| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
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| rdfs:comment
| - __NOEDITSECTION__ __NOWYSIWYG__
- A trough is an elongated region of relatively low atmospheric pressure, often associated with fronts. Unlike fronts, there is not a universal symbol for a trough on a weather chart. The weather charts in some countries or regions mark troughs by a line. In the United States, a trough may be marked as a dashed line. In the UK, Hong Kong or Fiji, it is represented by a bold line extended from a low pressure center or between two low pressure centers; in Macau or Australia, it is a dotted line. If it is not marked, troughs may still be identified as an extension of isobars away from a low pressure center.
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| sameAs
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| dcterms:subject
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| itemid
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| droppedBy
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| marketable
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| itemclass
| - Household Items
- Household Items
- Household Items
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| secondarytype
| |
| attrib
| - Hold liquid, not pickupable, not walkable.
|
| buyfrom
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| npcvalue
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| actualname
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| npcprice
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| sellto
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| walkable
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| usable
| |
| pickupable
| |
| primarytype
| - Fluid Containers
- Fluid Containers
- Containers
|
| dbkwik:es.tibia/pr...iPageUsesTemplate
| |
| dbkwik:sv.tibia/pr...iPageUsesTemplate
| |
| dbkwik:tibia/prope...iPageUsesTemplate
| |
| Article
| |
| Name
| |
| Value
| - 0(xsd:integer)
- Negotiable
- Negotiable
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| Weight
| - N/A
- in Furniture package; 30
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| dbkwik:weather/pro...iPageUsesTemplate
| |
| plural
| |
| Notes
| - Can hold Liquids. These can be seen in stables, camps, and other places with animals.
- Can be obtained by unpacking a Trough Kit. Can be seen in stables, camps and other places with animals.
- Can be seen in stables, camps and other places with animals.
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| destructible
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| holdsliquid
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| abstract
| - __NOEDITSECTION__ __NOWYSIWYG__
- A trough is an elongated region of relatively low atmospheric pressure, often associated with fronts. Unlike fronts, there is not a universal symbol for a trough on a weather chart. The weather charts in some countries or regions mark troughs by a line. In the United States, a trough may be marked as a dashed line. In the UK, Hong Kong or Fiji, it is represented by a bold line extended from a low pressure center or between two low pressure centers; in Macau or Australia, it is a dotted line. If it is not marked, troughs may still be identified as an extension of isobars away from a low pressure center. Sometimes, the region between two high pressure centers may assume the character of a trough when there is a detectable wind shift noted at the surface. In the absence of a wind shift, the region is designated a col, akin to a geographic saddle between two mountain peaks. 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. 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. In the mid-latitude westerlies, troughs and ridges often alternate, especially when upper-level winds are in a high-amplitude pattern. For a trough in the westerlies, the region just west of the trough axis is typically an area of convergent winds and descending air - and hence high pressure - while the region just east of the trough axis is an area of fast, divergent winds and low pressure. Tropical waves are a type of trough in easterly currents, a cyclonic northward deflection of the trade winds.
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![[RDF Data]](/fct/images/sw-rdf-blue.png)