water Flashcards
(53 cards)
is the orlds hyrological cycle an open or closed system
a closed system and therefore no water can enter or leave. Therefore the imputs and outputs are balancefd and the amount of water on earth does not change
however on a local scale it is an open system with imputs outputs and throughputs
imputs and outputs of the water cycle
imputs- precepitation(water rain, snow and hail)
outputs- evaporatio, streamflow traspiration
stores of water are
an accumulation or quantity of water or carbon in a system
2 processes that drive the global hydrological cycle
evaporation due to heat in the solar cycle
gravitational potential energy- the way gravity drives the movment of water
Types of preceptitation- 1- orographic
common in the western parts of the uk
warmer moist air from the atlantic rises as it reaches the western upland it begins to cool aover high ground producing heavy rain over the west and north of the uk
types of preceptitation2- convectional
typical in eastern and south eastern k in summer when it is hot rain is intense and causes thunder and lightning
types of precipitation 3- frontal
low pressure areas form fronts (depressions) then when cold air from poles reaches warm air from south west warm air is forced over the cold air t create a warm or cold front
global water budget- where is the fresh water
97% of global water is stored in oceans
only 2.5% are fresh water- 69% being stored in glaciers
1% in living things
30% is groundwater
hydrology in polar regions
permafrost creates impermable surfaces
lakes and rivers freeze
rapid run off in spring
organic and frontal precipitation
hydrology in tropical regions
dense vegettion consume 75%
deforestation limits evapotranspiration
high temps and humid
itcz
earch consists of several hemispheres-
and different cells
hadley cells
polar cells
ferel cells
factors effecting the volume of imputs into a drainage basin…
- seasonality- change in weather depending on change in time of the year
- varability- sudden or long term changes in the climate which could effct precipitation and therfore the drainage basin directly
-secular variablity- long term climate events
-periodic variability- short term annual events
-stochastic variability- such as localistatio of thunderstorms
3.lattitude of the drainage basin the higher the lattutude the further from the equator and therefore the more snowfall and precipitation
what is and how does interception effect rainfall
when the surface of or a plant or leaf catches rainfall changing its direction or storing it stopping it from reaching the groun. The level of interception can depend on the plant type
what is infiltration-
the movment of water from the surface to the soil#
factors effceting infiltration
- soil composition- sandy soil can infiltrate more than clay
- previous precipitation- more saturated soil which already has high stores of precipitation cannot infliltrate as much water leading tob more surface run off after long periods of rainfall
- type and amount of vegitation- plants with dense root growth will have maximum infiltrationa and plants with many leaves will stop water reaching ground reducing infiltration into soil
- relief of land- if land is sloped this will lead to more surface run off and less infiltration
what is throughflow
when water foves through soil and ground and reaches and becomes a store in a river or lake. speed of low depends on soil eg sandy soil will be fatser than clay soil
what is percolation
when water flows into fractures of rocks or into aquifers as it percolates from the ground into rocks
what is groundwater
the gradual transfer of water through pourous rocks, this can often get trapped tp form aquifers and is a very slow process
since drainage basin is an open system what are their 3 main outputs
- evaporation- this is the direct loss of water. it is more common on warm windy and dry days
evaporation depends on-
1. volume of water, more water evaporates quicker
2. canopy cover anhything covering the soil will reduce evaporation
3. colour of the surface- any dakrer surface means evaporation will happen faster
-transpiration- where water is lost to the atmosphere through the pores of plants but can be effected by the moisture and time of day
what are the stores of water
water stored in soil- utilised by plants
groundwater- water that is stored in the pore spaces of rock
river channel- water stored in a river
physical factors influencing a drainage basin
climate- influences amount of rainfall and vegetation growth
soil composition-influences rate of throughflow and infiltration
geology- effcets percolation
relief- steeper gradients of ground will encourage fater rates of run off
human factors iinfluencing a drainage basin
deforestation- more deforestation means they is less vegetation and less infiltration
more overland flow leading to more flooding
more surface sun off
dams- reduce flow down stream- increasing river stores- more evaportation
urbanisation- less impermable surfaces less infiltration and increase surface run off
overabstraction- when peopole overabstract an aquifer eg- brazil build illegal wells as price of licence went up and water inecurity got worse
what is a drainage basin
a local scale hydrological process. operated within areas
water budget definition
the difference in imputs of water and outputs of water in any given area