Dew forms as the temperature drops to the dew point. Water droplets love to collect on surfaces or tiny particles. It is very difficult for water drop.
Haze Hygroscopic aerosols Wet Haze with less than 75 % RH Condensation nuclei needed to form fog or cloud Hydrophobic aerosols.
Weather Forecasting Information Courtesy of: University of Illinois at Urbana-Champaign (Gh)/guides/mtr/fcst/home.rxml)Gh)/guides/mtr/fcst/home.rxml.
Chapter 7- Synoptic climatology Instantaneous climatological conditions a snap shot of what the climate is like at some point in time Typically used in.
Chapter 15 Global Circulation: Big Picture: Idealized View Ferrel cell Polar cell.
Air
Weather Forecasting Guide Forecasting Temperatures Forecasting Precipitation Reading Weather Maps.
Air Masses and Severe Weather
How to “Grow” a Storm
Air Chapter 12. What Causes Air Pollution 1273- King Edward I banned burning lignite (a form of dirty coal) because of air pollution. Air pollution-
How to “Grow” a Storm Upper level shortwave passes Upper level divergence -> sfc low Cold advection throughout lower troposphere Cold advection intensifies.
Air Masses and Fronts What’s the difference?. Air Mass O An air mass is a large volume of air with the same temperature and moisture content. O As an.
