berry climate change projections and implication
DESCRIPTION
Presentation at "The River, the Bay and the Strait" public forum, 5 October, 2008, Hervey BayTRANSCRIPT
Climate Change ProjectionsClimate Change Projectionsand Implicationand Implication
The River, the Bay and the Strait The River, the Bay and the Strait ForumForum
Up FrontUp Front This presentation is not about the This presentation is not about the
science of climate change.science of climate change. Assuming that the climate is already Assuming that the climate is already
changing and it will continue to do so changing and it will continue to do so even with mitigation.even with mitigation.
Projection not fact. Still requires Projection not fact. Still requires development of peer review process development of peer review process and adoption into policy.and adoption into policy.
ProblemsProblems Differing projections depending on model Differing projections depending on model
used.used. State Government guaranteeing flow rates State Government guaranteeing flow rates
and yield based on CSIRO projections.and yield based on CSIRO projections. 78% of catchment area does not 78% of catchment area does not
correspond to 78% of flow.correspond to 78% of flow. Removing 22% of a catchment area will Removing 22% of a catchment area will
have an impact, especially in addition to have an impact, especially in addition to reduced rainfall.reduced rainfall.
SimCLIM Family TreeSimCLIM Family Tree
VANDACLIM (island version)
BDCLIM (Bangladesh)
VANDACLIM (fictitious country)
OZCLIM (CSIRO)
1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005
CLIMPACTSCLIMPACTS
CHAMP (New Zealand)
CANCLIM (Canada)
SimCLIM
SriLankaCLIM
HOTSPOTS (NZ)
TopoCLIM
Hard-wired
Open-system
DryCLIM
COMMERCIAL VERSION
Source: CLIMsystemsSource: CLIMsystems
Climate ModellingClimate Modelling
Where computer programs make Where computer programs make projections about future climate projections about future climate using:using:1. Global circulation models (GCMs),1. Global circulation models (GCMs),
2. Emission scenarios, and2. Emission scenarios, and
3. Climatic sensitivity.3. Climatic sensitivity.
Global Circulation Models Global Circulation Models (GCMs)(GCMs)
Physically based, complex, 3D models.Physically based, complex, 3D models. Take into account as many factors as Take into account as many factors as
possible that could influence climate and possible that could influence climate and hence simulate the global climate system.hence simulate the global climate system.
Climate factors include: wind patterns and Climate factors include: wind patterns and ocean currents, cyclones, El Nino, ice-ocean currents, cyclones, El Nino, ice-sheets, clouds, ecosystems etc.sheets, clouds, ecosystems etc.
Source: CLIMsystemsSource: CLIMsystems
Emission ScenariosEmission Scenarios
Source: Source: http://www.grida.no/climate/ipcc/emission/index.htm
2008 2020
2050 2100
Kandanga
Imbil
Kenilworth
Maleny
Kandanga
Imbil
Kenilworth
Maleny
Kandanga
Imbil
Kenilworth
Maleny
Kandanga
Imbil
Kenilworth
Maleny
Annual Average Change in Annual Average Change in Precipitation (mm):Precipitation (mm):
20082008 20202020 20502050 21002100
KandangaKandanga 1197.5 – 1197.5 – 1374.01374.0
1197.5 – 1197.5 – 1374.01374.0
1020.9 – 1020.9 – 1197.51197.5
844.3 – 844.3 – 1020.91020.9
ImbilImbil 1020.9 – 1020.9 – 1197.51197.5
1020.9 – 1020.9 – 1197.51197.5
1020.9 – 1020.9 – 1197.51197.5
844.3 – 844.3 – 1020.91020.9
KenilworthKenilworth 1197.5 – 1197.5 – 1374.01374.0
1197.5 – 1197.5 – 1374.01374.0
1020.9 – 1020.9 – 1197.51197.5
844.3 – 844.3 – 1020.91020.9
MalenyMaleny 1727.2 – 1727.2 – 1903.81903.8
1727.2 – 1727.2 – 1903.81903.8
1550.6 - 1550.6 - 1727.21727.2
1374.0 – 1374.0 – 1550.61550.6
Annual Average Change in Annual Average Change in Precipitation (mm/year):Precipitation (mm/year):
19901990 21002100
BundabergBundaberg 10601060 840840
MaryboroughMaryborough 11481148 920920
GympieGympie 11851185 955955
KingaroyKingaroy 790790 612612
GayndahGayndah 725725 550550
MontoMonto 702702 535535
2008 2020
2050 2100
Kandanga
Imbil
Kenilworth
Maleny
Kandanga
Imbil
Kenilworth
Maleny
Kandanga
Imbil
Kenilworth
Maleny
Kandanga
Imbil
Kenilworth
Maleny
Annual Average Maximum Annual Average Maximum Temperature Change (Temperature Change (00C)C)::
20082008 20202020 20502050 21002100
KandangaKandanga 24.0 – 24.0 – 25.325.3
25.3 – 25.3 – 26.626.6
26.6 – 26.6 – 27.927.9
31.7 – 31.7 – 33.033.0
ImbilImbil 24.0 – 24.0 – 25.325.3
25.3 – 25.3 – 26.626.6
26.6 – 26.6 – 27.927.9
31.7 – 31.7 – 33.033.0
KenilworthKenilworth 22.7 – 22.7 – 24.024.0
24.0 – 24.0 – 25.325.3
25.3 – 25.3 – 26.626.6
29.1 – 29.1 – 30.430.4
MalenyMaleny 21.5 – 21.5 – 22.722.7
22.7 – 22.7 – 24.024.0
24.0 – 24.0 – 25.325.3
29.1 – 29.1 – 30.430.4
Annual Average Maximum Annual Average Maximum Temperature Change:Temperature Change:
19901990 21002100
BundabergBundaberg 26.6326.63 29.71 - 33.3129.71 - 33.31
MaryboroughMaryborough 26.5026.50 29.49 - 32.9929.49 - 32.99
GympieGympie 25.7825.78 28.82 - 32.3828.82 - 32.38
KingaroyKingaroy 24.8224.82 28.21 - 32.1928.21 - 32.19
GayndahGayndah 27.5927.59 30.98 - 34.9530.98 - 34.95
MontoMonto 27.3327.33 30.71 - 34.6630.71 - 34.66
Number of days over Number of days over 353500CC/year/year
20082008 20302030 20502050 20752075 21002100
ImbilImbil 77 1212 2020 4545 7272
Kandanga, Cooroy, Kenilworth and Maleny – no temperature data recorded.
Number of days over Number of days over 404000CC//yearyear
20082008 20302030 20502050 20752075 21002100
ImbilImbil 0.10.1 0.70.7 1.71.7 66 1414
Kandanga, Cooroy, Kenilworth and Maleny – no temperature data recorded.
Number of days over Number of days over 353500CC//yearyear19901990 20202020 20502050 20752075 21002100
BundabergBundaberg 11 22 1010 5959 123123
MaryboroughMaryborough 33 55 3737 6666 114114
GympieGympie 1010 1414 3030 5959 9191
KingaroyKingaroy 44 77 2424 6565 108108
GayndahGayndah 2222 3333 7777 140140 193193
MontoMonto 1919 2828 6262 118118 164164
ConclusionsConclusions Impossible to guarantee water above or Impossible to guarantee water above or
below dam.below dam. Different software packages, models and Different software packages, models and
scenarios can give different projections.scenarios can give different projections. Higher temperatures mean higher levels of Higher temperatures mean higher levels of
evaporation and evapotranspiration.evaporation and evapotranspiration. Longer growing seasons for aquatic Longer growing seasons for aquatic
weeds.weeds. Higher demand for water. Higher demand for water.
Future ResearchFuture Research
Increase accuracy of rainfall projections to Increase accuracy of rainfall projections to local areas i.e. models & data used.local areas i.e. models & data used.
Flow rate projections for the Mary River to Flow rate projections for the Mary River to be determined.be determined.