'Saturation ratio' diaporamas de présentation

Formation of Cloud Droplets

1.28k views • 121 slides

Why the aerosol are important for clouds and Why clouds are important for the aerosol Jeff Snider

Why the aerosol are important for clouds and Why clouds are important for the aerosol Jeff Snider University of Wyoming, Laramie jsnider@uwyo.edu. Outline - Basic physics of cloud/aerosol and aerosol/cloud interactions Properties of aerosol particles that make them good nuclei

424 views • 42 slides

Coagulation

Coagulation. Reading: Chap 12. PbO-SiO 2 -PbSiO 3 composite. AEROSIL from Degussa, Inc. Q: How is rain droplet formed? Why is it larger in a thunderstorm? .

769 views • 29 slides

CCN predictions and and the role of organics

CCN predictions and and the role of organics. Development of a simple model predicting Cloud Condensatio n Nuclei concentrations, CCN Applying the model on data from CLAIRE 2001 Hygroscopic measurements on some organics (laboratory data). Jenny Rissler, Aerosolgroup, Lund University.

241 views • 16 slides

Primer for Skew-T Diagram Use In Atmospheric Thermodynamics

. Primer for Skew-T Diagram Use In Atmospheric Thermodynamics. Location of Chart Lines Saturation Point. Table of Contents. 600 700 800 900 1000. The Skew-T diagram contains multiple parameters to calculate thermodynamic variables. They include: Pressure - p (mb).

191 views • 14 slides

Arctic Aerosol Size Distributions Schematic Picture

Arctic Aerosol Size Distributions Schematic Picture. Number Surface Volume/Mass. Hoppel Minimum. (Ice crystals). Particle Diameter (Dry / Wet ). 20 n m. 80 n m. 1 ? m. 10 ? m. UCPC ? --------------------------------------------------------------------------- ?.

221 views • 12 slides