ESCI409 Floods
Floods are the most widely experienced catastrophic geologic hazard
Flooding in NH is the most common and most expensive geologic hazard
Flood = river stage that is “too” high
When the watershed delivers more water than the river can hold, the excess water spills out of the channel and onto the floodplain
River stage (aka gauge height) = how high the water is at a specific location
Bankfull stage
How high the water needs to be to fill the river to its banks
Flood occurs when stage exceeds bankfull
Damage worsens as stage increases
Horizontal flood extent increases as stage rises
Bankfull discharge
How much discharge Is needed to fill a river to its banks
Most rivers are big enough to hold their typical flor
If too small, will erode bed + banks and increase cross-sectional area
If too big, then sediment will deposit within the channel and decrease cross-sectional area
Flood stage categories
Below flood – normal levels
Action –
Minor
Moderate
Major
River flooding factors
Excessive rainfall
Snowmelt
Severe storms
Hazardous blocking of stream channel (increases stage without change in discharge)
Trees
Rock avalanches
Stream discharge fluctuates over time
Extreme event frequency
Magnitude of extreme events is inversely proportional to how often they occur ( higher magnitude = lower frequency)
Magnitude = 1/frequency
Typically assume that historical record (frequency of past events) is useful in predicting the future (probability of future events)
Flood recurrence interval: R=(N+1)/M
N = number of years, M – ranking
Probability of occurrence = P=1/R
Human impacts on flooding
Climate change
Watershed development
River corridor development
Annual peak flows are changing for many rivers – higher peaks are becoming much more common
Human impacts change floodplains by changing land use and climate
Buildings and fill replace water volume, raise stream height
Infrastructure increases costs/financial impact when floods occur
Storm drains: built to rapidly deliver storm water to streams, which increases stream height
Urbanization causes floods by routing water more quickly to streams
Flood control: Levees
Raised banks along a stream channel
Causes increased flow further down the stream and therefore worsened floods
Flood control: Dams
Store river water, delaying arrival downstream
Also trap sediment – can create scour downstream
Flood control: retention ponds
Trap surface water and sediments before they get to water
Delays arrival of water
Water may also be lost to infiltration and evaporation
Netherlands “Room for the River” project – began in 2007 after severe river flood damage in the 1990s, approx 2.3bil euros cost
Fun Fact – Weeks Act in 1911 permits federal govt to purchase private land to protect headlands of rivers in the eastern US