Water cycle Flashcards

1
Q

System

A

An assemblage of interrelated parts that work together by way of a driving process

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2
Q

Open system

A

Matter and energy transferred in/out of system boundary

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3
Q

Closed system

A

Energy transferred in/out of system boundary e.g. water cycle

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4
Q

Isolated system

A

No energy/matter transferred in/out of system boundary

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5
Q

Stores

A

Parts of the system where energy/mass is stored/transferred

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6
Q

Components/elements

A

Things that make up the system of interest

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7
Q

Attributes

A

Perceived characteristics of elements

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8
Q

Relationships

A

How elements and attributes interact to carry out a process

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9
Q

Dynamic equilibrium

A

Balance between inputs and outputs with unchanging store magnitude, preserved by negative feedback, disrupted by positive feedback

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10
Q

Earth system

A

Closed system with four major open subsystems (atmosphere, lithosphere, hydrosphere, biosphere) to form a cascading system

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11
Q

Water stores

A

Oceanic, cryospheric, terrestrial, atmospheric. Not evenly distributed worldwide (Antarctic ice caps, NW Saharan aquifers). Transfers over time

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12
Q

Water remains in shallow groundwater stores for how long

A

100-200 years

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13
Q

Water remains in deep groundwater stores for how long

A

10,000 years

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14
Q

Water remains in seasonal snow cover for how long

A

2-6 months

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15
Q

Water remains in glaciers for how long

A

20-100 years

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16
Q

What % of the Earth’s water is saline

A

97.5%

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17
Q

Of the % freshwater, what % is snow and ice

A

68.7%. 95% in 2 ice sheets covering Antarctica and Greenland. Long and short term storage

18
Q

Of the % freshwater, what % is aquifers

A

30.1%. Can be fossil (NW Sahara), saline, etc.

19
Q

Of the % freshwater, what % is surface and other

A

1.2%

20
Q

Relief rainfall

A

Warm moist ocean air hits highland, rises, cools, and condenses, causing rainfall and a rain shadow on the other side

21
Q

Convectional rainfall

A

Evaporation saturates air to be energetic and unstable, it then rises with particles bumping into each other making charge, at dew point temp this forms storms

22
Q

Frontal rainfall

A

Warm and cold air from equators and poles meet, different densities don’t mix so warmer rises, cools, and condenses to rain. Temperature inversion forms fog

23
Q

Global atmospheric circulation model

A

Explains cloud formation and precipitation varying with time and space. Inter-tropical convergence zone, local variance with storms, mid-latitude cloud formation from air convergence and jet streams

24
Q

Glacial cycle significance

A

Currently in interglacial period where ablation>accumulation so functional hydrological cycle, in past interglacial 50m higher water levels

25
Q

P=

A

Q+E+-change in storage

26
Q

Water budget graph

A

Months on x-axis, mean precipitation on y-axis, mean evapotranspiration on z-axis

27
Q

Flashy hydrograph

A

Flood, short lag time

28
Q

Subdued hydrograph

A

No flood, long lag time

29
Q

Physical factors affecting lag time

A

Gradient, antecedent rainfall, geology, vegetation, rainfall amount and intensity, basin size, drainage density

30
Q

Human factors affecting lag time

A

De/afforestation, agriculture, urbanisation, flood alleviation schemes, water abstraction

31
Q

Physical factors affecting water cycle

A

Rock permeability, evaporation rate, precipitation, drought, soil, topography, desertification, extreme weather events

32
Q

Human factors affecting water cycle

A

Climate change, de/afforestation, agriculture, land use, urbanisation, abstraction, desertification, irrigation

33
Q

Effect of drought on the water cycle

A

2012-16 Californian drought

34
Q

Effect of land use changes on the water cycle

A

Mainly from urbanisation and deforestation

35
Q

Effect of seasonal changes on the water cycle

A

Affect soil water, river channel flow, evaporation, vegetation and precipitation

36
Q

Effect of farming practice on the water cycle - UK

A

East Anglian Fens and Somerset levels drained to farm, 584m tonnes C in English peatlands, lowered water table so friable peat and Fen Blows, still floods e.g. 2014 Somerset

37
Q

Effect of farming practice on the water cycle - global

A

Perforated plastic tube network below soil surface for drainage, aerates soil, Ohio State University shows for $1 spent on corn/soy $1.20-1.90 back. However, nitrate loss, expensive, more throughflow, eutrophication, dry topsoil

38
Q

Effect of abstraction on the water cycle - Middle East

A

Aquifers in danger of depletion so use nets to stop evaporation

39
Q

Effect of abstraction on the water cycle - Malta

A

Must desalinise as saline intrusion

40
Q

Effect of abstraction on the water cycle - Greek Argolid Plains

A

400m deep seawater contaminated boreholes

41
Q

Effect of abstraction on the water cycle - London

A

Chalk-basal sands aquifer overabstracted in 19th and 20th century so in 1960s 88m below sea level. Deindustrialised, rise at 3m/yr, threatened London Basin, 2000-14 GARDIT, E,C+S fell