5.2 + 5.3 Flashcards

1
Q

describe orographic rainfall

A
  • air is forced to rise over a barrier such as a mountain
  • due to cooler temperatures (resulting from higher altitudes) the water vapour condenses into clouds
  • heavy rain on the highlands, which empties the clouds and leaves a rain shadow down the slope
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2
Q

describe cyclonic (frontal) rainfall

A
  • warm and cold air move towards each other
  • as warmer air is less dense it rises over the colder denser air
  • as it rises it cools and condenses, the extra potential energy also means it looses the ability to store the vapour so it precipitates
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3
Q

describe convectional rainfall

A
  • warm air rises vertically up over cool air
  • warm air cools due to increased altitude and condenses
  • as more vapour builds up, it rains
  • as the air cools down it begins to descend and is replaced by warmer air
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4
Q

what conditions are needed for rainfall

A
  • air cooled to saturation point with relative humidity near 100%
  • condensation nuclei, such as dust particles to facilitate the growth of droplets in clouds
  • temperature below the “dew point”, temperature at which dew forms, a measure of atmospheric moisture
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5
Q

which water store has the longest residence time

A

crysphere- 15,000 years

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6
Q

what is the largest store of water and what is its percentage. What is its residence time ?

A

Oceans, 96.9%

residence time: 3600 years

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7
Q

what impacts the drainage basin hydroglogical system

A

1) the volime of percipitation direct impact on discharge, the higher the amoun the lower the variability
2) Type of percipitation (rain, snow or hail) snow can act as a temporary store and large fluxes of water can be released after a thaw, resulting in rapid melting
3) seasonality- some climates such as the mediteranean, a monsoon or continued have strong seasonal patters of percipiration which have major impact on the physical processes operating in the drainage basin system
4) percipiration intensity - If percipitation of e.g. rain is intense then it is less likely that it will infiltrate the soil as it will be laready saturated
5) variability:
- secular variability, long term for example as a resilt of climae change
- periodic variability, happens in an annual seasonal monthly diuralcontext
- stochaic variability, results from random factors, for example the localisation of a thunder storm within a basin
6) distribution of percipitation form basin (mainly for large basins e.g. nile) were bateries start in different climatic zones. At a local scale and shorter time scales,the location of a thunerstorm can have a large impact temporarily as inputs will vary

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8
Q

list which land types intercept most, starting from most interception to least

A
  • coniferous
  • decidious, summer + spring
  • decidious, autumn + winter
  • arable farmland
  • deforested
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9
Q

what atmospheric factors contribute to high levels of intercpetion

A
  • intermitent percipiration
  • sunlight
  • not windy conditions
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10
Q

what increases infiltration rates

A
  • many trees with many roots
  • porous and sandy soil
  • low water table
  • porous/permeable rocks
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11
Q

what increases surface run-off

A
  • soil saturation
  • imperbeable rocks
  • clay rather than sany soil
  • urbanisation
  • steeper slopes
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12
Q

wjat increases rates of soil throughflow

A
  • sandy soil
  • saturated soil
  • premiale rock
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13
Q

define evapotransipration

A

total amount of moisture removed from drainage basin by process of evaporation and transpiration

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14
Q

what factors affect evapotranspiration and how do they affect it

A
  • temperature: icreases rate of evaporation, evaporation and temperature increases with sunshine hours
    wind: will increase the rate of evaporation by reducing the relative humidity
  • vegitation cover: transpiration increases proportionally with vegitaiton cover which depends on the season and type of vegitation. Low albedo vegitation, such as a dark forest will absorb more solar radiation which increase transpiration
  • soil moisture content: determines the volume of water available for transpiration. It is dependandt on soil and rock permeability
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15
Q

define Channel flow

A

water that has collected to flow in a rivulet, stream or river and is another output from the drainage basin system

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16
Q

define discharcharge

A
  • discharge of a river is the volume of water passing a specific gorging station per unit time and is measured in cubic metres per seceond, cumecs
  • It is dependant on: percipitation flowing in the channel, contributions from drainage basin stores via surface run off, throughflow or groundwater flow
17
Q

what are the human disruptions in the drainage basin

A
cloud seeding
dam construction
urbanisation
ground water extraction
arable and pastoral farming
18
Q

what is cloud seeding

A

expulsion of particulates from power stations such as hydrosopic nuclei which provide space for water milecules to attatch onto to form clouds

19
Q

how does dam construction intefere with drainage basin

A
  • increase surface storage

- exposed water increases evaporation

20
Q

how do aaquifiers interfere with drainage basin

A
  • water is taken from ground
  • goundwater stores decrease
  • lowers the groundwater flow