5.1 Flashcards

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1
Q

What are fluxes in the global hydrological cycle

A

Fluxes measure the rate of flows between the stores

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2
Q

What are stores in the hydrological cycles

A

Stores are reservoirs where water is held e.g oceans

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3
Q

What is green water

A

Green water is water stored in the soil and vegetation ( invisible)

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4
Q

What is blue water

A

Blue water is water stored in rivers, stream lakes and groundwater in liquid form ( visible part of hydrological cycle)

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5
Q

How does water exist in the atmosphere

A

Water exists largely as vapour in the atmosphere, with the carrying capacity directly linked to temperature.

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6
Q

Where is water stored on land

A

On land water is stored in rivers, streams,lakes and groundwater in liquid form. It is often known as blue water. Water can be stored in vegetation after interception or beneath the surface in the soil . This type of water is known as green water

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7
Q

What is water stored as in the cryosphere

A

In the cryosphere water is largely found in a solid statement, with some in liquid form a s meltwater and lakes

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8
Q

How is the vast majority of water stored in oceans

A

In oceans the vast majority of water is stored in liquid form, with only a minute fraction as icebergs

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9
Q

What are the significant stores in the global hydrological cycle from smallest to largest

A
  • Oceans are by far the largest stores of water as they contain an estimated 96.5-97 percent of the worlds total water
  • The next largest store occur in the cryosphere which contain 1.9 percent of water
  • The next largest store is groundwater which contains 1.1% of global water
  • After that the next largest store is rivers and lakes which store 0,01 % of water
  • The next largest store is soil moisture which stores 0.01%
  • Atmospheric moisture is next after that storing 0.001 % of water
  • Biological water ( biosphere is then last storing 0.0001 % of water
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10
Q

What type of system is the global hydrological cycle

A

The global hydrological cycle is a closed system driven by solar energy and gravitational potential energy

  • In the closed system there is a fixed amount of water in the earth and atmosphere ( estimated at 1385 million km3)
  • A closed system does not have any external inputs or outputs so this volume of water is constant and finite
  • Water can exist in different states within the system and the proportions held in each of the states can vary for both physical and human reasons
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11
Q

What are processes in the global hydrological cycle

A

Processes are the physical mechanisms which drive the fluxes of water between the stores

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12
Q

What are the levels of fluxes between the atmosphere,oceans and land

A
Ocean to atmosphere :413 10^3km3 
Atmosphere to ocean:373 10^3km3
Land to atmosphere =73 10^3km3;
Atmosphere to land: 113 10^3km3
Transfer in atmosphere: 40 10^3km3
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13
Q

What is the global water budget

A

The global water budget is the annual balance of water flows and size of water stores

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14
Q

Why is there a lack of fresh water available to humans

A
  • In the earths finite amount of water ( due to it being a closed system) only a small percentage is accessible freshwater (only 0.084% of total water)
  • This is due to the large volumes in the salinous oceans (96.5%) and due to the volumes locked in glaciers , ice caps and frozen permafrost
  • The location of the accessible freshwater means there is less available for humans, as large volumes are stored in locations remote from large population centres ( e.g lake Baikal in sparsely populated eastern Russia)
  • Residence times are another factor affecting freshwater available for humans. Some of the largest freshwater stocks (e.g the major ice sheets in Antarctica and Greenland )store water as ice for very long periods ( up to 15,000 years according to ice core data).This means that water availability is reduced in some parts of the world for humans
  • Another reason why there is a lack of freshwater available for humans is because stores with longer residence times are more likely to become polluted due to their increase in time in situ which means they are not available for humans
  • One further reason why there is a lack of freshwater available for humans is due to the fact that fossil water stores( which occur as a result of pluvial periods ) (Lake Vostok , Antarctica)are not renewable and are not reachable for general human use, reducing the amount available for humans .
  • Another reason why there is a lack of freshwater available for humans a is due to population rise. Population rise is having an affect on both the drinkability of Water due to pollution and climate change. It is also causing increased consumption of water and therefore increasing demand of already waining supplies of freshwater , causing problems with supply
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15
Q

What are the different percentages for freshwater stores

A
  • 2.5% of water is freshwater
  • Only 1.2% of freshwater is accessible surface water
  • 68% of this is ground ice and permafrost, with the rest in more accessible forms such as soil moisture and rivers and lakes
  • In total only 0.084% of total water is accessible freshwater
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16
Q

What are the inputs to the drainage basin system

A

Precipitation- all ways that moisture comes out of the atmosphere

17
Q

What are outputs from the drainage basin system

A
  • Evaporation ~ water turning into vapour
  • Transpiration~ evaporation from plant leaves
  • River discharge~ the flow from rivers into water stores
18
Q

What are the stores in the drainage basin system

A

Interception- when precipitation lands and is temporarily stored on vegetation
Vegetation-water taken up by plants
Surface storage- water in depressions in the land
Groundwater storage- Water stored in the ground in soil moisture or the water table
Aquifers- porous rocks that store water
Channel storage- Water that is held in a river channel

19
Q

What are the transfers in the drainage basin system

A

-Surface run off-Water flowing over the land
-Through fall- water dripping from vegetation
-Stem flow-Water running down a plants stem
-Infiltration-Water soaking into the soil
-Percolation-Water seeping from soil into rocks and the water table
-Through flow-water flowing down through the soil
-Groundwater flow-water flowing below the water table
-Baseflow-Water that flows from groundwater into channels
-Interflow-water flowing through the rock above the water table
Channel flow - water flowing in a river

20
Q

What are three of the main natural factors influencing the drainage basin

A

The amount of precipitation-