Transcript Document

“Applying probabilistic
climate change information
to strategic resource
assessment and planning”
Funded by
ENVIRONMENT AGENCY
TYNDALL CENTRE
OUCE
Oxford University Centre for the Environment
Overall Objective
To develop a risk-based framework for
handling probabilistic climate change
information and for estimating
uncertainties inherent to impact
assessments performed by the Agency
for strategic planning (water resources
and biodiversity in the first instance).
OUCE
Oxford University Centre for the Environment
Specific Objectives

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To develop and compare methods for generating
regional/local scale climate change probabilities
from coarse resolution CP.net data.
To trial the application of probabilistic climate
change information to Agency-relevant case
studies (initially for water resources and
biodiversity management).
To explore the added-value of probabilistic
scenarios for strategic planning and practical
lessons learnt from the case studies.
To share the techniques and experience gained
from the exemplar projects with a wider
community of partner organisations and
stakeholders.
OUCE
Oxford University Centre for the Environment
climateprediction.net aims to…
 Sample
uncertainty in climate
models across
– Physics
– Initial conditions
– Climate forcing
 Provide
better understanding of
plausible future climate changes that
can be forecast with one GCM
species
OUCE
Oxford University Centre for the Environment
Experimental Strategy
 Distributed
public computing – port
HadCM3 to windows/linux/mac
 Each
participant runs a specific
experiment
– Different model physics, initial
conditions, forcing
– Currently 17 million model years
OUCE
Oxford University Centre for the Environment
Phase 1
2
x CO2 equilibrium experiments
– 15 years calibration at 1 x CO2
– 15 years control at 1 x CO2
– 15 years at 2 x CO2
OUCE
Oxford University Centre for the Environment
ClimatePrediction.net
OUCE
Oxford University Centre for the Environment
Data Available
 Global
 Eight
mean time series
year seasonal climatologies
– Surface air temperature
– Precipitation
– Cloudiness
– Surface heat budget
OUCE
Oxford University Centre for the Environment
Phase 2
 Transient
simulations with HadCM3
– 1920-2000 “hindcast”
– 2001-2080 forecast
 Launched
with BBC in February
OUCE
Oxford University Centre for the Environment
Data Available in Phase 2
 More
variables
 Global
mean monthly time series
 Regional
monthly time series (Giorgi;
NAO; MOC)
 UK
grid-box monthly series
 Ten-year
seasonal climatologies
(1920-2080)
OUCE
Oxford University Centre for the Environment
First Results
 Use
of CP.Net probabilistic climate
change data for water resource
assessment in the Thames basin
– CATCHMOD: water balance model of
River Thames basin
– CP.net data available from Experiment 1
– Results and discussion
OUCE
Oxford University Centre for the Environment
CATCHMOD: water balance model
of River Thames basin.
OUCE
Oxford University Centre for the Environment
River Thames Basin upstream of
Kingston gauge and GCM grid-boxes
OUCE
Oxford University Centre for the Environment
CATCHMOD: parameters
 Six
key parameters controlling
– Direct runoff
– Soil WC at which evaporation is reduced
– Drying curve gradient
– Storage constant for unsaturated zone
– Storage constant for saturated zone
Wilby and Harris (2005)
OUCE
Oxford University Centre for the Environment
CATCHMOD
 Inputs:
daily time series of
precipitation (PPT) and potential
evaporation (PET)
 Output:
daily time series of river flow
 Parameters
:chosen as the ones that
best reproduce observed flows for
the period 1960-1991
OUCE
Oxford University Centre for the Environment
CP.net Data
 Grand
ensemble of 2578 simulations
of the HadAM3 GCM
 Explores
7 parameter perturbations
and perturbed initial conditions
 450
IC ensembles (model versions)
OUCE
Oxford University Centre for the Environment
CP.net variables and CATCHMOD
Inputs
 8-year
seasonal means for:
– total cloud amount in LW radiation
– surface (1.5m) air temperature
– total precipitation rate
 Use
these to calculate change factors
for PPT and PET over Thames
 Change
factors used to perturb
CATCHMOD daily time series of PPT &
PET
OUCE
Oxford University Centre for the Environment
Results: Change Factors
Temperature at
2xCO2
PPT (%CF)
PET (%CF)
PPT vs PET
OUCE
Oxford University Centre for the Environment
Results: Standard CATCHMOD
+ unperturbed HadAM3
* present day
OUCE
Oxford University Centre for the Environment
Results: CP.net and CATCHMOD
Q50
Q50
OUCE
Oxford University Centre for the Environment
Results: CP.net and CATCHMOD
Q95
Q95
OUCE
Oxford University Centre for the Environment
Factors not Considered
 Full
set of CP.net perturbations
 Emissions
uncertainty
 Downscaling
uncertainty
 Alternative
model structures (GCM
and Hydrological)
 Coupled
transient climate response
OUCE
Oxford University Centre for the Environment
Are Probabilistic Approaches
Useful?

CP.net provides useful climate information
– particularly joint probabilities of key
variables

Enable more informed decision making

Issues for Water Utility stakeholders
–
–
–
–
Understanding the information
Having time and resources to use information
Regulatory constraints
In many cases other (non-climate) factors are
more uncertain
OUCE
Oxford University Centre for the Environment
CP.net parameters
Parameter
Description
VF1(m/s)
Ice fall speed.
CT(1/s)
Cloud droplet to rain conversion rate.
RHCRIT
Threshold of relative humidity for
cloud formation.
CW_sea
(1/kgm^3)
Cloud droplet to rain conversion
threshold.
CW_land
EACF
Empirically adjusted cloud fraction.
ENTCOEF
Scales rate of mixing between
environmental air and convective
plume.
OUCE
Oxford University Centre for the Environment
Potential Evaporation
Penman PET is a function of mean air T, mean vapour pressure (vp), sunshine
and wind speed
Present : calculate monthly Penman PET using observed climate variables for
London (monthly long term means 1961-1990, UK national grid)
2xCO2 : calculate monthly Penman PET assuming:
wind speed = constant
relative humidity = constant thus relative change in vp=relative change in svp
relative change in sunshine = - relative change in cloud amount
T at 2xCO2= observed T + deltaT
vp at 2xCO2= observed vp x (1+CF(svp))
sunshine at 2xCO2 = observed sunshine x (1-CF(cloud))
CF calculated using control and 2xCO2 phases for all the variables.
OUCE
Oxford University Centre for the Environment
Smoothed frequency
distributions and
CDFs: Q50
Uncertainties:
•Climate model parameterization
•Hydrological model
parameterization
•No downscaling
•No hydrological model structure
OUCE
Oxford University Centre for the Environment
Smoothed
frequency
distributions and
CDFs: Q95
Uncertainties:
•Climate model parameterization
•Hydrological model parameterization
•No downscaling
•No hydrological model structure
OUCE
Oxford University Centre for the Environment
Smoothed frequency
distributions and CDFs:
Q95
Uncertainties:
•Climate model parameterization
•Hydrological model parameterization
•No downscaling
•No hydrological model structure
OUCE
Oxford University Centre for the Environment
Frequency distribution of
flows: annual statistics
Uncertainties:
•CP.net parameter dependence
•No hydrological model
•No downscaling
•No hydrological model structure
OUCE
Oxford University Centre for the Environment
Frequency distribution
of flows: annual
statistics
Uncertainties:
•CP.net parameter dependence
•No hydrological model
•No downscaling
•No hydrological model structure
OUCE
Oxford University Centre for the Environment
Frequency distribution
of flows: annual
statistics
Uncertainties:
•CP.net parameter dependence
•No hydrological model
•No downscaling
•No hydrological model structure
OUCE
Oxford University Centre for the Environment