Optional Theme - Freshwater Flashcards
Drainage divide
Also known as WATERSHED, it is the line defining the boundary of a river drainage basin separating it from adjacent basins
Interception
- The capture of raindrops by plant cover, which prevents direct contact with the soil.
- If rain is prolonged, the retaining capacity of leaves will be exceeded +water will drop to ground (THROUGHFALL)
- Some will trickle along branches + down stems / trunks (STEMFLOW)
- Water retained on leaves later evaporates
Evapotranspiration
The loss of water from vegetation and water surfaces to the atmosphere
Potential evapotranspiration
The rate of water loss from an area if there were no shortage of water
How does potential evapotranspiration vary?
- In Atbara (Sudan) potential evapotranspiration is 6,250mm p/a (High rates recorded in deserts)
- Rates much lower in rainforests due to high humidity (500-750mm)
- Lower in cold climates also e.g London (330mm p/a)
Why are evapotranspiration rates in Egypt less than 250mm p/a?
- Egypt’s annual rainfall is less than 250mm
- If Egypt received more rainfall (e.g.2000mm), the evapotranspiration rate would increase due to very high temps.
- Thus if there were no water shortage in Egypt, potential evapotranspiration could be as high as 2000mm p/a
What is eustatic change?
Eustatic change refers to a global change in sea level.
What is isostatic adjustment (or isostacy)?
The level of the land varies in relation to the sea. Land may rise as a result of tectonic uplift or the removal of an ice sheet. The change in the level of the land relative to the level of the sea is know as isostatic adjustment.
Examples of countries experiencing isostatic adjustment
Parts of Scandinavia and Canada are continuing to rise at rates of up to 20mm a year
What is the Steric effect?
seawater expands with higher temperatures. Thus, even if ice sheets and ice caps did not melt, sea levels would rise in a warmer world.
Infiltration capacity
The amount of moisture that a soil can hold
Infiltration rate
The speed at which water can enter the soil
Percolation
Percolation refers to water moving deep into groundwater zone
Overland runoff
Overland runoff occurs when precipitation intensity exceeds the infiltration rate, or when the infiltration capacity is reached and the soil is saturated
What is the zone of aeration?
The zone of aeration is a transitional zone in which water is passed upwards or downwards through the soil
What factors determine the moisture of soil?
- porosity (the amount of pore spaces in soil)
- permeability (the ability to transmit water)
What is through flow?
Throughflow refers to water flowing through soil in natural pipes and percolates (lines of concentrated water flow between soil horizons)
What is base flow?
Baseflow refers to the movement of water within the zone of aeration
What is interflow?
Interflow refers to the movement of water within the zone of saturation
Why is the soil moisture deficit low during late winter and early spring in London and Madrid?
- high levels of precipitation
- limited EVT
What is soil moisture recharge?
Soil moisture recharge occurs when precipitation exceeds potential EVT
What is soil moisture surplus?
Soil moisture surplus is the period when soil is saturated and water cannot enter, and so flows over surface
What is soil moisture utilisation
Soil moisture utilisation is the process by which water is drawn to the surface through capillary action and may be used by plants or evaporated
Discharge
The volume of water passing a given point over a set time
Why do steeper slopes lead to higher velocities?
Influence of gravity
Which river variables increase downstream ?
Discharge, width, depth, velocity
Does channel roughness increase or decrease downstream?
Channel roughness decreases
How does friction create an uneven distribution of velocity in a stream?
- water closest to the bed + bank travels slowest
- water nearest centre travels fastest
How is the shape of the river channel determined by the type of rock?
- solid rock allows only slow changes
- alluvium allows rapid changes
- silt + clay produce steep, deep, narrow valleys
- sand + gravel promote wide, shallow channels
What is the river regime?
The river regime is the seasonal variation in the flow of a river
What does a storm / flood hydrograph show?
It measures the speed at which rain falling on a drainage basin reaches the river channel