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A conveyor belt, also referred to as the warm conveyor belt, describes the flow of a stream of warm moist air originating within the warm sector of an extratropical cyclone ahead of the cold front which slopes up above and north of the surface warm front. The idea of the conveyor belt originated in
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precipitation develops north of the warm front along the conveyor belt. Active precipitation north of the warm front implies potential for greater development of the cyclone. A portion of this conveyor belt turns to the right (left in the
Southern Hemisphere), aligning with the upper level
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and warm fronts around the low become better defined. As the low matures, it couples with the upper level disturbance moving into the cyclone's cold sector. The cold front catches up to the westward portion of the warm front, forming an
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263:. The frontal boundary becomes weaker and surrounds the equatorward portion of the cyclone, waiting for the next upper level disturbance to form a new low pressure area.
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1969. The left edge of the conveyor belt is sharp due to the higher density air moving in from the west forcing a sharp slope to the cold front. An area of
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appeared to be focused along these convergence zones. The concept of frontal zones led to the concept of
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will begin to form ahead of the surface low, within the cold sector of the cyclone poleward of the
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A depiction of warm conveyor belt precipitation during a wintertime extratropical cyclone
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84:. This theory proposed that the main inflow into a cyclone was concentrated along two
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develop as they move up and along a frontal boundary, eventually
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A wave along a frontal boundary, in the form of a broad area of
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44:cold environment. It was developed completely from
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24:, developed during and shortly after
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92:or cold front. Areas of clouds and
72:Polar front theory is attributed to
465:Reexamining the Cold Conveyor Belt.
46:surface-based weather observations
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484:Synoptic meteorology and weather
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346:The Norwegian Cyclone Model.
323:The Norwegian Cyclone Model.
222:Dissipating stage of cyclone
199:A mature low pressure system
48:, including descriptions of
30:Bergen School of Meteorology
20:development is known as the
16:The older of the models of
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351:September 1, 2006, at the
328:September 1, 2006, at the
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366:"Norwegian Cyclone Model"
68:Development of the theory
467:Retrieved on 2007-05-17.
463:University of Oklahoma.
451:Retrieved on 2007-05-17.
442:Norwegian cyclone model.
355:Retrieved on 2007-05-17.
344:University of Oklahoma.
332:Retrieved on 2006-10-11.
303:Surface weather analysis
22:Norwegian cyclone model
489:Extratropical cyclones
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370:oceanservice.noaa.gov
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117:Stages of development
110:Extratropical cyclone
18:extratropical cyclone
86:lines of convergence
153:Wave forms on front
32:. In this theory,
447:2016-01-04 at the
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60:above the surface
54:frontal boundaries
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240:low pressure
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440:JetStream.
90:squall line
82:World War I
52:found near
28:within the
26:World War I
478:Categories
309:References
282:stratiform
248:warm front
108:See also:
98:air masses
62:warm front
58:cold front
104:Evolution
38:occluding
445:Archived
422:cite web
349:Archived
326:Archived
297:See also
94:rainfall
34:cyclones
412:10 June
80:during
78:Norway
50:clouds
406:(PDF)
399:(PDF)
428:link
414:2016
382:2023
291:snow
252:cold
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