Causes of floods Make a copy of the column headings below. Causes of floods Rainfall Snow and ice melt Tidal influences Other (natural causes) Put the causes into the correct column(s). Some can go in more than one column. Affects mainly mountainous and high latitude areas. Affects the lower course of a river. Affects mainly the upper course of a river. Occurs infrequently. Is due to large earthquakes or tsunamis. Could also be caused by a landslide. Long periods of heavy rain. High intensity rainfall exceeds the infiltration capacity of the soil. High antecedent rainfall can leave the soil saturated. In some areas, 75% of the year’s river flow can occur when temperatures suddenly rise. Can affect all parts of a river. Presence of downstream ice can act as a dam and force upstream water to rise. Occurs more frequently after large areas have been covered recently by impermeable materials. © www.teachitgeography.co.uk 2012 17509 Page 1 of 4 Causes of floods Flood-intensifying conditions Write brief notes explaining how each of the following factors may increase the size of a flood. Urbanisation and urban growth Bridges, dams and other obstructions Changes in vegetation cover River engineering works e.g. levees Floodplain developments Small drainage basins Steep slopes Global warming © www.teachitgeography.co.uk 2012 17509 Causes of floods Teaching notes Students could be asked to research a case study for each cause, presenting their research to the class. Some possible hyperlinked examples are given below. Causes of floods: answers Rainfall Other (natural causes) Snow and ice melt Tidal influences Long periods of heavy rain, e.g. Carlisle 2005. Affects mainly mountainous and high latitude areas. Affects the lower course of a river, e.g. Boscastle 2004. High intensity rain exceeds the infiltration capacity of the soil, e.g. North-east England and Scotland 2011. Affects mainly the upper course of a river. High antecedent rainfall can leave the soil saturated, e.g. Boscastle 2004. Can affect all parts of a river. Occurs more frequently after large areas have been covered recently by impermeable materials. In some areas, 75% of the year’s river flow can occur when temperatures suddenly rise. Occurs infrequently. Is due to large earthquakes or tsunamis, e.g. Japan 2011. Could also be caused by a landslide, e.g. Hunza Valley 2010. Presence of downstream ice can act as a dam and force upstream water to rise, e.g. Red River flood 2011. © www.teachitgeography.co.uk 2012 17509 Causes of floods Flood-intensifying conditions: answers Urbanisation and urban growth Bridges, dams and other obstructions Changes in vegetation cover The increase in impermeable surfaces and increase in drainage density (gutters and sewers, etc.) leads to an increase in flood frequency and in the degree of flooding. These may act as temporary obstructions causing the water to ‘pond up’. This may increase pressure on the bridge and eventually cause the collapse of the bridge. Downstream ice can also act as a temporary dam causing the upstream water to rise. The removal of vegetation leads to less interception of water, more overland flow and an increased risk of flooding. In contrast, the planting of vegetation can decrease the probability of flooding and/or the size of peak discharge. River engineering works e.g. levees Levees protect floodplains from a certain size of flood (the ‘50 year flood’, for example) but they do not offer protection from larger floods. They cause local people to become complacent as to the flood risk. Floodplain developments Any development on the floodplains (factories, roads, housing and car parks, etc.) increases the amount of impermeable surface. This increases both the amount of surface runoff and reduces the lag time, thereby increasing the risk of flooding. It may cause other locations to flood, and floodwaters to be deeper. Small drainage basins Small drainage basins respond quickly to high rainfall events causing ‘flash floods’ and allowing less time for taking action / response. Steep slopes Water flow is faster on steep slopes. The time lag between maximum rainfall and the flood’s peak discharge is reduced. Global warming Some places may become wetter and so flooding may be more common. Other places however, may become drier and so flooding may possibly be reduced. Some places may become drier in summer (drought conditions) but wetter in winter, increasing the risk of flooding. © www.teachitgeography.co.uk 2012 17509