FACTOID # 6: Clipperton Island wins our prize for the most unusual looking country.
 
 Home   Encyclopedia   Statistics   Countries A-Z   Flags   Maps   Education   Forum   FAQ   About 
 
WHAT'S NEW
RECENT ARTICLES
More Recent Articles »
 

SEARCH ALL

FACTS & STATISTICS   

Search encyclopedia, statistics and forums:

 

 

(* = Graphable)

 

 


Encyclopedia > Trough (meteorology)

A trough is an elongated region of relatively low atmospheric pressure, often associated with fronts. diurnal (daily) rhythm of air pressure in northern Germany (black curve is air pressure) Atmospheric pressure is the pressure above any area in the Earths atmosphere caused by the weight of air. ... A guide to the symbols for weather fronts that may be found on a weather map: 1. ...


If a trough forms in the mid-latitudes, a temperature difference between two sides of the trough usually exists in the form of a weather front. A weather front is usually less convective than a trough in the tropics or subtropics (such as a tropical wave). Sometimes, collapsed frontal systems will degenerate into troughs. A guide to the symbols for weather fronts that may be found on a weather map: 1. ... Tropical waves, also known as easterly waves, are elongated areas of relatively low air pressure, oriented north to south, causing areas of cloudiness and thunderstorms. ...


Convective cells may develop in the vicinity of troughs and give birth to a tropical cyclone. Some tropical or subtropical regions such as the Philippines or south China are greatly affected by convection cells along a trough. Cyclone Catarina, a rare South Atlantic tropical cyclone viewed from the International Space Station on March 26, 2004. ...


The weather charts in some countries or regions mark troughs by a line. In Hong Kong or Fiji, it is represented by a bold line extended from a low pressure center [1] or between two low pressure centers [2]; in Macau, it is a dotted line.


Sometimes, a trough may be a region between two high pressure centers and there is not a low pressure center. In this case, it is still represented by a line between the two high pressure centers.


In United States, a trough may be marked as a brown dashed line. If it is not marked, troughs may still be identified as an extension of isobars away from a low pressure center. A pressure system is a region of the Earths atmosphere where air pressure is unusually high or low. ...


See also


  Results from FactBites:
 
Trough (meteorology) - Wikipedia, the free encyclopedia (257 words)
A trough is an elongated region of relatively low atmospheric pressure, often associated with fronts.
If a trough forms in the mid-latitudes, a temperature difference between two sides of the trough usually exists in the form of a weather front.
A weather front is usually less convective than a trough in the tropics or subtropics (such as a tropical wave).
Mauna Kea Weather Center Glossary/Dictionary (1307 words)
To the west of the trough line in an easterly wave over the ocean, there is generally found divergence, a shallow moist layer, and exceptionally fine weather.
The moist layer rises rapidly near the trough line; in and to the east of the trough line intense convergence, much cloudiness, and heavy rain showers prevail.
In meteorology, the mixing of environmental air into a preexisting organized air current so that the environmental air becomes part of the current; the opposite of detrainment.
  More results at FactBites »

 

COMMENTARY     


Share your thoughts, questions and commentary here
Your name
Your location
Your comments
Please enter the 5-letter protection code


Lesson Plans | Student Area | Student FAQ | Reviews | Press Releases |  Feeds | Contact
The Wikipedia article included on this page is licensed under the GFDL.
Images may be subject to relevant owners' copyright.
All other elements are (c) copyright NationMaster.com 2003-5. All Rights Reserved.
Usage implies agreement with terms.