Water and Carbon Cycle Flashcards
Systems
On a local scale, the water and carbon cycles are both open systems however, on a global scale they are closed systems
The Water Cycle outputs
Run-Off
Evapotranspiration
Streamflow
The Water Cycle Inputs
Precipitation
The Water Cycle flows
Infiltration
Percolation
Throughflow
Surface runoff
groundwater flow
stemflow
The water cycle stores
Groundwater
Soil Water
River Channel
Interception
Surface Storage
The Water Balance
Used to express the rates of water storage and transfers in a drainage basin system
Precipitation = total runoff + Evapotranspiration +/- (Change in) Storage
Changes to the water system
Deforestation
Storm Events
Seasonal Changes
Agriculture
Urbanisation
Soil Water Budget
Annual balance between inputs and outputs in the water system and their impact on store water availability. Dependent on soil type and depth
Seasonal variation in the Soil Water Budget
Autumn; Greater input from precipitation than their is output from evapotranspiration as deciduous trees lose their leaves. Cooler temps mean plants photosynthesise less
Winter; Evapotranspiration from plants reaches minimum due to colder temps
Spring; Plants start to grow again and evapotranspiration increases, still a water surplus
Summer; Evapotranspiration peaks and rainfall is at a minimum, soil water stores are depleating
Water Cycle at a Global Scale
Oceans contain 97% of Earth’s water stores, Only 2.5% of stores is freshwater of which around 70% is stored in glaciers and 30% is stored as groundwater
How can water be stored?
Hydrosphere
Cryosphere
Atmosphere
Lithosphere
Inter Tropics Convergence Zone (ITCZ)
Determines precipitation and cloud formation, ITZM is a low pressure zone
Water Cycle Changes Over Time, natural
Seasonal changes
Storm Events
Droughts
El nino - Occures every 2-7 years and causes warmer temperatures
La Nina - Occurs every 2 - 7 years and causes cooler temperatures
Water Cycle Changes Over Time, Human
Farming
Land Use Changes
Over Abstraction
Flood Hydrographs
Discharge
Falling Limb
Rising Limb
Lag Time
Base flow
Flashy vs Subdued