Yahoo Web Search

Search results

    • Elongated area of low atmospheric pressure

      Image courtesy of pinterest.com

      pinterest.com

      • A trough is an elongated area of low atmospheric pressure, often associated with the movement of weather systems and mid-latitude cyclones. It typically represents a region where air is converging and rising, leading to cloud formation and precipitation.
  1. People also ask

  2. Sep 29, 2024 · Quick Reference. 1 An extension of low atmospheric pressure from the central regions of a low-pressure system into a zone where generally higher pressure prevails. The term ‘trough’ is also, and in accordance with this definition, applied to equatorward meanders of the flow of the upper westerly winds over middle latitudes. (The ...

  3. In geology, a trough is a linear structural depression that extends laterally over a distance. Although it is less steep than a trench, a trough can be a narrow basin or a geologic rift. These features often form at the rim of tectonic plates.

  4. Aug 9, 2024 · Learn about the formation of glacial landforms from corries to troughs, along with examiner tips and worked examples for the AQA GCSE Geography exam.

  5. In geology, a trough refers to a linear depression that extends in one direction over a distance. It is less steep than a trench. A trough can be a narrow basin or a geologic rift. There are various oceanic troughs, troughs found under oceans; examples include the rifts along the mid-ocean ridges

  6. standing wave, combination of two waves moving in opposite directions, each having the same amplitude and frequency. The phenomenon is the result of interference; that is, when waves are superimposed, their energies are either added together or canceled out.

  7. Definition. A trough is an elongated area of low atmospheric pressure, often associated with the movement of weather systems and mid-latitude cyclones. It typically represents a region where air is converging and rising, leading to cloud formation and precipitation.

  8. Trough –rillepit systems occur scattered in the northern Gordii region (Fig. 4.11A), parallel to the Olympica 1–3 channels on both sides, and on the banks of central Olympica Fossa.

  1. People also search for