Search results
Results from the WOW.Com Content Network
Stationary front symbol: solid line of alternating blue spikes pointing to the warmer air mass and red domes pointing to the colder air mass. A stationary front (or quasi-stationary front) is a weather front or transition zone between two air masses when each air mass is advancing into the other at speeds less than 5 knots (about 6 miles per hour or about 9 kilometers per hour) at the ground ...
Description: Weather fronts cold front; warm front; stationary front; occluded front; surface trough; squall line; dry line; tropical wave; trowal (Trough of warm air aloft by Canadian Avalanche Association and World Meteorological Organisation)
Stationary fronts either dissipate after several days or devolve into shear lines, but they can transform into a cold or warm front if the conditions aloft change. Stationary fronts are marked on weather maps with alternating red half-circles and blue spikes pointing opposite to each other, indicating no significant movement.
The following other wikis use this file: Usage on ca.wikipedia.org Front estacionari; Usage on cs.wikipedia.org Wikipedista:-xfi-/tvorba; Usage on de.wikipedia.org
Add context and color to your emails for a more professional, impactful, or fun presentation whether you're sending a fun pick-me-up message or a professional resume, adding Stationery to your email is the perfect way to brighten up any message. 1. Click Compose to start a new message. 2. Click Add Stationery. 3. Select a stationery template. 4.
Main page; Contents; Current events; Random article; About Wikipedia; Contact us
You can customize your emails, allowing them to stand out from the rest. Features include adding custom backgrounds, flowing text, and more. For instance, under "Get Well", you can choose a "Get Well Soon" template to send it to a friend. 1. Sign in to Desktop Gold. 2. Click Write in the upper left. 3. At the top, click the Extras menu | select ...
A stationary front is a non-moving boundary between two different air masses. They tend to remain in the same area for long periods of time, sometimes undulating in waves. [ 29 ] Often a less-steep temperature gradient continues behind (on the cool side of) the sharp frontal zone with more widely spaced isotherms.