Hydrological Cycle Flashcards

1
Q

What are drainage basins?

A

Local open systems

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2
Q

What is the global hydrological system?

A

A closed system - there are no input or outputs

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3
Q

4 facts about drainage basin hydrological cycles?

A
  1. a river’s drainage basin is the area surrounding the river where the rain falling on the land flows into that river. Also known as the river’s catchment
  2. the boundary of a drainage basin is the watershed - any precipitation falling beyond the watershed enters a different drainage basin
  3. drainage basins are open systems with inputs and outputs
  4. water comes into the system as precipitation and leaves via evaporation, transpiration and river discharge
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4
Q

Inputs - precipitation - define?

A

includes all the ways moisture comes out of the atmosphere

mainly rain, but also snow, hail, dew and frost

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5
Q

storage - water coming into the system - types? (5)

A
interception
vegetation storage
surface storage
groundwater storage
channel storage
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6
Q

explain interception

A

when some precipitation lands on vegetation or other structures, like buildings and concrete or tarmac surfaces, before it reaches the soil
creates a significant store of water in wooded areas
storage is only temporary as the collected water evaporates quickly

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7
Q

explain vegetation storage

A

water thats been taken up by plants

is all water contained in plants at any one time

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8
Q

explain surface storage

A

includes water in puddles (depression storage), ponds and lakes

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9
Q

explain groundwater storage

A

water stored in the ground, either in soil (soil moisture) or in rocks
water table is the top of the surface of the zone of saturation - zone of soil or rock where all the pores in the soil or rock are full of water
porous rocks (lots of holes in them) that hold water are called aquifers

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10
Q

explain channel storage

A

water held in a river or stream channel

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11
Q

types of flows and processes (10)

A
surface runoff
throughfall
stemflow
throughflow
infiltration
percolation
groundwater flow
baseflow
interflow
channel flow
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12
Q

explain surface runoff/overland flow

A

water flowing over the land
can flow over whole surface or in little channels
common in arid areas where torrential rain falls on hard baked land

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13
Q

explain throughfall

A

water dripping from one leaf (or another plant) to another

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14
Q

explain stemflow

A

water running down a plant stem or a tree trunk

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15
Q

explain throughflow

A

water moving slowly downhill through the soil

faster through ‘pipes’ - things like cracks in the soil, or animal burrows

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16
Q

explain infiltration

A

water soaking into the soil
infiltration rates are influenced by soil type, soil structure and how much water is already in the soil
in a heavy storm, water can’t infiltrate fast enough, so it flows over the surface

17
Q

explain percolation

A

water seeping down through soil into the water table

18
Q

explain groundwater flow

A

water flowing slowly below the water table through permeable rock
water flows slowly through most rocks, but rocks that are highly permeable with lots of joints (gaps water cannot get through) can have faster groundwater flow, e.g limestone

19
Q

explain baseflow

A

groundwater flow that feeds into rivers through river banks and river beds

20
Q

explain interflow

A

water flowing downhill through permeable rock above the water table

21
Q

explain channel flow

A

water flowing in the river or stream itself

also known as river’s discharge

22
Q

outputs - water leaving system

4 types?

A

evaporation
transpiration
evapotranspiration
river discharge/river flow

23
Q

explain evaporation

A

water turning into water vapour - liquid to gas

24
Q

explain transpiration

A

evaporation from plant leaves
plants and their trees take up water through their roots and transport it to their leaves where it evaporates into the atmosphere

25
Q

explain evapotranspiration

A

process of evaporation and transpiration together

26
Q

what is potential evapotranspiration

A

amount of water that could be lost by evapotranspiration

27
Q

what is actual evapotranspiration

A

what actually happens
e.g in desert PET is high (as heat increases amount of evap) but actual transpiration is low (as not much moisture in first place)

28
Q

what is the water balance

A

shows balance between inputs and outputs

affects how much water is stored in the basin

29
Q

what is the water balance in the UK

A
  1. in wet seasons, precipitation exceeds evapotranspiration. this creates water surplus. ground stores fill with water so theres more surface runoff and higher discharge, so river levels rise.
  2. in drier seasons precipitation is lower than evapotranspiration. ground stores are depleted as some water is used(e.g by plants/humans) and some flows into the river channel, but isn’t replaced by precipitation
  3. so, at the end of a dry season theres a deficit (shortage) of water in the ground. ground stores are recharged in the next wet season (i.e autumn)