Search results
Results from the WOW.Com Content Network
The MM5 (short for Fifth-Generation Penn State/NCAR Mesoscale Model) is a regional mesoscale model used for creating weather forecasts and climate projections. It is a community model maintained by Penn State University and the National Center for Atmospheric Research .
In 1965 Harrisburg Commuter began flights from State College to Harrisburg, two flights each weekday; the 1965 Official Airlines Guide does not state which airport they served, but starting in 1978 Allegheny Commuter flights were at University Park. Penn State assumed the lease and assets of the airport in 1972. [4]
A difference in air pressure causes an air displacement and generates the wind. The Coriolis force deflects the air movement to the right in the northern hemisphere and the left in the southern one, which makes the winds parallel to the isobars on an elevation in pressure card. [1]
Penn State-West Virginia weather forecast According to The Weather Channel, thunderstorms are possible around 2:30 p.m. ET. Thunderstorms are expected to continue through 9 p.m. ET, which could ...
Due to the baroclinic density field, the Alaska current is highly sheared vertically, and the cross-current density gradient is reflected by the offshore salinity gradient. The surface salinities are less than 30 PSU (Practical Salinity Unit) at the coastal areas, more than 31 PSU on the shelf, and more than 32.5 PSU in the central Gulf of Alaska.
Zonal and meridional flow are directions and regions of fluid flow on a globe. Zonal flow follows a pattern along latitudinal lines, latitudinal circles or in the west–east direction. [ 1 ] Meridional flow follows a pattern from north to south, or from south to north, along the Earth's longitude lines, longitudinal circles ( meridian ) or in ...
ahead of an upper-ridge, the airflow that comes from the polar regions and brings cold air. behind the upper-ridge line, the flow that comes from the equator and brings mild air. Surface ridges, just like highs, generate fair weather because they develop under wind convergence in the negative vorticity advection zone ahead of the upper-level ...
Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!