Water Cycles Flashcards

(56 cards)

1
Q

Outline the 4 global freshwater storages and how much they store (in %)

A

Lakes = 20.9%
Ground Ice & Permafrost = 69%
Living things = 0.26%
Rivers = 0.44%

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2
Q

Outline the 4 major physical systems of the Water Cycle`

A

1.Lithosphere (land)
2.Hydrosphere (water)
3. Cryosphere (frozen water - snow & ice)
4. Atmosphere (air)

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3
Q

Outline the water type % for the global water cycle

A

Saline water = 97.4%
Fresh water = 2.5%

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4
Q

Outline the coverage, and storage of Oceanic water.

A

72% surface coverage
97% water storage
5% explored

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5
Q

Outline how Carbon has changed the pH in Oceanic water and why

A

250 years ago - 8.25
Now: Saline, alkaline water of pH 8.14
Increase of atmospheric C

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6
Q

Outline how Sea Ice forms and why it doesn’t raise sea levels when it melts

A

Oceans r cooled to below freezing temperatures
From oceanic water so doesn’t raise

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7
Q

Outline how Ice Shelves form and their impact on the ocean

A

Ice sheets/glaciers drift into oceans (mostly in Antarctica & Greenland)
Raise sea lvl only when they drift out to sea not melting

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8
Q

Outline what Ice Sheets are and how they form

A

Glacial ice > 50,000 km^2
Layers of snow pile up 1000s of yrs -> grow thicker old layers compress

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9
Q

Outline the storage of freshwater in Ice Sheets and why they constantly move

A

Greenland & Antarctica store >99%
Slowly flowing under their own weight

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10
Q

Define Ice Caps and where they form

A

Thick ice layers <50,000km^2
Form in the highest Mountainous areas and r dome shaped

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11
Q

Define Alpines and how they form

A

Thick ice masses in deep valleys/upland hollows
Fed by ice caps

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12
Q

Outline the importance of the 15,000 Alpine Glaciers in the Himalayas

A

Reservoir supporting rivers (Indus/Ganges)
Supports mils in South Asia

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13
Q

Outline how Permafrost and Subsea permafrost forms

A

Permafrost:
Ground at/below 0 C
Formed during cold glacial periods

Subsea:
Close to 0 C Arctic continental shelf

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14
Q

Outline the impact of melting Permafrost

A

Releases CO2&CH4 - climate change

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15
Q

Outline the impact of rivers on the water cycle

A

Store & transfer H2O
Transfer from ground, soil & atmosphere

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16
Q

Outline how Lakes form

A

Ground hollow >2ha
Fresh - N hemisphere Caspian Sphere

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17
Q

Outline how Wetlands form

A

Marsh, fen, peatland, water. Static water dominated by veg
Found in Polar area

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18
Q

Outline how groundwater forms and their storage

A

H2O collects in pore spaces of rock
>30% freshwater

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19
Q

Outline Aquifers and how they form

A

Underground reservoirs
Form in porous, permeable rock (chalk)

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20
Q

Outline the H2O table

A

Upper lvl of saturated rock

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21
Q

Outline how the H2O table rises & falls

A

Response to groundwater flow, H2O abstraction or recharge

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22
Q

Outline the difference of Porous/Sandy soils & Clay soils

A

Porous = hi storage low transfer
Clay = low storage hi transfer

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23
Q

Outline how Water Vapour causes + feedback

A

Absorbs/reflects/scatters solar radiation
Small increase in H2O = Increase of atmosphere temp

24
Q

Define groundwater flow

A

Slow H2O move thru underlying rock

25
Define Thrufall
H2O falls thru veg canopy to floor
26
Define Stemflow
Intercepted H2O flows down to ground on stems
27
Define Percolation
H2O moves down in rock under soil
28
Define Interception storage
H20 falls on veg/man-made surface Stored temporarily/evaporated (lowers floods)
29
Define Drainage basin
Land drained by river & tributaries (surface, soil & near surface)
30
Define Infiltration
H2O moves down surface -> soil
31
Define Thruflow
H2O movement downslope thru subsoil (effective with underlying permeable rock)
32
Define runoff
All H2O that enters a river channel & out of basin
33
Define Overland Flow
Infiltration capacity surpassed -> water flow across land
34
Define Saturated
H2O store @ max capacity
35
Define H2O Balance
Balance of inputs & outputs in a drainage basin
36
Define Transpiration
Loss of H2O from veg thru pores on surfaces
37
Define Evapotranspiration
Total output of H2O in drainage basin into atmosphere
38
Outline the features of a Flood Hydrograph
Lag time Rising Limb Peak Discharge Falling Limb Base Flow
39
Define Discharge & the equation
Vol of H2O flows river per second Discharge (m^3/s)=cross section area (m^2) X velocity (m/s)
40
Define Lag Time
Delay between peak rainfall & peak discharge (rain to reach river)
41
Define Rising Limb
Part of graph up to peak discharge
42
Define Falling Limb
Graph after peak discharge (less water flowing into river)
43
Define Base Flow
Start & finish lvl of river
44
Define Peak Discharge
Highest flow in channel
45
Define the features of a 'Flash' Hydrograph
Short lag time & high peak
46
Define the opposite of a 'Flash' hydrograph
Long lag time & low peak
47
Outline the features that cause a 'Flash' hydrograph (7 factors)
Small basin size High drainage density Impermeable Urbanisation Steep slopes Saturated Heavy Rain
48
Outline the features that cause the opposite of a 'Flash' Hydrograph to form
Large basin Low density Permeable Forests Gentle Slopes Dry soil absorbs Light rain
49
Outline Drainage Basin traits that affect hydrographs
1. Big drainage basin = more rain & hi peak discharge Small = opposite impact 2. Steep-sided = short lag time 3. Circular = short lag time even distance from watershed so more H2O
50
Outline how rock types affect Hydrographs
Impermeable rock -> low infiltration & hi surface runoff = short lag & hi dis
51
Outline how Soil Type affects Hydrographs
Clay soil = low infiltration ->short lag, hi dis
52
Outline how Veg affects hydrographs
Hi veg density -> more infiltration = long lag, low discharge
53
Outline how Precipitation affects Hydrographs (2 ways)
Intense storms & hi rain = HI PEAK Type of precipitation (winter storm = long lag time-must melt in heat)
54
Outline how Temperature affects Hydrographs (2 ways)
Hot, dry weather= short lag & HI peak High temp -> hi evapotranspiration = low peak
55
Outline how Human Factors affect Hydrographs
Urbanisation -> hi surface runoff = short lag & hi peak Drainage Systems -> H2O into river no evap/infiltr = short lag & Hi peak
56
Outline how Deforestation affects Hydrographs
Low interception/evaporation/infiltration = hi peak & flood risk