Coping with Climate Risk climate sensitivity, coping ranges and risk

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Coping with Climate Risk climate sensitivity, coping ranges and risk

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Title: Coping with Climate Risk climate sensitivity, coping ranges and risk


1
Coping with Climate Riskclimate sensitivity,
coping ranges and risk
AIACC Training Workshop on Adaptation and
Vulnerability TWAS, Trieste June 3-14 2002
  • Roger N. Jones

2
Coverage
  • Impacts are sensitive to climate variability and
    extremes
  • Coping ranges as a tool to understand the
    relationship between V, I and A.
  • Operationalising coping ranges for risk assessment

3
Impacts are sensitive to climate variability and
extremes
  • Sensitivity to climate is
  • how much a system or activity is affected by
    climate-related stimuli

4
Insensitive Unaffected by rain, hail, sun, wind
or snow
5
Sensitive Easily affected by rain, hail, sun,
wind and snow
6
Sensitivity to what?
7
Extreme temperature
8
Extreme temperature
Increasing stress
9
How do we assess extremes?
  • In two ways, rarity and impact
  • 1. As a rare event
  • 2. As an event with extreme outcomes
  • Extreme events are rare events with significant
    impacts, but under climate change may become more
    common

10
Types of extreme climate events
11
Confidence levels
  • Climate Variable
  • Atmospheric CO2 concentration
  • Global-mean sea-level
  • Global-mean temperature
  • Regional seasonal temperature
  • Regional temperature extremes
  • Regional seasonal precipitation/cloud cover
  • Changes in climatic variability (e.g. El Niño,
    daily precipitation regimes)
  • Rapid or non-linear change (e.g. disintegration
    of the West Antarctic Ice Sheet)

High confidence Low confidence Very low or
unknown
12
Modelling climate variability
  • Most impacts are sensitive to climate variability
    rather than the mean (atmospheric CO2 is a
    notable exception)
  • Climate models represent climate variability
    relatively poorly
  • Realistic and plausible scenarios of climate
    variability are needed

13
Linking climate to impacts
14
IPCC 1994
15
Two approaches to VA
  • ?V ?I ?A
  • V ? I A, t
  • t 0, current climate, reference or baseline
  • Time t relates to the planning horizon

16
Coping with climate (variability and extremes)
  • A system can cope with some combinations of
    climate but other combinations will cause damage
  • The ability to cope is a function of the
    sensitivity of a system to climate and its
    response to that sensitivity
  • This response is the interaction of
    socio-economic and biophysical factors

17
Coping range under current climate
18
Coping range under current climate - limited
ability to cope
19
Coping range structure (1)
  • A coping range exists where climate
    socioeconomic interactions are beneficial or
    suffer only tolerable damage. The width of the
    coping range is in part due to historical
    adaptation
  • It is separated from an area of vulnerability by
    a threshold. The threshold can be critical,
    marking a level of harm that is intolerable, or
    mark a given level of hazard
  • Beyond the coping range and threshold is a zone
    of vulnerability

20
Coping range structure (2)
  • Simple
  • Expressed in terms of one or two climate
    variables (e.g. rainfall, temperature)
  • Complex
  • Expressed in terms of secondary or tertiary
    variables with a known relationship with climate
    (e.g. stream flow, crop yield, rates of
    infectious disease)

21
Coping range dynamics
  • Two aspects of the coping range can change
  • 1. Climate
  • 2. Socioeconomic (affecting the width of the
    coping range)
  • a. autonomous socioeconomic change may increase
    or decrease the width
  • b. climatic events may trigger a contraction
    (through damage) or an expansion (adaptation to
    similar future events)
  • We would like to add
  • c. expansion to reduce anticipated future
    vulnerability

22
Changing coping range - socioeconomic change
23
Changing coping range - response to climate
stress
24
Future climate - no adaptation
25
Future climate with adaptation
26
Thresholds
  • A non-linear change in a measure or system,
    signalling a physical or behavioural change
  • Climate-related thresholds are used to mark a
    level of hazard

27
Thresholds as climate hazards
  • There are two ways to construct climate hazards
    to use as thresholds
  • 1. Natural hazards approach a fixed threshold
    such as 1 in 100-year flood, storm surge or given
    storm strength applied over time and space.
    Especially good for locating most vulnerable
    areas.
  • 2. Vulnerability-based approach the climatic
    conditions resulting in a degree of harm that
    exceed the limits of tolerance. Usually specific
    to a given activity and location (e.g. drought,
    water supply, crop yields). Useful when
    constructed with stakeholder participation.

28
Thresholds
  • Biophysical
  • (simple to complex)
  • Tropical cyclone
  • Coral bleaching
  • ENSO event
  • Island formation
  • Island removal
  • Socioeconomic
  • (usually complex)
  • Legal/regulatory
  • Profit/loss
  • Cultural
  • Agricultural
  • Critical

29
Critical thresholds
  • A level considered to represent an unacceptable
    degree of harm
  • This is a value judgement and may be decided by
    stakeholders, be a legal requirement, a safety
    requirement, a management threshold etc

30
Planning horizons
31
Using coping ranges to assess risk current risk
  • Choose a reference or baseline period pertinent
    to both climate and the socioeconomic background
  • Calculate threshold exceedance based on climate
    exposure during the reference period
  • Existing adaptations and those needed to reduce
    risk under present climate provide the short-term
    options for a win-win adaptation strategy
    (helping cost-benefit and efficiency criteria)

32
Using coping ranges to assess risk future risk
  • Each scenario will give a different probability
    of threshold exceedance
  • If using single, or several scenarios, these
    should be related to the full range of
    uncertainty for climate change, when
    communicating results
  • The effect of climate and socioeconomic scenarios
    can be assessed separately or together
  • Methods can range from semi-quantitative (simple)
    through to the application of advanced
    probabilistic techniques (difficult but
    interesting)

33
What is a risk?
  • Two uses
  • 1. In general language
  • 2. A specific operational meaning

34
Characterising risk
  • Risk is a combination of hazard, likelihood and
    vulnerability, i.e. stress, how likely that
    stress is, and how much damage that stress will
    cause.

35
Natural hazards approach to risk
  • Fixed climate hazard - e.g. 1/100 flood,
    hurricane.
  • Likelihood - frequency of occurrence likelihood
    that it will occur
  • Vulnerability - damage incurred
  • Risk f(hazardlikelihood, vulnerability)

36
Natural hazards approach to risk
  • Examples
  • Heat stress - hastened mortality per 103 or 105
    population
  • Flood damage mapping (e.g. damage or dwellings
    inundated per 100 year flood)
  • Storm damage mapping (structural damage for a
    given windspeed in or no. of buildings
    damaged)
  • Disease mapping (vector density aligned with
    infection rates)
  • ENSO frequency and intensity aligned with known
    hazards

37
Vulnerability-based approach to risk
  • Level of climate associated with given level of
    harm, e.g. critical threshold
  • Likelihood - frequency of occurrence likelihood
    that it will occur
  • Risk f(hazardvulnerability, likelihood)

38
Example - water supply for irrigation and wetland
management
  • Macquarie catchment - Australia
  • Climate baseline Daily P and Ep data 1890-1996
    infilled across the catchment
  • Management reference 1996 infrastructure and
    catchment management rules
  • Irrigation water allocation is capped and supply
    is shared between irrigation and environmental
    flows through the Macquarie Marshes
  • Thresholds
  • Supply of 350 GL into the Macquarie Marshes for
    waterbird breeding
  • Irrigation water allocation of 0, 50 or 100

39
Simulated flow into the Macquarie Marshes -
baseline case
40
Simulated flow into the Macquarie Marshes -10
flow (IS92c HCM3)
41
Simulated flow into the Macquarie Marshes -10
flow (IS92c HCM3)
42
Simulated irrigation allocations baseline and
-10 flow (IS92c HCM3)
43
Simulated irrigation allocations baseline and
-10 flow (IS92c HCM3)
44
Sensitivity analysis for Burrendong Dam storage
45
Sensitivity analysis for Burrendong Dam storage
Driest (SRES)
Exceeding critical threshold
Wettest (SRES)
46
Changes to MAF for 9 models in 2030 ()Based on
IPCC 2001
A1T at 4.2C 1.27C
B1 at 1.7C 0.55C
A1 at 2.5C 0.91C
47
Changes to Burrendong Dam storage 2030
48
Probabilities of flow changes - impacts view
Range of possible outcomes
49
Basic principles
  • Pay greater attention to recent climate
    experience. Link climate, impacts and outcomes to
    describe the coping range.
  • Address adaptation to climate variability and
    extremes as part of reducing vulnerability to
    longer-term climate change.
  • Assess risk according to how far climate change,
    in conjunction with other drivers of change, may
    drive activities beyond their coping range.
  • Focus on present and future vulnerability to
    ground future adaptation policy development in
    present-day experience.
  • Consider current development policies and
    proposed future activities and investments,
    especially those that may increase vulnerability.
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