4 - precipitation and excess runoff within the water cycle ✅ Flashcards

1
Q

what causes clouds

A

air uplift and condensation occurs and clouds form

OROGRAPHIC, FRONTAL and CONVECTION mechanisms create this

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2
Q

what are the effects of deforestation

A
  • increased flood risk
  • infiltration rate into the soil is 67x higher under trees compared to grassland
  • devastating effects of Cumbria 2009 and Boscastle 2004 were caused by excess overland flow generated on deforested hills
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3
Q

what is the effect of glaciers

A
  • mountain snow fields and glaciers act as natural reservoirs
  • they store precipitation from the cool season (when precipitation falls and forms snow packs) until the warm season when most or all snow packs melt and release water into rivers
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4
Q

what is the bergeron findeisen process

A
  • clouds at high altitude ( >0 degrees) have water droplets and ice crystals
  • ice crystals grow rapidly at the expense of the water droplets due to rapid flux of water vapour from droplets towards ice crystals
  • the ice crystals fracture as they are jostled by fast high altitude air currents.
  • hexagonal ice shapes develop with larger surface areas.
  • more water vapour condenses around the larger snowflake shapes, accelerating growth further
  • eventually hexagonal snowflakes become too large and fall under gravity, warming as they melt to produce rain
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5
Q

what evidence is there for and against the bergeron-findeisen process

A

FOR::
- in the UK precipitation is often derived from clouds with temperatures below -5 degrees
- cloud seeding with dry ice can successfully generate rainfall

AGAINST::
- however this process cannot explain rainfall formation in the warm tropics

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6
Q

what is the collision process

A
  • super sized condensation nuclei (eg large sea salt particles) provide ‘seeds’ around which water droplets form
  • they are larger and heavier than normal sized droplets
  • larger droplets fall and collide with smaller droplets by sweeping them in their wake and absorbing them
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7
Q

what evidence is there for the collision process (3)

A
  • Langmuir carried out experimental work to produce the theory
  • he argued that higher terminal velocity of large droplets allows them to overtake and absorb many smaller droplets causing rapid fusion and raindrop growth
  • unexpected downpours and flash floods in arid areas demonstrate how high numbers of large raindrops can be generated quickly
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8
Q

what physical characteristics contribute to flooding (10)

A
  • vegetation
  • soil type
  • drainage area
  • basin shape
  • elevation
  • topography, especially the slope of the land
  • drainage network patterns
  • ponds, lakes, reservoirs, sinks, etc in the basin which prevent or delay runoff from continuing downstream
  • prolonged precipitation and intense storms
  • snowmelt
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9
Q

what is the main contributor to excess runoff and causes

A

STORMS and INTENSE RAINFALL

causes are usually frontal rainfall in winter and convectional events in summer

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10
Q

what can hydrographs reveal about the contribution of snowmelt to excess runoff to rivers

A

large peaks are the melting of snow (but storms can also contribute)

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11
Q

how might climate change impact snow melt in the future (4)

A
  • recent warming of global climate has reduced accumulation and increased ablation (output) levels
  • large volumes of summer melt water and a reduction in winter accumulation has led to lower storage levels in global ice cycle sheets and glaciers
  • impact on drainage basins across the world is serious - seasonal river levels dropping due to a lack of meltwater from individual mountain glaciers
  • hill slope changes occur as individual glaciers melt completely, depositing their encased material as moraines
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12
Q

what are monsoons

A

a seasonal change in the strongest, or prevailing winds of a region

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13
Q

how do monsoons work

A

Southeast Asia experiences two monsoon seasons

the first brings in moisture filled clouds from the Indian Ocean

the second brings cooler, dry air from eastern Asia and the Himalayan region

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14
Q

how could future climate change affect monsoon rainfall

A
  • climate change could affect global precipitation patterns considerably:
    increase in precipitation from increased evaporation, regular rainfall could reduced
  • monsoon rainfall is reducing in duration, affects India/China who rely on it for drinking and food growing
  • a complete stop of the monsoon rains in central southern china and northern india:
    generated by sharp heat gradients in the atmosphere where warm land meets cool ocean, blocking solar energy = aerosols cool coastal atmosphere, sap monsoons strength)
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15
Q

what is a condensation nuclei

A

condensation results in cloud formation but needs a surface to occur upon

dust and other microscopic solids in the atmosphere act as condensation nuclei

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16
Q

what is the feeder seeder mechanism

A

a process that increases levels of orographic rainfall

water droplets/ice particles from high altitude seeder clouds fall through lower level stratus clouds that are commonly formed from orographic rainfall

these seeder clouds then contain more water droplets increasing the rate of precipitation

17
Q

how does urbanisation increase the magnitude and frequency of floods

A
  • creation of highly impermeable surfaces eg roads, roofs, pavements
  • smooth surfaces served with dense network of drains, sewers increase drainage density
  • natural river channels often constricted by bridge supports/riverside facilities
18
Q

what is the hydrological response to removal of trees/vegetation

A
  • decreased evapotranspiration and interception
  • increased stream sedimentation
19
Q

what is the hydrological response of house, street and culverts construction (3)

A
  • decreased infiltration
  • increased storm flows
  • decreased base flows during dry periods
20
Q

what is the hydrological response of complete development of residential, commercial and industrial areas

A

decreased porosity = reduces time of runoff concentration = increases peak discharges and compresses the time distribution of the flow

greatly increased volume of runoff and flood damage potential

21
Q

what is the hydrological response of construction of storm drains and channel improvements (2)

A
  • local relief from flooding
  • concentration of floodwaters may aggravate flood problems downstream
22
Q

human causes of flooding in the Ganges river basin

A

DEFORESTATION - population increase in Nepal = greater demand for food, fuel and building materials reducing interception and increases run off = significant soil erosion and sedimentation of high % of river channels

URBANISATION - of flood plane due to industrialisation and population increase has increased runoff and magnitude/frequency of floods

POORLY THOUGHT BUILDING OF DAMS - in India increased sedimentation problem in Bangladesh

POORLY MAINTAINED EMBANKMENTS - (Levees) leak and collapse in times of high discharge

23
Q

how can drainage basins be managed (7)

A
  • afforestation, reseeding sparsely vegetated areas to increase evaporative losses
  • mechanical land treatment of slopes eg contour ploughing/terracing to reduce runoff coefficient
  • protection of existing vegetation from wild fires, clear cutting of forests
  • dredging to increase channel capacity
  • construction of storm water and sediment holding areas eg reservoirs
  • preservation of natural water detention zones
  • hard engineering options to protect land eg artificial levees