How does deforestation affect a drainage basin? Example?
Amazon
What is an example of over abstraction?
Aral Sea
What are the human impacts on drainage basins
Over-abstraction - eg Thames, Murray Darling, Mexico City
Deforestation - Amazon. ; removes vegetation which reduces interception and therefore increases infiltration and surface runoff.
Changing land use - urbanisation increases interception and stops infiltration which means more surface runoff.
Reservoirs - interrupt natural flow of water; estimated 7% more water is evaporated from reservoirs than used by people.
What are river regimes
The pattern of flow of a river throughout the year.
Complex = larger rivers that cross several relief and climate zones, therefore they experience the effects of different seasonal climatic events. - Amazon, Yukon
Simple = river experiences a period of seasonally high discharge, followed by low discharge; typical of rivers where inputs depend on glacial meltwater or seasonal storms.
What are the characteristics of the river Yukon
Characteristics of the Amazon river
Murray darling characteristics
Influences:
- seasonal sub tropical climate; monsoon climate in northern tributaries of Queensland = increases discharge during rainy seasons
Why do storm hydrographs vary?
Reflects localised and contemporary characteristics of the drainage basin
- every change in land use and previous period of weather will determine timing and height of the peak
What are physical factors that affect hydrographs?
What are human factors that affect hydrographs?
How do hydrographs in rural areas and urban areas vary?
Urban: high levels of impermeable surfaces = shorter lag time and higher peak flow - due to more runoff
• steel rising limb
Rural: more permeable surfaces = longer lag time as water takes longer to reach river.
• gradual rising limb
What is meteorological drought?
Due to a rainfall deficit which causes a loss of soil moisture and the supply of irrigation water declines.
What is hydrological drought?
Caused by a stream flow deficit and leads to reduced storage in lakes and reservoirs, less water for urban supply and power, and threats to wetlands and wildlife habitats.
Describe a high and low pressure system
Warm air rises and condenses in the atmosphere to form clouds = rainfall - low pressure
Cold air sinks = no clouds = no rain
- high pressure.
What are the 3 cells called?
Hadley cell = 0 - 30 degrees
Ferrell cell = 30 - 60 degrees
Polar cell = 60 - 90 degrees
What are the features of the polar cell?
= cool air sinks at 90* due to low insolation. Coriolis effect causes cold air to move south along the surface - these are called the polar winds. These meet the warm westerlies and cause them to rise = low pressure at 60*
What are the features of the Ferrell cell?
At 30, the sinking air from the Hadley cell forms high pressure, the warm surface air moves from high to low pressure = westerlies. When these winds meet cold air from polar cell, it rises, cools and condenses into clouds at 60
What are the features of the Hadley cell?
High levels of solar insolation at the equator causes air to rise, forming a low pressure. = clouds and rain. Due to Coriolis, this air moves north.
It sinks at 30* as it is now cool, and causes high pressure.
Surface air moves from areas of high to low pressure - these are called trade winds in the Hadley cell.
Describe a normal year
Pacific winds circulate the walker cell. Winds travel west taking warm surface water with them. Warm moist air rises over Indonesia/Australia creating low pressure and heavy rain. The air then circulates east in the upper atmosphere, sinking into cooler high pressure over South America = dry conditions from the deserts.
Describe an El Niño year
Warmer waters in the eastern pacific cause low pressure = draws westerly winds from pacific. Warm, moist air rises creating heavy rainfall over South America. This then circulates west in the upper atmosphere and descends over Australia creating high pressure and leading to drought.
Describe a La Niña year
Low pressure over west pacific becomes lower and high pressure over the eastern pacific becomes higher. As a result, easterly trade winds become more intense and even more warm water is taken west. This causes flooding in Australia and Indonesia
What are the physical causes of drought in the Sahel?
•Almost all rainfall - 85% - occurs in summer
•unusually warm waters cause more upwelling = more rainfall over Atlantic rather than over land.
•Albedo effect = the reflectivity of the surface causes solar energy to reflect back into the atmosphere, increasing evaporation and reducing the potential for rainfall. - exacerbated by deforestation
What are the human causes of drought in the Sahel
•Overgrazing of nomadic tribes and deforestation cause land degradation and desertification.
•deforestation also worsens the Albedo effect - less trees = more reflective land exposed. Also leads to less moisture getting into atmosphere by transpiration.
•population growth = more demand
•unsustainable water extraction
•civil conflicts
When was storm Desmond?
December 2015