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Perspectivas INPE: 20052009

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Title: Perspectivas INPE: 20052009


1
Session 3 Impacts of Weather and Climate-Related
Extremes Social and Economic Impacts
José A. Marengo Earth System Sciences Center-
CCST National Institute for Space Research
INPE Sâo Paulo, Brazil
IPCC Working Group II Scoping Meeting Possible
Special Report on Extreme Events and Disasters
Managing the Risks Oslo, Norway 23-26 March
2009
2
EMDAT - The International Emergency Disasters
Database (www.emdat.be)  -
3
Climate change processes, characteristics
and threaths
4
Variability and changes in extremes
  • Where extreme weather events become more intense
    and/or more frequent?economic and social costs of
    those events will increase,
  • In drier areas?climate change is expected to lead
    to salinisation and desertification of
    agricultural lands (e.g In Latin America,
    semi-arid and arid areas)
  • Northeast Brazil may suffer a decrease of water
    resources due to climate change, with increasing
    precipitation variability with more dry spells
    and drought, and also a decrease in the
    groundwater recharge, and the rapid increase of
    population and water demand will exacerbate
    vulnerability.

5
Climate-related disasters (or not?)
  • There is evidence from various sources that
    indeed suggests that climate-related disasters
    are increasing in frequency at the global scale
  • By climate-related disaster, we mean a
    detrimental outcome of a climatic event with
    respect to a human system or a system on which
    humans directly depend.
  • Such a disaster is precipitated by the climatic
    event in question (for example an extreme
    precipitation event, windstorm, or drought), but
    its nature and severity is mediated by a variety
    of non-climatic factors and processes that serve
    to dampen or amplify the primary impacts of the
    triggering event.
  • Changes in the frequency of climate-related
    disasters are therefore not necessarily caused by
    meteorological changes, and are not necessarily
    attributable to global climate change.

6
R10
Tebaldi et al (2007)
CDD
Changes in R10 (number of days with rainfall
above 10 mm) and CDD (Consecutive dry days)
indices for IPCC AR4 A1B, 20802099 relative to
19801999.
7
Battisti et al (2009)
(1900-2006)
8
Drought
More rain
Drought
Less rain
El Niño impacts in South America
More rain
Drought
Less rain
High temp
More rain
9
Risk of frost in the Northern Andes
Glacier retreat in the Central Andes
Convergence of climatic, poverty and
agrodiversity vulnerabilities in Peru
10
Drought of Amazonia 2005 Relationship between
July-October anomalies in rainfall in
Western Amazonia and in the Index of the
north-south SST gradient across the tropical
Atlantic ocean (Cox et al. 2007)
Observations for the period 1901-2002
Model output from the HadCMLC GCM simulation
including aerosols is shown (1901-2002
Mean and STDV of the observation,
Simulation of the 21st century (2003-2100) using
the HadCMLC.
Mean and STDV estimated values for the 2005
Amazon drought
A 2005 drought caused widespread devastation
across the Amazon basin. Cox et al. (2008)
estimates that by 2025 a drought on this scale
could happen every other year and by 2060 a
drought could occur in nine out of every ten
years.
11
a.k.a. The Pentagon Report
Weather and climate extremes
climate refugees
12
Increase in the frequency of extreme rainfall
events for 2071-2100 relative to 1961-90 in
western Amazonia and southern Brazil-Northern
ArgentinaIncrease in the frequency of
consecutive dry days in eastern Amazonia,
Northeast Brazil west central Brazil
A2-CDD-Consecutive dry days
A2-R10-days com rainfall above 10 mm
13
Impacts and consequences
  • Floods?huge economical disasters both for not
    insured people/companies, under insured
    people/companies and insurance companies, numbers
    of human lives.
  • In Southern Brazil, heavy rainfall affected Santa
    Catarina State in November 2008 causing severe
    flooding and deadly mudslides, which affected 1.5
    million people and resulted in 120 casualties and
    left 69,000 people homeless. It was reported that
    most of the fatalities were caused by mudslides
    that swept away homes and business. Estimated
    cost so far US 350 million.
  • Drought? cut off entire cities from their current
    by rain feed water sources, causing major
    economical damage. Water shortages will lead to
    severe societal turbulence and drifting of the
    populations of complete regions.

14
Impacts and consequences
  • Rainfall deficits during summer and fall 2001
    resulted in a significant reduction in river flow
    throughout central Brazil, thereby reducing the
    capacity to produce hydroelectric power in these
    areas (90 of Brazils energy is from
    hydroelectric sources).
  • In 2005, large sections of SW Amazônia
    experienced one of the most intense droughts of
    the last hundred years. For the Acre State, the
    Defesa Civil estimated a lost of about US 87
    million due to the fires only, about 10 of the
    States GDP. As in 2001, the total cost of these
    droughts is not known
  • The drought that affects northern Argentina since
    2008 determined a reduction in the agricultural
    production, and together with the international
    price reductions determined a projection of
    reduction of about 30 in exportation, of about
    US 8-9 billion for 2009.

15
Cumulative Climate Change Index CCI
16
Human Development Index (HDI) for Brazil-2000
Human Development Index (HDI)-Income
Human Development Index (HDI)-Education
17
Sustainable development-human development-vulnerab
ility to climate change
  • The sustainability of development in South
    America is strongly linked to the capacity of
    responding to the challenges and opportunities
    associated with climate change. The economy is
    strongly based on climate-dependent natural
    resources.
  • Using the Human Development Index (HDI) as
    indicator, we see that the regions with lowest
    HDI are in the tropical region such as Amazonia
    and Northeast Brazil
  • The Cumulative Climate Change Index CCI suggests
    that tropical South America exhibits the highest
    CCI, indicating regions where climate change
    would be most intense.
  • The Amazon region and Northeast Brazil are the
    regions with highest CCI and also the regions
    with lowest HDI, suggesting that impacts of
    climate change would be strongest on poor
    regions in the tropics.

18
Elements of vulnerability profiles to climate
related disasters
19
A conceptual framework for risk
  • Research into the human dimensions of climate
    change tends
  • to concentrate on the concept of vulnerability,
    although various
  • definitions of vulnerability exist. These
    definitions essentially fall
  • into two categories
  • A formulation that views vulnerability as a
    function of climate hazard, the exposure of a
    system or population to that hazard, and the
    sensitivity of the system or population to the
    impacts of the hazard. In this context hazard is
    defined purely in physical terms, for example
    absolute values of or anomalies in meteorological
    or climatic variables such as rainfall,
    temperature, or wind speed.
  • A formulation that views vulnerability as a
    function purely of the internal properties of a
    system, for example the set of social, economic,
    political and environmental factors that mediate
    the impacts of any given hazard for a particular
    system.

20
Social and economical aspects of climate change
Need for integrated assessments and adaptation
measures
  • Not only places, but also persons have distinct
    vulnerabilities. Different social groups are
    exposed to different hazards of climate change
    and with different resources to respond to them.
  • It is therefore necessary to identify these
    groups, locate them in the urban space and
    describe them socially and demographically for
    more efficient public policy.
  • There is a need for projects intended to
    integrate the projections of climate alterations
    and socio-economic models, such that an
    integrated analysis of the economic impacts of
    these phenomena can be produced.
  • On the basis of that, adaptation and mitigation
    policies may be proposed and implemented.

21
Countries must prepare for possible impacts of
climate change and extremes for IVA assessments
  • Improve regional and global climate models,
    including historical trend analyses
  • Assemble comprehensive integrated models of
    climate change impacts.
  • Create vulnerability metrics to understand
    countrys vulnerability to the impacts of climate
    change.
  • Prepare and test adaptive responses to address
    and prepare for inevitable climate driven events
    such as massive migration and food and water
    supply shortages.
  • Explore local implications of climate change and
    extremes in urban and rural areas, and develop
    estimates economical damages. Risk management can
    be applied in all of these contexts.
  • Future sustainable development plans should
    include adaptation strategies to enhance the
    integration of climate change into development
    policies.

22
Developing adaptation efforts (Interaction of
GT1 and 2 of IPCC)
  • Effective adaptation strategies require
    understanding of regional / local dimensions of
    vulnerability
  • Climate change does not occur in isolation
    multiple stresses (non climatic)
  • Domestic policies can enhance or constrain
    society ability to adapt to climate change
  • Adapting to climate variability and climate
    change
  • Adaptation and sustainable development policies
  • Take advantage of the work of the UN-Department
    of Economic and Social Affairs (UNDESA) on the
    indicators of Climate Change and Sustainable
    Development, as official national indicators
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