Floods%20and%20disturbances%20in%20aquatic%20communities - PowerPoint PPT Presentation

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Floods%20and%20disturbances%20in%20aquatic%20communities

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Describe the effects of floods, particularly on aquatic communities ... Disturbance (Grime and Connell): rainforests, various vegetation types, coral reefs ... – PowerPoint PPT presentation

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Title: Floods%20and%20disturbances%20in%20aquatic%20communities


1
  • Floods and disturbances in aquatic communities
  • Outcomes
  • Discuss the practices that exacerbate floods, and
    flood control measures
  • Describe the effects of floods, particularly on
    aquatic communities
  • Use disturbance ecology as a theoretical
    framework to assess the extent and severity of a
    disturbance

2
Floods as catastrophes
  • Variations in stream flow lead to floods and
    droughts.
  • Floods are natural earth processes, amongst
    earthquakes, volcanoes, fires, drought etc.
  • Why do we see an increase in flood incidence?
  • Less mortality, but more damage due to
  • changes in land use patterns (overconfidence in
    flood control)
  • urbanisation
  • overpopulation
  • changes in magnitude and frequency (climate
    Bangladesh)

3
  • Definitions and terms
  • River discharge is simply a measure of the amount
    of water moving down a channel past a given point
    per unit time (m3 s-1). It is related to stream
    width, depth, current velocity and roughness of
    the substrate.
  • Flood- when stream flow exceeds bankfull
    discharge and water spreads out onto adjacent
    land or floodplain
  • During rainfall events, flood hydrographs are
    used to measure base flow, the time taken to
    reach peak discharge, and the time taken to
    achieve base flow when rainfall ceases.
  • Floodplain- should not be considered as dry land
    that is damaged, but a natural extension of the
    riverbed that is less frequently used.

4
  • Causes
  • INCREASE IN STREAM DISCHARGE (proximal cause)
  • snow melt
  • arterial drainage, waterway improvement both act
    to reduce time of rise to peak discharge.
  • Increase in rainfall
  • Major features of floods
  • the flood hydrograph
  • relationship between time and flood severity
  • overhead
  • Response time related to
  • catchment size
  • catchment shape
  • gradient
  • vegetation
  • soil and permeability

5
Floods as disturbances in aquatic systems
  • What is a disturbance?
  • A relatively discrete event that in time that is
    characterised by a frequency, severity and
    intensity that lies outside a predictable range
    for the system (Resh et al 1988)
  • focuses on physical phenomenon
  • Any relatively discrete event in time that
    through its frequency, severity or intensity lies
    outside a predictable range for the system, and
    that removes organisms and opens up space or
    other resources that can be utilised by
    individuals of the same or different species
    (Townsend 1989)
  • focuses on physical and biological
  • Intermediate Disturbance Hypothesis

6
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7
  • Factors affecting species richness/diversity over
    large spatio-temporal scales
  • Time
  • Environment
  • favourability (mean conditions)
  • stability (variance in conditions, little
    fluctuation) e.g. stable climate, Abysal ocean
    depths
  • Disturbance (Grime and Connell) rainforests,
    various vegetation types, coral reefs
  • Spatial structural heterogeneity
  • Area
  • Productivity
  • Competition/Predation
  • (Further info Chapter 8 of Giller Community
    Structure and the Niche, available in library)

8
The disturbance regime is influenced by a number
of factors
  • Magnitude. The intensity or strength of the
    disturbing force, it consists of two main
    components
  • Intensity- a measure of the strength of the
    disturbing force
  • Severity- a measure of the damage caused
  • The physiological and morphological
    characteristics of organisms
  • Frequency. Number of disturbances per unit
    time. Separate terms are used for the average
    frequency of disturbance at the local and the
    regional spatial scales.
  • Random point frequency
  • Regional frequency
  • Different types of rivers have different
    frequencies of flood

9
  • The disturbance regime- contd
  • Predictability (mentioned in definition) results
    from three main processes
  • events that occur with a constant probability
    e.g. snow melt, winter rain
  • predictable cycles in climate or weather (storms,
    temperature, rain, El Nino, glacial periods)
  • biological processes with predictable cycles e.g.
    production/ accumulation of biomass
  • predicatability in space (upper vs lower river)
  • If a flood is very predictable, it may not be a
    disturbance!
  • Areal extent.
  • The absolute and relative size of the disturbed
    area, and the shape of the disturbed area, have
    an important effect on recolonisation.
  • E.g. hurricane vs thunderstorm, climate and
    catchment
  • Larger scale disturbances are rarer in
    occurrence.

10
Effects of floods on physical system
  • There are a number of beneficial aspects for the
    ecology of both the river and lowland system
    (Giller 1996)
  • Nutrient and energy transfer
  • Provision of nursery areas for fish
  • Fertilisation of the floodplain
  • Creation and maintenance of specialised habitats
  • Creation of patchiness (e.g. the Amazon lowland
    forest).
  • Substrate and o.m. in riffle areas (shallow
    fast-flowing and steep) dislodged
  • severe flooding scours the stream bed removing
    vegetation/animals
  • removal of sediments to depths between 20cm and
    2m
  • In pools and glides (slow and low slope) large
    amounts of sediment redeposited

11
Effects on biota
  • Case and netbuilding, locomotion, territoriality,
    respiration,
  • Dislodgement and downstream transport
  • Mortality
  • Impact may be related to life stage
    (..predictability..)
  • e.g. greatest impact on fish is on eggs (buried
    in substrate) or fry, and loss of habitat or food
    resources
  • Usually, recovery can take in the region of
    months
  • Catastrophic floods
  • Yoshino, Japan (typhoon) 1959 32g/ 0.25m2
    1964 0.5g/ 0.25m2
  • see overheads

12
Recovery and resistance to floods
  • Adaptations to strong flow
  • life-history strategies (and timing of flood)
  • recolonisation fastest when areal extent small
    at the usual time of year
  • upstream areas, flight from downstream areas
  • REFUGIA
  • Flood plain (especially for fish, in lowland
    floodplains)
  • Hyporheic zone
  • Flow refugia (see handout)

13
  • (modern) Flood Alleviation
  • Realises that physical simplification of river
    system makes catchment more vulnerable to flood
    (WHY?), and less likely to recover (WHY?)
  • use the floodplain to dissipate energy
  • physical complexity of the river system spreads
    the risk and avoids simultaneous catastrophes.

14
Summary
  • Floods are natural phenomena that form part of
    the normal part of many aquatic systems. The
    impacts of floods will depend on several factors,
    the more important of these being the size of the
    disturbed area, the nature of the river system,
    and the timing, frequency and duration of the
    flood.
  • Human activities are continuing to alter the rate
    at which river water enters stream channels, and
    these alterations become most apparent during
    heavy rainfall and normal flood events. These
    activities include (after Giller 1996)
  • Drainage
  • Afforestation development (preparation, growth,
    harvesting)
  • Dams
  • Channelisation
  • Dredging and straightening of streams
  • Flood alleviation schemes.
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