Roughness Sublayer Turbulence in the Community Land ... - cmmap

ePAPER READ

DOWNLOAD ePAPER

cmmap.org

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

START NOW

Comparison with observa6ons -‐ scalar profiles

unstable ~neutral stable

Similar agreement for water vapor concentra6on but not for CO 2 concentra6on

Harman and Finnigan (2008)

How can freezing make something warmer? - Little Shop of Physics

Eddy-diffusivity/Mass-flux PBL parameterization: Dry ... - cmmap

A moist static energy budget analysis of the MJO in the ... - cmmap

Modeling the West African Monsoon - cmmap

Table 1- Relative humidities as a function of temperature ... - cmmap

Convection-Resolving Forecasting with the WRF Model - cmmap

How does the general circulation of the atmosphere ... - cmmap

Climate during the Paleocene-Eocene Thermal Maximum ... - cmmap

Focus on deep and shallow convection, and turbulence - cmmap

What's the difference between weather and climate? - Little Shop of ...

Comparison with observa6ons -‐ scalar profiles unstable ~neutral stable Similar agreement for water vapor concentra6on but not for CO 2 concentra6on Harman and Finnigan (2008)

RSL impact on CLM4 surface fluxes (diurnal cycle) • Howland Forest, ME • Average over the 1996 growing season -‐ DOY 153 to 244 • Offline simula6on -‐ driven by observa6ons • Currently only modifying above-canopy flux-‐gradient rela6onships

Page 1 and 2: Roughness Sublayer Turbulence in
Page 3 and 4: Theory for canopy-‐structure
Page 5 and 6: Comparison with observa6ons - N
Page 7: Comparison with observa6ons -
Page 11 and 12: RSL impact on CLM4 surface flu
Page 13 and 14: Summary and Conclusions • Intr

Roughness Sublayer Turbulence in the Community Land ... - cmmap

Create successful ePaper yourself

Delete template?

Save as template?