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- L. Li (LMD/CNRS):
- Atm. as observed
- L. Li (LMD/CNRS):
- Atm. as observed
L. Li (LMD/CNRS): Atm. as observed page 1 Schematic showing the - - PowerPoint PPT Presentation
L. Li (LMD/CNRS): Atm. as observed page 1 Schematic showing the - - PowerPoint PPT Presentation
L. Li (LMD/CNRS): Atm. as observed page 1 Schematic showing the Earths climate system with its five components and the interactions (thin arrows). Thick arrows indicate the possible causes of climate change. L. Li (LMD/CNRS): Atm. as
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SLIDE 3
- L. Li (LMD/CNRS):
- Atm. as observed
page 3 Cloud Climatology
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- L. Li (LMD/CNRS):
- Atm. as observed
page 4 Rainfall climatology
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- L. Li (LMD/CNRS):
- Atm. as observed
page 5 Instantaneous IR and WV images of the atmosphere
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- L. Li (LMD/CNRS):
- Atm. as observed
page 6 Climatology of the atmosphere
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- L. Li (LMD/CNRS):
- Atm. as observed
page 7 Climatology of the atmosphere
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- L. Li (LMD/CNRS):
- Atm. as observed
page 8 Potential temperature θ is the temperature that an unsaturated par- cel of dry air would have if brought adiabatically and reversibly from its initial state to a standard pressure p0, typically 1000 hPa: θ = T(p0 P )R/Cp Equivalent potential temperature θe is found by lowering an air parcel to the 1000 mb level AND releasing the latent heat in the parcel. θe = Te(p0 P )R/Cp ≈ (T + Lq Cp )(p0 P )R/Cp = θ exp(Lq Cp ) where Te is the equivalent temperature.
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- L. Li (LMD/CNRS):
- Atm. as observed
page 9 Climatology of the atmosphere
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- L. Li (LMD/CNRS):
- Atm. as observed
page 10 Climatology of the atmosphere
SLIDE 11
- L. Li (LMD/CNRS):
- Atm. as observed