unit 4 Flashcards
water on earth
Fresh water only makes up a small fraction (approximately 2.5% by volume) of the Earth’s water storages
Of this fresh water, approximately 68.7% is stored in glaciers and ice sheets and 30% is stored as groundwater
The remaining 1.3% of freshwater is in rivers, lakes and the atmosphere
All water is part of the hydrological cycle
the hydrological cycle
The hydrological cycle is a closed system
Within the hydrological cycle, there are stores and transfers (flows)
The hydrological cycle is a series of processes in which water is constantly recycled through the system
The cycle also shapes landscapes, transports minerals and is essential to life on Earth
the main processes that occur within the hydrological cycle
Evaporation - the sun evaporates surface water into vapour
Condensation - water vapour condenses and precipitates
Flows - water runs off the surface into streams and reservoirs or beneath the surface as ground flow
These processes transfer the water on Earth from one store to another (river to ocean or ocean to atmosphere)
The hydrological cycle involves energy exchange, leading to local temperature fluctuations
As water evaporates, it absorbs energy from its surroundings
This effectively cools the environment
The reverse happens when water condenses (heat is released)
This heat exchange influences the local climate
storages in the hydrological cycle include
Rivers, lakes and oceans
Groundwater (aquifers)
Soils
The atmosphere
Glaciers and ice caps
Organisms (e.g. trees)
flows in the hydrological cycle include
Evapotranspiration
Sublimation
Evaporation
Condensation
Advection
Precipitation
Melting
Freezing
Flooding
Surface run-off
Infiltration
Percolation
Stream-flow or currents
evaporation
The process by which liquid water changes into a gaseous state (water vapour) and enters the atmosphere from water bodies such as oceans, lakes, and rivers
transpiration
The process by which plants absorb water from the soil through their roots and release it as water vapour through tiny openings called stomata in their leaves
evapotranspiration
The combined process of water vaporisation from the Earth’s surface (evaporation) and the release of water vapour by plants through transpiration
sublimation
The direct transition of water from a solid (ice or snow) to a vapour state without melting first
condensation
The process in which water vapour in the atmosphere transforms into liquid water, forming clouds or dew, as a result of cooling
advection
The horizontal movement of water vapour, clouds, or precipitation caused by the prevailing wind patterns
precipitation
The process of water falling from the atmosphere to the Earth’s surface in the form of rain, snow, sleet, or hail
melting
The process by which solid ice or snow changes into liquid water due to an increase in temperature
freezing
The process by which liquid water changes into a solid state (ice or snow) due to a decrease in temperature
flooding
The overflow of water onto normally dry land, often caused by heavy rainfall, melting snow, or dam failure
surface run-off
The movement of water over the Earth’s surface, typically occurring when the ground is saturated or impermeable, leading to excess water
infiltration
The process of water seeping into the soil from the surface, entering the soil layers and becoming groundwater
percolation
The downward movement of water through the soil and underlying rock layers, eventually reaches aquifers or groundwater reservoirs
stream-flow or currents
The movement of water in streams, rivers, or other water bodies, driven by gravity and the slope of the land, ultimately leads to oceans or lakes
human impact on the hydrological cycle
Human activities, such as agriculture (specifically irrigation), deforestation, and urbanisation, have significant impacts on the hydrological cycle, altering the natural processes of surface run-off and infiltration
The impact of agriculture and irrigation on the hydrological cycle
Irrigation is the process of artificially supplying water to agricultural crops
It has a direct impact on the hydrological cycle by modifying the water distribution and availability in a region
Increased irrigation leads to artificially high evapotranspiration rates as more water is supplied to plants than would occur naturally, resulting in increased atmospheric moisture levels
This can lead to localised increases in precipitation downwind of irrigated areas, altering rainfall patterns in the region
Additionally, excessive irrigation can result in increased surface run-off
When water is applied faster than the soil can absorb it, it flows over the surface, carrying sediments, fertilisers, and pesticides, leading to water pollution and nutrient imbalances
the impact of deforestation on the hydrological cycle
Deforestation refers to the clearing or removal of forests, primarily for agriculture, logging, or urban development purposes
Forests play a crucial role in the hydrological cycle
They act like natural sponges, absorbing rainfall and facilitating infiltration, which helps recharge groundwater and maintain stream flows
When forests are cleared, surface runoff increases significantly
Without the tree canopy and vegetation to intercept and slow down rainfall, more water reaches the ground surface, leading to higher surface runoff rates
Deforestation also reduces evapotranspiration rates
As trees are removed, there is less transpiration and evaporation occurring, resulting in reduced moisture release into the atmosphere
Overall, deforestation disrupts the balance between surface run-off and infiltration, leading to increased erosion, reduced groundwater recharge, and altered stream flow patterns
the impact of urbanisation on the hydrological cycle
Urbanisation involves the transformation of natural landscapes into urban areas with buildings, roads, and infrastructure
Urban development dramatically alters the hydrological cycle by replacing permeable surfaces (such as soil and vegetation) with impermeable surfaces (concrete, asphalt)
Impermeable surfaces prevent infiltration, leading to reduced groundwater recharge
Instead of infiltrating into the soil, rainfall quickly becomes surface runoff, resulting in increased flooding and diminished water availability during dry periods
Urban areas typically have efficient drainage systems designed to remove the excess water quickly
This further accelerates surface runoff, which can overload natural water bodies and cause downstream flooding
Urban areas often experience higher temperatures due to the urban heat island effect
This effect, caused by the concentration of buildings and paved surfaces, increases evaporation rates, altering local precipitation patterns
what causes ocean circulation
Ocean circulation systems are driven by differences in temperature and salinity
The resulting difference in water density drives the ocean conveyor belt, which distributes heat around the world and thus affects climate
ocean conveyor belt
Ocean currents redistribute heat energy around the globe
The currents (warm or cold) act a bit like ‘rivers’ of water in the sea
Cold currents move towards the equator and warm currents towards the poles
Each ocean has its own pattern of currents
E.g. the warm Atlantic Ocean waters of the low latitudes are moved to high latitudes via the North Atlantic Drift
how are ocean currents triggered
by the prevailing surface winds created by global atmospheric circulation
how is ocean circulation maintained
hrough convection currents driven by cold water freezing into ice at the poles
The polar cold waters contain denser, saltier sea water, which sinks to the ocean floor
Water then flows in above it at the surface, which forms a current
The deep ocean currents then flow towards Antarctica along the western Atlantic basin, before splitting off into the Indian and Pacific Oceans where the water begins to warm up
The warming makes the water less dense so it loops back up to the ocean surface in the South and North Atlantic Ocean
The warmed surface waters continue to flow around the globe and eventually return to the North Atlantic, where the cycle begins again
This movement of water is known as the thermohaline circulation and drives the ocean conveyor belt