Water Flashcards

(51 cards)

1
Q

DEFINITION : Condensation

A

Condensation can happen at the high altitudes of the atmosphere or even at ground level.
In the atmosphere, water vapor condenses into liquid water.
Clouds are formed when water vapor condenses around minuscule particles such as specks of dust, salt, or pollutants in the air.

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2
Q

DEFINITION : Evaporation

A

Evaporation is the process in which water in its liquid state changes into its gaseous state.
In the water cycle, liquid water stored in the rivers, oceans, lakes, and other bodies of water evaporates, turns into water vapour, and rises into the atmosphere.

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3
Q

DEFINITION : Transpiration

A

Transpiration is the transfer of water vapour from vegetation to the atmosphere. This occurs mostly via pores in leaves known as stomata. 10% of atmospheric water originates from transpiration. Wind speed, availability of water to the plant and air temperature all affect the rate of transpiration at any one time.

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4
Q

DEFINITION : Percolation

A

Percolation is the downward movement of water through soil layers due to gravity and capillary forces. Percolation is an important process required to replenish aquifers that hold groundwater in the saturation zone. It is also a component of the water cycle.

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5
Q

DEFINITION :Infiltration

A

Infiltration is the movement of water into the soil. The type of soil affects the rate of infiltration. Sandy soil has a higher infiltration rate than clay soil. Water is transferred through the soil as throughflow. Water moves through soil under the force of gravity towards rivers and streams.

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6
Q

DEFINITION : Ground water flow

A

Ground Water Water from precipitation can flow through the soil-water belt under the force of gravity.
We call this flow percolation. Eventually, the percolating water reaches ground water. Ground water is the part of the subsurface water that fully saturates the pore spaces in bedrock, regolith, or soil

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7
Q

DEFINITION : Surface Run Off

A

Water that runs on land

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8
Q

What type of system is the global hydrological cycle

A

Closed Cycle - water can neither enter nor leave the system.

The sum total remains constant being stored in oceans/lakes/icecaps

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9
Q

What flows are driven by the sun?

A

CET

Condensation
Evaporation
Transpiration

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10
Q

What flows are driven by gravity?

A

PIGS

Percolation
Infiltration
Ground water flow
Surface RunOff

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11
Q

DEFINITION : Flux

A

The measure of the rate of flow between stores

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12
Q

STATISTIC : What percentage of the earths water is stored in OCEANS?

A

96.9%

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13
Q

STATISTIC : What percentage of the earths water is stored in ICE CAPS/ GLACIERS?

A

1.9%

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14
Q

STATISTIC : What percentage of the earths water is stored in GROUNDWATER

A

1.1%

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15
Q

STATISTIC : What percentage of the earths water is stored in RIVERS?

A

0.01%

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16
Q

Name the three atmospheric systems

A

Polar
Ferrell
Hadley

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17
Q

What is the air pressure at the equator?

A

Low

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18
Q

What is the air pressure at 30’ N/S

A

High

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19
Q

What is the air pressure at 60’ N/S

A

Low

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20
Q

What is the air pressure at 90’ N/S

A

High

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21
Q

What two latitudes are considered deserts?

A

30’ and 90’

22
Q

Where is convectional rainfall more common?

23
Q

Where is frontal rainfall more common?

24
Q

Which way does air move through pressures?

25
What creates trade winds?
Air flows from high to low pressure and the corilanus effects moves it towards the west
26
DEFINITION : Porosity
Number of air pockets in a place
27
DEFINITION : Permeability
Whether air pockets are well connected
28
How does CONVECTIONAL rainfall form?
The sun heats the ground which heats the air above it as well as the moisture on the ground. The air rises with moisture which condenses and forms rain. Cumulonimbus clouds
29
How does FRONTAL rainfall form?
When cold air meets warm air, the warm air rises and the cold air is forced underneath which forms forms clouds and rain. UK
30
How does OROGRAPHIC rainfall form?
Cool wet air is forced over a mountain, it condenses and rains on one side of the mountain, leaving a rain shadow on the other side.
31
What type of system in a Drainage Basin?
Open There are several inputs and outputs.
32
What increases the capacity of the interception store?
Light precipitation for a short duration.
33
What slows down percolation?
Permeable Ground Slopes at low gradients Pours poorly connected
34
Physical factors that effect a drainage basin
PIGIVE Precipitation Infiltration Geology Interception Vegetation Evaporation
35
DEFITION : Evapotranspiration
The combined effect of evaporation and transpiration. 100% output in arid 75% output in humid areas
36
DEFINITION : Water Budgets
Annual balance between inputs and outputs and their impacts on soil water availability. INPUT = OUTPUT + OUTPUT +- INPUT
37
- C A - - - - B = - - ===== == - E -= D = - = - -= = ------------------- = = = evapotranspiration - precipitation
a max precip b max evap c soil mois surplus d soil mois deficit e soil mois recharge
38
DEFINITION : River Regime
Annual variation in river discharge
39
What effects a rivers regime?
Humans Precipitation Evapotranspiration Geology
40
How can human activity effect regimes?
Rural areas Urban Surfaces Dams
41
DEFINITION: LAGTIME
Time is takes for precipitation to fall to peak flooding
42
DEFINITION: PEAK DISCHARGE
The highest amount of discharge
43
DEFINITION: Baseflow
Average amount of riverdischarge on a normal day
44
DEFINITION: Rising Limb
Water discharge gradually increasing
45
What does a storm hydrograph show?
How a rivers discharge changes over a short period of time
46
Why do storm hydrographs vary?
S S I G C H Steepness High intensity rain Impermeability Smaller basin Low porosity Vegetation
47
How is the global air circulation driven?
the heating of the earths surface at the equator
48
What does ITCZ stand for?
Intertropical convergence zone
49
What is the ITCZ
The area of low pressure from where the trade winds meet near the equator.
50
Why does the ITCZ move?
Land heats up quicker than the ocean and theres more land in the north- different hemisphere seasons.
51
How do monsoons form in the northern hemisphere
Dry cool air falls on the continent which is high pressure. Wind moves from high to low pressure so the wind picks up water which is condenced.