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Assessing climate change impacts on water resources in Chile

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Title: Assessing climate change impacts on water resources in Chile


1
Assessing climate change impacts on water
resources in Chile
Reunión profesores Estadounidenses
Fulbright Valparaiso, Chile 15 setiembre 2011
Ed Maurer Civil Engineering Department
2
Global Climate is Changing
  • Temperatures are increasing globally
  • Most recent warming attributed to human-driven
    GHG emissions
  • Some impacts already evident and attributable to
    warming

Source U.S. Global Change Research Program
(USGCRP)
3
Observed Changes 1970-2004
  • High confidence changes in
  • rainfall intensity
  • extreme temperatures
  • regional drought
  • glacier melt
  • early snowmelt
  • lake warming
  • Changes are consistent with observed warming, if
    not attributable

Source IPCC Climate Change 2007 Impacts,
Adaptation, and Vulnerability -- Summary for
Policymakers.
4
Projections of Global Change
  • Range of likely warming by end of 21st century
    variable
  • By mid-21st century most differences smaller

1.8
3.4
4.0
2.4
2.8
5
Which pathway are we on?
  • Current emissions are tracking above the most
    intense IPCC emission scenario

Raupach et al., PNAS, 2007 Global Carbon Project,
2009
  • Scenarios trends are averages across all models
    available for each scenario class.

6
Looking toward the future end of 21st century
21 modeled changes for A1B emissions 2080-2099
minus 1980-1999 Warming is large-scale,
certain Precipitation changes more regional, less
confident Regional changes drive regional
impacts .
Precipitation
number of models out of 21 that project increases
in precipitation
source IPCC, 2007
7
How do changes in Chile compare to the California
Case?
21 modeled changes for A1B emissions 2080-2099
minus 1980-1999 Warming is large-scale,
certain Precipitation changes more regional, less
confident Regional changes drive regional
impacts .
8
Regional Changes
  • Projected changes non-uniform
  • Impacts also non-uniform

Median runoff change, 2041-2060 minus 1901-1970
Source U.S. Global Change Research Program
(USGCRP)
9
Estimating regional impacts
2. Global Climate Model
4. Land surface (Hydrology) Model
1. GHG Emissions Scenario
5. Operations/impacts Models
  1. Downscaling

Adapted from Cayan and Knowles, SCRIPPS/USGS, 2003
10
Availability of GCM Simulations
  • 20th century through 2100 and beyond
  • gt20 GCMs
  • Multiple Future Emissions Scenarios

11
Need for Downscaling
  • Dynamic
  • Better representation of terrain captures local
    processes and feedbacks
  • Computationally expensive
  • Still contain biases
  • Statistical
  • Assumes stationary transfer function

12
Downscaling for Impacts Models
  • Bias correct and spatially downscale GCM output
  • Run hydrology model with projected climate

Raw GCM Output
13
Multi-Model Ensemble Projections for Feather River
  • Increase Dec-Feb Flows
  • 77 for A2
  • 55 for B1
  • Decrease May-Jul
  • 30 for A2
  • 21 for B1

14
Impact Probabilities for Planning
Snow water equivalent on April 1, mm
  • Combine many future scenarios, models, since we
    dont know which path well follow (22 futures
    here)
  • Choose appropriate level of risk

15
Translating this approach to Chile
Four key basins Ecologically and economically
important
16
Mataquito Basin
Tmed, Tmax, Tmin, P
Qdía
  • Series diarias
  • Se rellenan de series incompletas de P y Q
  • Análisis (1) estacional, (2) periodo pluvial y
    nival, (3) anual
  • Variables hidroclimatológicas e índices
    representativos
  • Tendencias (Mann-Kendall y Regresión Lineal)

17
Escenarios de Cambio Climático específicos cuenca
Mataquito
Para un solo escenario (A1b) pero ahora
estudiando un poco cambios en variabilidad
18
Snow Cover and Extreme Events
2002 2008
P 2 días previos (mm) 103.6 83.9
Caudal Máximo (m3/s) 931 2690
Tmax promedio (C) 13,0 17,4
Cota estimada línea de nieve (m) 1700 2200
  • Two events
  • 23 may 2008
  • 27 may 2002

A partir de Ps y Ts en Curicó, adoptando una
tasa de lapso de 9 C/Km
2002
2008
2008, with lower total rain produced greater peak
stream flow.
19
Capturing Uncertainties in an Ensemble -
Temperature
  • Internal variability (forecast) important first
    few years
  • Model Uncertainty dominates through mid-21st
    century
  • Uncertain emissions pathway most important after
    that

Hawkins Sutton, BAMS, 2009
20
Does this capture the range of uncertainties?
  • Perturbed physics experiments and theoretical
    feedback analyses extend tail to right
  • Uncertainty in emissions is on same order if
    planning horizon includes end of 21st century or
    beyond

Roe and Baker, 2007
21
Thanks!
22
Caudales (mm/año)
Temperatura Media Anual (Celsius)
Precipitaciones (mm/año)
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