hydrology flooding and water quality Flashcards
3 reasons why floods occur
- excess rainfall due to cyclone activity or low-pressure systems (dunne flooding)
- locally intense rainfall (hortonian flash flooding)
- changed catchment conditions eg land cover, obstruction, development in flood plains
what are 3 predictions of climate change due to an increase in CO2 related to precipitation
- increase in global precipitation due to Clausis claperon equation that states warm air holds more water (7% per K)
- strong spatial and temporal variation meaning increase in tropics and decreases in arid.
- a higher maximum daily precipitation leading to more flooding
3 ways climate change will impact flooding
- higher probability of floods
- change in ENSO more intense periods of rainfall
- rise in sea level will cause bigger tides leading to compound risk of flooding
what is a flood risk
combination of exposure and probability, flood risk has increased due to population growth and development which has increased exposure
how can increasing Warragamba dam wall affect the water balance
might increase flooding on back end therefore shifted issue from downstream to upstream flooding. what is really needed is to have capacity for flooding downstream (storage)
what 5 things describe a flood
- frequency
- duration
- rates of change ie slope of limbs
- magnitude
- flow history
what is the flow duration curve and how do you read the shape
flow probability of the occurrence of a flood level (100% being always) (1% being rare)
the flood behaviour can be measured by the shape of the curve
the flatter the curve the more regular the flows
the steeper the curve the more variable
how can flood duration curve measure the flow regime
flow regime is flood timing duration and magnitiude, the before and after of the flood duration cruve and measure these effects of flow regulation
Q01 =
1% chance of occurring in a year
1:100 reaccurance interval
how to predict higher ARI
to get 1:100- 1:1500 data limited used linear regression etc using distributions
what is river routing and what are the two types
river routing predicts the movement of water through the channel and how its impacted by storage
- hydrological
- hydrualic (difficult)
what is attenuation
reduction of magnitude/height of flood peak as it makes downstream ie depression AND spread
what is translation
change in time of flood peak as it moves downstream (shift)
what is a linear reservoir
move runoff through a series of storages which delays flow as each store has a different retention time
what is the difference between the linear storage model and the Muskingum equation
linear storage is only a function of outflow whereas Muskingum is a function of inflow and outflow