Simulation of Seasonal and Interannual Variability in the Caspian Sea - PowerPoint PPT Presentation

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Simulation of Seasonal and Interannual Variability in the Caspian Sea

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Simulation of Seasonal and Interannual Variability in the Caspian Sea W. Paul Budgell Dept. of Physics and Physical Oceanography, Memorial University of Newfoundland – PowerPoint PPT presentation

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Title: Simulation of Seasonal and Interannual Variability in the Caspian Sea


1
Simulation of Seasonal and Interannual
Variability in the Caspian Sea
  • W. Paul Budgell
  • Dept. of Physics and Physical Oceanography,
  • Memorial University of Newfoundland
  • Ralf Toumi, Andrew Singleton,
  • Catherine Reifen, James Farley Nicolls
  • Dept. of Physics, Imperial College, London

2
Outline of Talk
  • Background/Motivation
  • ROMS Implementation
  • Forcing
  • Some Results
  • Conclusions/Future work

3
(No Transcript)
4
Motivation
  • Regional climate change but first we must gain
    confidence on recent history and variability
  • Dynamical downscaling, but after Gildas Cambons
    talk will revisit statistical downscaling
  • Regional coupled environmental model
  • Operational applications in oil spills, localized
    wave climate, contaminant /salt/aerosol transport

5
(No Transcript)
6
Caspian Sea Bathymetry (m)
7
(No Transcript)
8
(No Transcript)
9
CSL in IPCC 20th Century Simulations
From Elguindi and Giorgi, Clim. Dyn. 26 (2006)
395-379.
10
Projected Changes in CSL
From Elguindi and Giorgi, Clim. Dyn. 26 (2006)
395-379.
11
(No Transcript)
12
(No Transcript)
13
(No Transcript)
14
(No Transcript)
15
(No Transcript)
16
(No Transcript)
17
WRF Simulation Nov. 1996
18
(No Transcript)
19
ROMS Set-Up
  • Kate Hedströms branch
  • Ice dynamics/thermodynamics shallow
  • Wetting-drying (dcrit 0.2 m)
  • Sea level is dependent upon (E-P)
  • 4 km resolution
  • 32 and 20 vertical levels
  • Vtransform2, Vstretching2
  • ?s8, ?b0.4, hc10 m

20
ROMS Set-Up Contd
  • River inflow specified for 6 largest rivers
  • Atmospheric forcing from ERA40, ERA Interim, or
    WRF (down-scaling ERA40)
  • Runs for 1958-2001 (ERA40), 1989-2008 (ERA
    Interim), or 1980-2001 (WRF)
  • Climate sensitivity run with reduced river inflow
    for 1980-2001 (2045-2066)

21
Some Results
22
ROMS Sea Ice Extent
23
(No Transcript)
24
SST Comparison
25
Caspian Sea Levels
26
Conclusions/Future Work
  • E-P sea level wetting/drying sea ice works
  • Change in surface area important
  • Very sensitive to river runoff
  • WRF higher wind speeds improve evaporation
  • ROMS-WRF coupling needed
  • ROMS-WRF-SWAN coupling needed

27
Job Opportunity
  • Dept. of Physics, Imperial College, London is
    hiring post-doc to conduct development of Caspian
    Regional Environmental Model.
  • CREM based on coupled ROMS-WRF-SWAN for the
    Caspian Sea
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