedrock
Atmospheric water
Water found in the atmosphere
Terrestrial water examples
Rivers, wetlands, surface water, groundwater, soil water, biological water, biomass
Water balance
Within a drainage basin teh balance between inputs, outputs is known as water balance/ budget
River regime
How the water levels in a river change over the year
Water suplus
Precipitation exceeds evapotranspiration and the soil above field capacity (causes runoff)
Soil moisture utilisation
Evapotranspiration exceeds precpiitation. Plants and humans have to utilise water from the soil
Soil moisture recharge
When precipitation is greater tahn evapotranspiration agains so soil moisture is replenished until field capacity
Soil moisture deficiency/ water deficit
When all soil moisture is used up. Plants will wilt and may die - not enough water in the soil
Field capacity
The maximum amount of water that soil can hold
Discharge
Teh amount of water passing through the river each second
Discharge equation
Discharge = cross sectional area x velocity
Lag time
Time between peak rainfall and peak discharge
Rising limb
Increase in discharge until peak discharge following rainfall
Falling limb
Decrease in discharge following peak discharge
Base flow
The normal flow/ rate of discharge without precipitation
Peak rainfall
Highest amount of rainfall
Peak discharge
Point of highest amount of discharge
Storm runoff
Amount of discharge above base flow
Storm hydrographs
- bars = rainfall
- line = discharge
Flashy discharge
Discharge increases quickly
Subdued discharge
Very long lag time and peak discharge is low as a result
Carbon sequestration
The capture of CO2 from the atmosphere or capturing anthropogenic CO2 from large scale stattionary source before it is released into the atmosphere
Lithosphere
The crust and uppermost mantle; this constitues the hard and rigid outer layer of the earth
Carbon transfer
These are processes that transfer carbon between the stores - photosynthesis converts it into glucose
Carbon stores
The main stores of carbon are the lithosphere, cryosphere, atmosphere and biosphere
Greenhouse gas
Any gaseous compund in the atmosphere that is capable of absorbing infrared radiation, thereby trapping and holding heat in the atmosphere
Carbon sink
A store that absorbs more carbon than it releases
Weathering
The breakdown of rocks in situ by a combination of weather, plants and animals
Biosphere
The total sum of living matter