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ENVIRONMENT. PILPS Update & Proposal. Ann Henderson-Sellers ANSTO Environment and Andy Pitman Macquarie University Sydney, Australia. PILPS Update August 2003. Arctic basin: ACSYS/PILPS completed with 17 papers in Special Issue of Global & Planetary Change (August 2003) - PowerPoint PPT Presentation
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ENVIRONMENT
PILPS Update & Proposal
Ann Henderson-SellersANSTO Environmentand Andy PitmanMacquarie UniversitySydney, Australia
ENVIRONMENT
ENVIRONMENT
PILPS Update August 2003• Arctic basin: ACSYS/PILPS
– completed with 17 papers in Special Issue of Global & Planetary Change (August 2003)
• Tropical forests: PILPS1(c) – still contributing to publs. (e.g. H-S & Pitman, 2002, BAMS)
• Frozen soil and snow: PILPS 2(d)– generating publications & prompting questions
• Luo et al. 2003, J Hydromet. (Valdai analysis)
• Coupled PILPS/AMIP II DSP12– LSS clusters and importance of LSSs in coupled
models now demonstrated
ENVIRONMENT
PILPS - still learning from off-line
• Carbon fluxes: PILPS C1– going very well; possible introduction to carbon
isotopes
• Arid environments: PILPS San Pedro– workshop this week (Bastidas & Gupta)
• Isotopes in GLASS: IPILPS– proposal to be tabled today focuses on:
• Stable water isotopes• Carbon isotopes
• When do these updates go on the GLASS web page?
ENVIRONMENT
PILPS Update - Highlights
• Chronological sequence in LSSs– ‘simple’ schemes; SiBlings; current generation
• Classes of carbon parameterisation– Rapid equilibrium of NPP & early CO2 sinks
– Gradual NPP increase & net CO2 sink zero early
• LSSs behave differently with different GCMs– Choice of LSS matters to climate prediction
• VIC is a better surrogate for ‘truth’ than re-analyses for evaporation at least
ENVIRONMENT
• Chronological sequence in LSSs– ‘simple’ schemes; SiBlings; current generation
Which group is ‘best’????
PILPS - still learning from off-line
ENVIRONMENT
Land-surface Energy Partition
• Energy budgets of 20 models (A-T) & 3 reanalyses
Latent Heat Flux W m-2
Scatter along diagonal shows differences in partitioning surface available energy
Scatter around diagonal due to predictions of different values of surface available energy
ENVIRONMENT
LSS Clusters in All Climates
Buckets; SiBlings; latest LSSScaled latent heat W m-2
Sca
led
sens
ible
hea
t W
m-2
SEBs normalised by ensemble of 3 re-analyses –
SiBlings
Buckets
3 clustersSiBlings
Buckets
SiBlings
Buckets
ENVIRONMENT
ENVIRONMENT
• Chronological sequence in LSSs– ‘simple’ schemes; SiBlings; current generation
• LSSs behave differently with different GCMs– Choice of LSS matters to climate prediction
Coupling does not eliminate characteristics or impacts of LSSs
PILPS - Off-line Links to GLACE
ENVIRONMENT
Spatio-temporal Correlation
• Climate trajectories differ for SiBlings & buckets
• LH improves from Arid (worst) to E. Humid (best)
Bucket
SiBling
• SH flows the other way
• Bucket (O) SH v. small & low variability
Bucket
SiBling
ENVIRONMENT
ENVIRONMENT
Atm
osp
her
ic fo
rcin
g fr
om
AM
IP A
GC
Ms
Pseudo Land-surface Schemes• Derived a PLSS for every
AMIP II model (A-T): columns
LH
Amazon
Mississippi
Mackenzie
• Apply in 3 basins: Amazon, Mississippi, Mackenzie
• Forced by all AGCMs: rows • Find:
– Agreement on main diagonal• PLSSs do a good job
– Range for different forcings• LSSs respond to different AGCMs
– ‘avg’ forcing is close to reported values
• mean = good estmt.
}}
ENVIRONMENT
Pseudo Land-surface Schemes
• Ranking predicted LHs
Atm
osp
her
ic fo
rcin
g fr
om
AM
IP A
GC
Ms
RankIrannejad et al., GRL 2003
• Stripes show LSSs often dominate over atmospheric forcing– in three diverse
regimes: Amazon, Mississippi, Mackenzie
– for 20 different AMIP II models and land-surface schemes
Amazon
Mississippi
Mackenzie
ENVIRONMENT
PILPS Update - Highlights
• Chronological sequence in LSSs– ‘simple’ schemes; SiBlings; current generation
• LSSs behave differently with different GCMs– Choice of LSS matters to climate prediction
• VIC is a better surrogate for ‘truth’ than re-analyses
Generally, all known data have been (over) used for parameterisation – need new!
ENVIRONMENT
VIC Best “Truth” for E/P Ratios
Mississippi
BALTEX
Murray Darling
ENVIRONMENT
VIC
VICObs
Obs
AMIP modelsmajor basins
VIC closeswater budgets& best at E/P
ENVIRONMENT
Evaluating LSS Performance
SiBlings best cf. VIC
VIC
Intermediateclimates -reanalyses and current LSSs closely grouped
Irannejad et al. 2003 find VIC is best surrogate for truth
ENVIRONMENT
ENVIRONMENT
Isotopes in PILPS : IPILPS
• Stable and radioactive isotopes are valuable for both tracing and dating
• Stable water isotope measurements – Demonstrated that the Amazon recycles its
water (3 or 4 times)– Prompted early GCM deforestation experiments
(e.g. Henderson-Sellers & Gornitz, 1984)
• Carbon isotopes differentiate C3 and C4 photosynthesis
• Off-line (PILPS) inter-comparison is timely e.g.– “Heavy” water (HD16O & H2
18O) at the land surface– River routing schemes tested against GNIR – the Global
Network for Isotopes in Rivers
Gibson et al., EOS December 2002
ENVIRONMENT
Recycling Small 18O Gradient
Gradient ~ 1.5‰ per 103 km cf. 2.0‰ for Europe
BelemManaus
Porto Velo
Sao Gabriel
Izobamba
1980s
1960s GNIP
H-S, McGuffie & Zhang, J. Clim., 2002, 15, 2664
ENVIRONMENT
Basin Isotope Modelling
• Isotopes provide an independent climate and water resource validation tool
H-S, Stone, McGuffie etc GRL, 2003,
Manaus
Enhanced D/H ratio
Darling
• Weakened signal in central Amazon (Manaus) indicates increased water recycling
• Logarithmic enhancement in Darling reveals irrigation impacts
ENVIRONMENT
ENVIRONMENT
Darling River 2002-3 Drought
Burtundy
WilcanniaWilcannia
MenindieMenindie
BourkeBourke
GunnedahGunnedah
CollarenabriCollarenabri
WalgettWalgett
0
10
20
30
40
50
60
1 3 5 7 9 11 13
delta O-18
del
ta D
Jan 2002Jan 2002
Jul 2002Jul 2002
Jan 2003Jan 2003
18O and Dmeasured in 2002-3 drought
Tracing a non-linear relation
Sydney
Melbourne
Brisbane
ENVIRONMENT
IPILPS: New Data & Results
Belem
Belem, Amazon
Precip
Vapour
D
18O
New isotopic data from Belem
Simulations with ISOLSM
Sim
ula
ted
18
O
ENVIRONMENT
Precip
ENVIRONMENT
IPILPS Science & Timeline • QUESTION: Are the stores and fluxes of two different
“heavy” water isotopes (HD16O & H218O) correctly
characterised at the land surface?• TIMELINE:
– August 2003: Approval by GLASS Panel– September/October 2003:
• Quality control of the available isotopic & met./hydro. data
– November/December 2003: • Experimental framework described and agreed
• Water isotopes only or plus carbon isotopes?
– January/February 2004: Call for participation to all current & past PILPS & AMIP II DSP 12
– April/May 2004: First workshop (possibly in Vienna)– December 2004: Publication of results