'Stratocumulus' diaporamas de présentation

Update on stratocumulus simulations by the UCLA AGCM

Update on stratocumulus simulations by the UCLA AGCM. C. R. Mechoso, I. Richter, G. Cazes, and R. Terra University of California, Los Angeles OUTLINE Sensitivity of Sc incidence to African orography A comparison with similar results for South American orography

432 views • 37 slides

Cloud #1: 5,000 meters high with pretty sunsets!

Cloud #1: 5,000 meters high with pretty sunsets!. Cloud #1: 5,000 meters high with pretty sunsets!. Altocumulus. Cloud #2: 12,000 meters high with curls of hair!. Cloud #2: 12,000 meters high with curls of hair!. Cirrus. Cloud #3: 5,000 meters high and puffy!.

453 views • 36 slides

429 views • 33 slides

TEST #2 Review Slides

TEST #2 Review Slides. Cumulus clouds. Stratocumulus clouds over the Rockies. Stratus clouds. Nimbostratus clouds over the North Sea. Nimbostratus clouds. Altocumulus clouds. Cirrus clouds. Cirrus clouds over Golden Gate Bridge.

590 views • 23 slides

399 views • 23 slides

Clouds

Clouds. 4.02 Analyze the formation of clouds and their relation to weather systems. 5th Grade Science SCOS Objective. Essential Question. What are clouds?. Clouds are made up of millions of tiny droplets of water and ice.

408 views • 22 slides

Entrainment rates in stratocumulus computed from a 1D TKE model

Entrainment rates in stratocumulus computed from a 1D TKE model. Stephan de Roode KNMI. Turbulent mixing and entrainment in simple closure models. Computation of the flux Representation of entrainment rate w e 1. K-profile K = w e D z , w e from parametrization

310 views • 20 slides

Entrainment rates in stratocumulus computed from a 1D TKE model

Entrainment rates in stratocumulus computed from a 1D TKE model. Stephan de Roode KNMI. Turbulent mixing and entrainment in simple closure models. Computation of the flux Representation of entrainment rate w e 1. K-profile K = w e D z , w e from parametrization

207 views • 20 slides

203 views • 12 slides

Parameterization of liquid water path fluctuations in non-precipitating stratocumulus

Stratocumulus albedo bias. Temperature and humidity. Liquid water fluctuations are smaller than total specific humidity fluctuations because of the temperature effect on the saturation specific humidity.

120 views • 1 slides