The Global Water Cycle (Booklet 2) Flashcards

1
Q

What is the process of a solid (e.g. ice) vhanging to liquid (e.g. water) called?

A

Melting which uses latent heat

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2
Q

What is the process of a liquid (e.g. water) changing to a gas (e.g. vapor) called?

A

Evaporation which uses latent heat

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3
Q

What is the process of a solid (e.g. ice) changing to a gas (e.g. vapor) called?

A

Sublimation which uses latent heat

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4
Q

What is the process of a gas (e.g. vapor) changing to a liquid (e.g. water) called?

A

Condensation which releases latent heat

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5
Q

What is the process of a liquid (e.g. water) changing to a solid (e.g. ice) called?

A

Freezing which releases latent heat

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6
Q

What is the process of a gas (e.g. vapor) changing to a solid (e.g. ice) called?

A

Deposition which releases latent heat

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7
Q

Which changes in state use latent heat?

A

Melting, Evaporation & Sublimation use latent heat

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8
Q

Which changes in state release latent heat?

A

Consensation, Freezing & Deposition release latent heat

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9
Q

What do all of the changes in state involve?

A

All changes in state involve heat energy (latent heat)

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10
Q

What are clouds and what do they do?

A

Clouds are condensed water vapour which clean the atmosphere of tiny specks of dust

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11
Q

Why is cloud formation and precipitation essential?

A

Cloud formation and precipitation are essential parts of the water cycle as precipitation is the main flow of water from the atmosphere to the ground.

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12
Q

When do clouds form?

A

Clouds form when warm air cools down, which causes the water vapour in it to condense into water droplets, which gather as clouds. When the droplets get big enough, they fall as precipitation.

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13
Q

What causes the warm air to cool which leads to precipitation?

A

There are several things that can cause warm air to cool, leading to precipitation and these include:
- Other air masses
- Topography
- Convection

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14
Q

What are other air masses?

A

Other air masses can cause precipitation to occur as the warm air in the atmosphere is less dense than the cool air. As a result, when warm air meets cool air, the warm air is forced up above the cool air. It cools down as it rises. this results in frontal precipitation.

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15
Q

What is topography?

A

Topography occurs when warm air meets mountains, it’s forced to rise as the hills almost act as a barrier, causing it to cool and form clouds. This results in orographic/relief precipitation.

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16
Q

What is convection?

A

Convection occurs when the sun heats up the ground, which causes moisture on the ground to evaporate and rise up in a column of warm air. As it gets higher, it cools. This results in convective/convectional precipitation.

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17
Q

Why can’t water droplets form clouds on their own?

A

Water droplets caused by condensation are too small to form clouds on their own. For clouds to form, there have to be tiny particles of other substances (e.g. dust or soot) to act as cloud condensation nuclei/hydroscopic nuclei. They give water a surface to condense on. This encourages clouds to form, rather than allowing the moist air to disperse.

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18
Q

How do cloud formation and precipitation vary?

A

Cloud formation and precipitation can vary seasonally (e.g. in the UK there’s normally more rainfall in winter than in summer) and by location (e.g. precipitation is generally higher in the tropics tham at the poles).

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19
Q

In which form is water stored in the water cycle?

A

Water is stored in Solid, Liquid and Gas forms

20
Q

How much water does the hydrosphere contain?

A

The hydrosphere contains 1.4 sextillion litres of water

21
Q

Where is water stored on Earth?

A

Water is stored within four major physical systems - the lithosphere (land), hydrosphere (liquid water), cryosphere (frozen water - snow and ice) and in the atmosphere (air).

22
Q

What is the definition of the oceanic water store?

A

The oceans are the biggest stores of water (saline) they dominate the amount of water available with just over 97% of all of the water being found in the oceans.

23
Q

What is the definition of the cryospheric water store?

A

The cryopshere includes all of the frozen water in the Earth’s system. This means the frozen parts of the ocean, so water can be stored in glaciers, ice shelves, ice sheets, ice caps and permafrost.

24
Q

What is the definition of the terrestrial water store?

A

the terrestrial water store includes surface water, ground water, soil water & biological water, rivers and lakes are the most accessible in the terrestrial system.

25
What is the definition of the atmospheric water store?
Most of the water stored in the atmosphere is found in the gaseous state, water vapour which is a colourless and odourless gas. Atmospheric water absorbs solar energy, redistributes wateraround the globe and also removes impurities from in the air.
26
What is the biggest store of water on Earth?
Most of the water on Earth is saline water (97.4%) and it is stored in the oceans.
27
What percentage of the Earth's water is freshwater?
Only 2.5% of the Earth's water is freshwater: - 69% is frozen in the cryosphere - 30% is groundwater (water stored underground in the lithosphere). - 0.3% is liquid freshwater on the Earth's surface in lakes, rivers etc. - 0.04% is stored as water vapour in the atmosphere.
28
What must water be for humans to be able to use it?
Water must be physically and economically accessible for humans to be able to use it (e.g. groundwater is hard to access, so it may not be cost effective to extract it). As a result, only a small amount of water on the planet can be used by humans.
29
What can water change between?
Water can change between solid, liquid and gaseous forms. For water to boil or melt, it has to gain energy (e.g. from the sun). For water to condense or freeze, it has to lose energy.
30
What is the definition of sea ice?
Sea ice is frozen seawater that floats on the ocean surface it must be extremely cold to form as the salty ocean water means that it freezes at a lower temperature. It forms in both the Arctic and the Antarctic.
31
What is the definition of an iceberg?
An iceberg is ice that broke off from glaciers or shelf ice and is floating in open water. Most icebergs are near greenland and some are found in Alaska
32
What is the definition of an ice sheet?
An ice sheet is a mass of glacial land ice which extends more than 50,000 square kilometres. Important examples include the Antarctic Ice sheet and the Greenland ice sheet.
33
What is the definition of an ice shelf?
Ice shelves are floating extensions of ice that extend from glaciers grounded on land. They are found along the coasts of the two remaining ice sheets in Greenland and also Antarctica.
34
What is the definition of permafrost?
Permafrost is any ground that remains completely frozen for at least two years straight and it occura in Northern Greenland, Canada, Russia, Alaska and the Himalaya.
35
What is the definition of an ice cap?
An ice cap is a thick layer of ice and snow that covers large areas of land under 50,000 kilometres. One Ice cap covers most of Greenland and the other spans across the continent of Antarctica.
36
What is the global hydrological cycle?
The Global hydrological Cycle/The Global Water Cycle is a closed system as there are no inputs or outputs of water. It is driven by energy from the sun and the system is in dynamic equilibrium. The cycle involves water continuously being cycled between different stores.
37
What is the definition of an aquifer?
An aquifer is an underground store of water that can be used as a resource for fresh drinking water.
38
What is the definition of residence time?
Residence time refers to how much time water tends to spend in a store.
39
What is the residence time of groundwater like?
The residence time of groundwater is very long (from 2 weeks to 10,000 years) as it cannot be evaporated into the atmosphere from underground. However this depends on how far the water is underground as the residence time can vary.
40
What is the typical trend between residence time and the size of the store?
Typically some of the biggest stores of water have the longest residence times. However, there is a large variation and range in the residence times of the stores of water.
41
How does the amount of water in a store vary?
The amount of water present in each store varies over a range of scales from local (e.g. an individual hillslope) to global. The magnitude of each store depends on the amount of water flowing between them and different flows/transfers occur at a range of spatial and temporal (time) scales.
42
Which spatial and temporal factors affect evaporation and therfore impact the magnitude of the water cycle stores?
Evaporation occurs when liquid water changes state into a gas, becoming water vapour - it gains energy, normally from solar radiation. Evaporation increases the amount of water stored in the atmosphere: - the magnitude of the evaporation flow varies by location and season. If there is lots of solar radiation, a large supply of water and warm, dry, air, the amount of evaporation will be high. - If there is not much solar radiation, little available liquid water and cool air that is already nearly saturated (unable to absorb any more water vapour), evaporation will be low.
43
Which spatial and temporal factors affect condensation and therfore impact the magnitude of the water cycle stores?
1) Condensation occurs when water vapour changes state to become a liquid - it loses energy to the surroundings. It happens when air containing water vapour cools to its dew point (the temperature at which it will change from a gas to a liquid), e.g. when temperatures fall at night due to heat being lost to space. 2) Water droplets can stay in the atmosphere or flow to other subsystems, e.g. when water vapour condenses, it can form dew on leaves and other surfaces - this decreases the amount of water stored in the atmosphere. 3) the magnitude of the condensation flow depends on the amount of water vapour in the atmosphere and the temperature. For example, if there is lots of water vapour in the air and there's a large or rapid drop in temperature, condensation will be high.
44
Which spatial and temporal factors affect cryospheric processes and therfore impact the magnitude of the water cycle stores?
1) Cryospheric processes such as accumulation and ablation change the amount of water stored as ice in the cryosphere. the balance of accumulation and ablation varies with temperature. 2) During periods of global cold, inputs into the cryosphere are greater than outputs - water is transferred to it as snow, and less water is transferred away due to melting. During periods of warmer global temperatures, the magnitude of the cryosphere store reduces as losses due to melting are larger than the inputs of snow. 3) The Earth is emerging from a glacial period that reached its maximum 21000 years ago. There are still extensive stores of ice on land in Antarctica and Greenland, as well as numerous alpine glaciers. there is also a large volume of sea ice in the Arctic and Antarctica. 4) Variations in cryospheric processes happen over different timescales. As well as the changes in global temperature that occur over thousands of years, variations can also occur over sjorter timescales. For example, annual temperature flucuations mean that more snow falls in the winter than in summer.
45
Where is there less cloud coverage on Earth?
There are less clouds in areas where there are deserts e.g. Antarctica and The Sahara because they are areas of high pressure where the air is sinking and not rising to form clouds.
46
Where is there more cloud coverage on Earth?
There are lots of clouds at 60 degrees North and South of the Equator as it is an area of extreme low pressure where the air is rising to form clouds e.g. cumulonimbus.