Normal conditions- Trade winds push warm, moistair and water to Australia, causing precipitation in Australia, Upwelling- coldwaterreplaceshotwater. Peru- colderairsinks, causing dry conditions
El Nino- Weaker trade winds- causing warmerair and water to travel to Peru. Peru- slightlywetter. Australia- slightlydryer
La Nina- (Extreme of normal conditions) Strongtradewinds towards Australia. Hot air leads to highprecipitation in Australia. Australia- flooding. Peru- drought.
What is the impact of drought in wetlands?
Less water in wetlands causes soil and wateracidification, leads to more decomposition of organicmatter, releasing CO2 and methane e.g. Iraq, Australia
Lessfloodcontrol
Wetlands filterwater- less fresh water supplies
Less criticalbreedingground for species
What impact does drought have on forests?
Tree mortality- Californiadrought2010s caused death of 100M
Increasedwildfirerisk, fires spread rapidly through dryvegetation e.g. California
More vulnerable to pests and diseases
Exposed areas are more vulnerable to soilerosion- less fertilesoil
What is flash flooding?
Flooding caused by intense, heavyrainfall in a shortperiod of time. Not much infiltration occurs and lagtime is short, so surface-run off significantly increases. e.g Spain2024
How is climate change affecting the hydrological cycle?
Increased precipitation in highlatituderegions e.g. NorthernEurope and America
Decreased precipitation in Mediterranean, SouthernAfrica and Australia. Leads to decline in groundwaterlevels
Tropical regions- Intenserainfall events in wetseasons and longer dryseasons in Amazon and CentralAfrica
Reduced water storage in cryosphere, Affects countries that rely on glacialmeltwater in dryseasons e.g. CentralAsia, Andes
ColoradoRiver- Use of dams has Mexico has reduced waterflowdownstream
AralSea- Use of dams has increasedwatercapacity on Kazakhstan but not Uzbekistan
RiverNile- Construction of dams on BlueNile, Ethiopia will affect Egypt's wateravailability
Define the different flows in a drainage basin
Interception: Water is absorbed by vegetation before reaching soil.
Infiltration: Water is absorbed by the soil.
Percolation: Water is absorbed by permeablerocks
Throughflow: Water is transferredthrough the soil.
Groundwater flow: the very slowtransfer of percolatedwater through permeablerocks.
Surface runoff- the movement of water that across the surface of the ground
Channel flow is where waterflows in smallchannels into another largerdrainagebasin
What are types of rainfall?
Frontal rainfall- warmmoistairrises over a colderairmass, causing rain along warm and coldfronts. Occurs in low pressure areas e.g. UK
Orographic rainfall- Warmmoistair is forced to rise due to high relief. Aircondenses which produces rainfall e.g. Himalayas
Convectional rainfall- Solarenergy causes moistair to rise due to evaporation and evapotranspiration. The aircondenses which produces rainfall. Occurs in warm, tropical areas e.g. Brazil
What are inputs to the drainage basin?
Inputs are the addition of water to a drainage basin through precipitation
How do inputs vary?
Inputs vary through form (rain, sleet, snow) intensities (flood, drought) and frequency (monsoon, seasons).
How do humans disrupt the drainage basin?
Irrigation- water is transferred to farms with a soil moisture deficit
Deforestation- less water is intercepted and absorbed into soil. Soil becomes less permeable over time. Loss of vegetation leaves soil vulnerable to erosion.
Groundwaterabstraction- use of freshwater stored in groundwater aquifers.
Construction of dams- reduces water flow downstream. Soil becomes less permeable over time. When water is let downstream due to risk of overflowing, there is more surfacerunoffdownstream and soil cannot infiltrate.
Urbanisation- use of impermeable materials like concrete and tarmac increase surface run-off
What are the different parts of the storm hydrographs?
Peak rainfall- highest amount of rainfall
Peakdischarge - highest amount of water carried in the river channel
Lag time- Time period between peak rainfall and peak discharge
Base flow- normal flow of river
Storm flow- Flow from increased precipitation, involving surface and thorough flow