A level Physical Geography: Water - Statistics

General Stats
  • This quiz has been taken 30 times
    25 since last reset
  • The average score is 11 of 30
Answer Stats
Hint Answer % Correct
The conversion of water to vapour Evaporation
70%
The combined effect of evaporation and transpiration Evapotranspiration
60%
The only open system in the water cycle where local factors control the throughput of water through a local store. Drainage Basin
55%
Water entering the top soil Infiltration
55%
Water is taken up by plants and is formed onto the leaf surface Transpiration
55%
When gaseous water transforms to liquid state Condensation
50%
A situation where pressure systems and weather patterns reverse in the Southern hemisphere El Nino
50%
Temporary storage as water is captured by plants, buildings and hard surfaces before reaching the soil Interception
50%
The downward seepage of water through rock under gravity Percolation
50%
Release of water in liquid state Precipitation
45%
Flow of water over the surface when the ground is saturated, frozen or impermeable Surface runoff
45%
Water availability falls below 1000m³ per person Water Scarcity
45%
When cold air meets a weather front, warm air rises above cold air which then cools and condenses, falling as rain. (Rainfall) Frontal
40%
Air is forced upwards due to the relief of an area. This air cools and condenses, falling as rain. (Rainfall) Orographic
35%
The store of water in gas state (store) Atmospheric
30%
Thermal energy from the sun causes air to rise into the atmosphere. This cools, condenses and falls as rain (Rainfall) Convectional
30%
The store of water in solid state (store) Cryospheric
30%
When 'normal' pressure systems and weather patterns intensify La Nina
30%
The flow of hot and cold water around the oceans Thermohaline Circulation
30%
The summation of all water in the seas and oceans (store) Oceanic
25%
The amount of water that could be evaporated and/or transpired from an area if there was sufficient water available Potential Evapotranspiration
25%
Precipitation (P) = Streamflow (Q) +Evapotranspiration (E) Changes in storage (S) Water Balance
25%
Where larger rivers cross several different relief and climate zones (river regime) Complex
20%
The amount of precipitation remaining after evapotranspiration Effective Rainfall
20%
Where a river experiences a period of seasonally high discharge followed by low discharge (river regime) Simple
20%
The hidden flow of water when food or other commodities are traded Virtual Water
20%
The amount of water usually available within a particular region Base flow
15%
The summation of all water on the land surface and in the subsurface (store) Terrestrial
15%
Consumption exceeds 10% of its renewable freshwater supply Water Stress
15%
Ways in which water accelerates under gravity Gravitational Potential Energy
10%
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