4.1 Introduction to water systems Flashcards
what kind of radiation drives the hydrological cycle
solar radiation
what fraction of the Earths water storage does fresh water make up
a small fraction (approximately 2.6% by volume)
storages of the hydrological cycle
- atmosphere
- organisms
- soil
- oceans
- groundwater
- lakes
- rivers
- glaciers
- ice caps
transformation flows within the hydrological cycle
( a change in the state of water during the movement process)
- Evaporation: Water changing from liquid to gas.
- Transpiration: Water vapor released from plants.
- EVT (evotranspiration) = most important aspect of water loss as its about 100% of annual percipitation in arid areas, and 75% in humid areas
- Condensation: Water vapor turning into liquid droplets.
- Sublimation: Ice changing directly to water vapor.
transfer flows within the hydrological cycle
( the movement of water from one storage to another without changing its state)
- Surface runoff: Water flowing over land surfaces into streams and rivers.
- Infiltration: Water seeping into the ground.
- Stream flow/currents: Movement of water in rivers and oceans.
human impacts on the hydrological cycle A
Agriculture
- Irrigation diverts water from natural water bodies, altering local water balances.
- Overuse of groundwater for irrigation can lead to aquifer depletion.
- Agricultural practices can increase surface runoff and soil erosion.
human impacts on the hydrological cycle D
Deforestation
- Reduces transpiration and increases surface runoff.
- Can lead to increased flooding and decreased water quality.
human impacts on the hydrological cycle U
Urbanisation
- Increases surfaces that dont let water through, reducing infiltration and increasing surface runoff.
- Can lead to urban flooding and decreased groundwater recharge.
Ocean circulation systems
driven by differences in temperature and salinity that affect water density. the resulting difference in water density creates a global “conveyor belt” of ocean currents that distributes heat around the world, so affecting the climate.
The Ocean Conveyor Belt
- Surface currents carry warm water from the equator towards the poles.
- As water cools near the poles, it becomes denser and sinks.
- Deep ocean currents carry cold water back towards the equator.
- This cycle helps distribute heat globally, influencing climate patterns.
inputs and outputs of the hydrological cycle
- Primary input: Solar radiation driving evaporation.
- Outputs: Water leaving the system (e.g., deep groundwater storage).
link between the hydrological cycle and climate
- Water vapor is a greenhouse gas, meaning it traps heat in the Earth’s atmosphere. As temperatures rise due to other greenhouse gases (like CO₂), more water evaporates, increasing the amount of water vapor in the atmosphere.
This amplifies the greenhouse effect, causing further warming. This is a positive feedback loop. - Cloud formation increases global albedo and therefore lowers temperature. BUT cirrus clouds (low, thin) trap heat (infrared radiation) and lead to higher temps, contributing to gh effect.
- Ocean currents distribute heat, shaping regional climates.