THERMAL SOARING FORECASTING Richard Kellerman [email protected] .
Process Lapse Rates When air rises it is depressurized and expands. As a result its temperature falls. When unsaturated air rises, its rate of cooling.
Atmospheric Thermodynamics – III Adiabatic Processes Leila M. V. Carvalho Dept. Geography, UCSB.
1 Buoyancy driven turbulence in the atmosphere Stephan de Roode (TU Delft) Applied Physics Department Clouds, Climate and Air Quality [email protected].
Lecture 13: Map discussion + Cloud development and forms (Ch 6) Quiz 2 next Friday 13 Oct covers to end of Ch. 6 map discussion (situation of Thurs 5 Oct)
ATS 351 ATS 351 Lecture 6 Stability & Skew-T Diagrams.
Quasi-geostrophic theory (Continued) John R. Gyakum.
AOSS 321, Winter 2009 Earth Systems Dynamics Lecture 13 2/19/2009 Christiane Jablonowski Eric Hetland [email protected]@umich.edu [email protected]@umich.edu.
Looking east toward Santa Ana Canyon along US-91 Santa Ana Winds.
1 Lake-Effect Snow (LES). 2 Overview of the Lake-Effect Process n Occurs to the lee of the Great Lakes during the cool season n Polar/arctic air travels.
AOSS 321, Winter 2009 Earth Systems Dynamics Lecture 13 2/19/2009
youtube/watch?v=2mTLO2F_ERY