Foundation - 1.2 Systems Flashcards

1
Q

Systems

A

An assemblage of constituent parts as well as the interactions and relationships which make up these parts, which together make up an entity

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2
Q

Systems approach

A

Term used to describe a method of simplifying and understanding a complicated set of interactions

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3
Q

Two ways of studying systems

A
  • reductionist approach
  • holistic approach
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4
Q

Reductionist approach

A

Breaking a system down into its parts and studying each individually
* can be useful for partially understood systems

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5
Q

Holistic approach

A

Looks at the system’s processes and interactions as a whole

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6
Q

Flows

A

Provide inputs and outputs of energy and matter
* they can either be transfers or transformations

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7
Q

Transfers

A

A change in location but no change in matter

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8
Q

Transformations

A

A change in chemical nature, a change in state or a change in energy as well as a change in location

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9
Q

Storage

A

Represented by rectangles, usually with their size being proportional to the storage itself

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10
Q

Emergent properties

A

A property of a system but not of the individual parts of the system

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11
Q

Main types of systems

A
  • Open
  • Closed
  • Isolated (hypothetical)
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12
Q

Open systems

A

Both energy and matter are exchanged between the systems and its surrounding
* usually organic (living) systems that interact with surroundings
* e.g. most ecosystems, as well as our bodies

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13
Q

Closed systems

A

Energy, but no matter, is exchanged between the systems and its surroundings
* usually inorganic
* e.g. the Earth (and its atmosphere) could be considered one, though its debated

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14
Q

Isolated systems

A

Neither energy nor matter are exchanged between the system and its surroundings
* do not exist naturally, theoretical concept (though universe could be one)

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15
Q

Scales of systems (with examples)

A
  • Small-scale ecological system: bromeliad (plant in rainforest) forms microcosm of life
  • Large-scale ecosystem: entire rainforest where countless species interact within a complex web of relationships
  • Giant, self-contained system: the Earth’s atmosphere
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16
Q

Gaia hypothesis

A

Proposed by James Lovelock (1970s)
* Presented Earth as a single, self-regulating system

17
Q

Tipping point

A

The minimum amount of change within a system that will destabilise it, causing it to reach a new equilibrium or stable state

18
Q

Positive feedback loops

A

The product of a reaction leads to an increase in that reaction, again and again

19
Q

Regime shift

A

The formation of a new equilibrium as a result of positive feeback loops

20
Q

Steps of reaching a tipping point

A
  1. The system is subject to some kind of pressure
  2. This pressure pushes the system towards a tipping point
  3. The tipping point is reached
  4. Positive feedback loops accelerate the shift into a new state
  5. Change is often irreversible or a high cost is required to return it to previous state
21
Q

Reasons why tipping points are difficult to predict (name 3)

A
  • Often delays of carying length involved in feedback loops which add complexity of modelling systems
  • Not all components change abrubtly at the same time
  • May be impossible to identify a tipping point until after it has been passed
  • One activity in one part of the globe may lead to a system reaching a tipping point elsewhere on the planet
22
Q

Resilience

A

Ability of a system to maintain stability and avoid tipping point

23
Q

Factors affecting stability of system (name 3)

A
  • Disturbance frequency and intensity
  • Size of storages
  • Species diversity, interactions (competition)
  • Trophic complexities (how many system components are there)
  • Rate of nutrient or energy influx (how fast nutrients and energy are moving in and out of system)
24
Q

Model

A

A simplified version of reality
* can be analysed or tested to learn about how the system works and predict its behaviour

25
Q

Strengths of models (name 3)

A
  • Models simplify complex systems
  • Models allow predictions to be made about how systems will react in response to change
  • System inputs can be changed to observe effects and outputs without the need to wait for real-life events to occur
  • Easier to understand than the real system
  • Results can be shared between researchers and communicated to the public
  • Results can warn us about future environmental issues
26
Q

Limitations of models (name 3)

A
  • Can be oversimplified or inaccurate
  • Results depend on the quality of data of inputs
  • Results become more uncertain the further they predict into the future
  • Different models can show vastly different outputs even if they have the same inputs
  • Results can be interpreted differently by different people
  • Can be very complex
27
Q

Static equilibrium

A

No inputs or outputs (of energy or matter) to the system and therefore the system shows no change over time
* no natural systems are such

28
Q

Unstable/dynamic equilibrium

A

Even small disturbances can cause the system to suddently shift

29
Q

Negative feedback

A

When the output of a process inhibits or reverses the operation of the same process in such a way as to reduce change
* stabilising as they counteract deviation

30
Q

Positive feeback

A

When a disturbance leads to an amplification of that disturbance, destabilising the system and driving it away from its equilibrium