Enquiry 1 what are the processes operating within the hydrological cycle from global to local scale Flashcards

1
Q

water cycle

A

operates on a variety of scales where physical processes control the circulation of water between stores on land, oceans, the cryosphere and atmosphere

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2
Q

type of cycle

A

closed system with inputs (precip), outputs, stores and flows

driven by solar energy and gravitational potential energy

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3
Q

stage 1

A

EVAPORATION: water vapour from oceans is lifted and condensed in the atmosphere to form clouds

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4
Q

stage 2

A

MOISTURE: transported around the globe, some evaporates back into atmos and some percolate the ground to form groundwater

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5
Q

stage 3

A

Balance of water that remains on the surface is called RUNOFF and is emptied into lakes, rivers and streams which carry it back to the ocean

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6
Q

ocean store

A

water- 96.9%

residence time- 3,600yrs

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7
Q

Icecaps

A

water- 1.9%

residence time- 15,000yrs (size dependent)

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8
Q

groundwater

A

water- 1.1

residence time- up to 10,000 yrs

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9
Q

rivers/lakes

A

water-0.01

residence time- 2 weeks to 10yrs

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10
Q

blue water

A

water in rivers/lakes (visible)

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11
Q

green water

A

water in soil/vegetation (invisible)

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12
Q

deep-seated groundwater

A
not renewable
Sahara desert
fossil water
result of the pluvial period
not reachable
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13
Q

accessible stores

A

soil moisture

lost to other stores by evap/ transpiration/ groundwater flow

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14
Q

water for life support

A

2.5% of global water is freshwater
rivers have 0.007% so are a source of conflict/disputes
30% in groundwater/ some fossil water (slow turnover period)

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15
Q

drainage basin

A

an area of land drained by a river

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16
Q

interception

A

precip that does not reach the soil as it is intercepted by vegetation and forest floor

17
Q

throughflow

A

flowing of water within the soil, moving towards the river

18
Q

infiltration

A

water on the ground soaking into the soils and porous rock

19
Q

percolation

A

movement of water through the soil or underlying porous rock, being stored as groundwater

20
Q

outputs in a drainage basin

A
evapo
runoff (all the water that enters a river channel and eventually flows out of the drainage basin)
21
Q

evapotranspiration in a drainage basin system

A

the total output of water from the drainage basin directly into the atmos

22
Q

stores in a drainage basin

A
interception storage
surface water
soil water
groundwater
channel storage
23
Q

transfers in a drainage basin

A

stemflow
infiltration
overland flow
channel flow

24
Q

watershed

A

boundary that separates one drainage basin from another, typically following a ridge or high land

25
drainage basin as an open system
it exchanges matter with its surroundings
26
human disruptions to the drainage basin
``` deforestation farming and irrigation dam construction pollution from industry urbanisation ```
27
physical factors affecting outputs (climate)
climate- (temp and precip patterns determine availability and vary according to latitude) seasonality determines patterns summer temp increases evap but plant growth increases transpiration equatorial areas receive the most rainfall
28
physical factors affecting outputs (geology)
geology- determines underground storage according to permeability
29
physical factors affecting outputs (river systems)
flow increases downstream but climate creates variation in discharge and water loss
30
Water budgets
Show the annual balance between inputs (precipitation) and outputs(evapotranspiration) and their impact on soil water availability
31
Water budgets influenced by
Climate types Temperate- mood temps and steady climate Tropical-tropical wet/ monsoon/ wet and dry seasons Polar-tundra and Ice caps. Tundra summers are short and in ice cap seasons temps are seldom above freezing
32
Storm hydrographs main features
Peak discharge- reached after peak rainfall Rainfall input- discharge rise and rising limb Storm input cease and river water decrease- recessional limb Time interval- between peak rainfall and discharge= lag time Discharge returns to normal (base flow)
33
Storm hydrographs shape factors
``` Shape- circular basin( shorter lag time and ‘flashy river’) Elongated basin (delayed and ‘flat river’) ``` Weather/climate- high temp (high evap) and steady rain (less infiltration) = flat river Human activity- urbanisation(impermeable) = flashy river
34
Soil moisture budget
Soil moisture surplus Soil water utilisation Soil water deficit Soil water recharge Field capacity