piotr wolski
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Piotr Wolski. Climatic and hydrological changes in the Okavango Delta. The Okavango. Mohembo. Maun. The Okavango. it is Delta, not delta it is the 5th largest Ramsar site in the world it is the 3rd largest inland “delta” in Africa. The Okavango. Regional tectonic setting - PowerPoint PPT PresentationTRANSCRIPT
Piotr WolskiClimatic and hydrological changes in the Okavango Delta
Mohembo
Maun
The Okavango
The Okavango
• it is Delta, not delta• it is the 5th largest Ramsar site in the world• it is the 3rd largest inland “delta” in Africa
The Okavango
Frequency of tectonic events (after McCarthy, 1993)
Regional tectonic setting (after Kampunzu, 1998)
The Okavango
• Depth of the Kalahari form aeromagnetic survey (after Brunner, 2007)
February August
Seasonal flood pulse
Seasonal flood pulse
Human factor
Exogenous variability? change?
• Interannual and multidecadal variability. Or is it change?
Mohembo
Maun
Endogenous change
After McCarthy et al.
• Channel aggradation and abandonment
• Animal action (hippo paths)
• Water flow-vegetation-fire feedbacks
• Tectonic activity
Multidecadal variability
Air temperatureRainfall
CRU dataset and observations
Is it rainfall or temperature that affects the Okavango?
Both Neither Only P Only TObserved
Multi-Taper Method (MTM) of spectral analysis
Wolski et al. submittedDischarges respond stronger to multidecadal
variability in rainfall than in temperature!
What causes MDV in rainfall?
Pacific Decadal Oscillation ???
How will future look like?
- 18 CMIP3 GCMs
- 42 runs for 20th and 21st century
20th century rainfall:- Multidecadal variability present
- Timing is off!
21st century rainfall:- Similar magnitude of MDV to this observed in 20st century
- No consistent trend
How will future look like?
Multidecadal variability present, but superimposed on downward trend
Simulations of Okavango River discharges based on ensemble of GCM runs
Is climate change happening already?
Climate change attribution
Stone, Lennard, Tadross, Allen, Stott & Pall (2011)
Adjustment of:
•Atmospheric greenhouse gas concentrations
•Sea surface temperatures
Plans to include:
•Tropospheric sulphate aerosols
•Stratospheric volcanic sulphate aerosols
•Sea ice coverage
Attribution - results
temperaturerainfall
Attribution - results
Okavango discharge at Mohembo
FAR: -0.03 for 2009-0.19 for 2010
Probability of high floods decreases in warmer climate
Skill of models
How good is the GCM-hydro model combination in simulating Okavango flows?
“Good”years
“Bad”years
Self Organizing Maps
Classes of synoptic variables in a 6x4 SOM based on NCEP reanalysis data
Air temperature @ 2 m Relative Humidity @ 850 mbar
Self Organizing Maps
Frequency of synoptic states for each year
Significance of difference in frequency between “good” and “bad” years
p-value
0
1
There is potential for distinguishing “good” years from “bad” ones based on synoptic conditions
Data deficiency and flood modelling
Simulations of Okavango flows based on TRMM rainfall
TRMM data“Tweaked” MIRA + obs
Particularly significant in the context of seasonal forecasting
observed
TRMM-based
Endogenous change
Sat image Inundation map Time series
Distributary inundation
Analysis of change in inundation
Pixel inundation status as a function of system’s inundation area
Deviation of probability as a function of time
Inundation trends independent on inputs
Temporal trend in deviation of probabilities of inundation status
drier wetterNo change
Causes not fully understood, yet have implications on planning, management, cc adaptation etc.
Summary
• Okavango – a complex hydrological system, dynamics of which is influenced by several endogenous and exogenous factors:
• Interannual climate variability
• Multidecadal climate variability
• Climate change
• Endogeneous system transformation• Tectonics
• Geomorphological development of the wetland
• Strong international and local appeal – thus need for forecasting at seasonal, decadal and climate-change time-scales
Summary
• In the context of expansion of AfricaArray into hydrology/climate research:
• understanding of hydrological role of isostatic adjustment in the Delta, both on seasonal and long-term time-scales
• understanding of role of tectonic events on distribution of water in the Delta and monitoring of tectonic displacement during events
• Verification/improvement of hydrological models using GRACE, in the context of poor rainfall data
• Tectonic studies of incipient rifting etc…