Pluvial: Difference between revisions
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{{Short description|Climate or climatological period climate characterized by relatively high precipitation}} |
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{{Expand German|Pluvial|date=May 2014}} |
{{Expand German|Pluvial|date=May 2014}} |
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{{distinguish|text=the [[Cope|pluviale]], a liturgical vestment}} |
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In [[geology]] and [[climatology]], a '''pluvial''' is either a modern [[climate]] characterized by relatively high [[precipitation]] |
In [[geology]] and [[climatology]], a '''pluvial''' is either a modern [[climate]] characterized by relatively high [[precipitation]] or an interval of time of variable length, decades to thousands of years, during which a climate is characterized by relatively high precipitation or humidity. Subdivisions of a pluvial, which are characterized by relatively high precipitation, are known as a '''subpluvials'''. Formally, pluvials were equated with [[glacial]] stages of the [[Quaternary]]. However, pluvials, as in equatorial regions, can also occur during [[interglacial]] stages. No lower latitudes have experienced major pluvials in early to mid-[[Holocene]] times. |
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In [[geomorphology]], pluvial refers to a geologic episode, change, process, deposit, or feature that is the result of the action or effects of rain. Sometimes it also refers to the [[fluvial]] action of rainwater flowing in a stream channel, including a flood, known as a '''pluvial flood''', that is the direct result of excessive precipitation.<ref name="Bradley2015a">Bradley, R.S. (2015) ''Paleoclimatology: reconstructing climates of the Quaternary.'' (3r ed.). Boston, Massachusetts, Academic Press 696 pp. {{ISBN|978-0-12-386913-5}}</ref><ref name="NeuendorfOthers2005a">Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. {{ISBN|0-922152-76-4}}</ref> |
In [[geomorphology]], a pluvial refers to a geologic episode, change, process, deposit, or feature that is the result of the action or effects of rain. Sometimes, it also refers to the [[fluvial]] action of rainwater flowing in a stream channel, including a flood, known as a '''pluvial flood''', that is the direct result of excessive precipitation.<ref name="Bradley2015a">Bradley, R.S. (2015) ''Paleoclimatology: reconstructing climates of the Quaternary.'' (3r ed.). Boston, Massachusetts, Academic Press 696 pp. {{ISBN|978-0-12-386913-5}}</ref><ref name="NeuendorfOthers2005a">Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. {{ISBN|0-922152-76-4}}</ref> |
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==See also== |
==See also== |
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{{Wiktionary|pluvial}} |
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*[[African pluvial periods]] |
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*[[Abbassia Pluvial]] |
*[[Abbassia Pluvial]] |
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*[[Carnian Pluvial Event]] |
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*[[Mousterian Pluvial]] |
*[[Mousterian Pluvial]] |
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*[[Neolithic Subpluvial]] |
*[[Neolithic Subpluvial]] |
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==References== |
==References== |
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==External links== |
==External links== |
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*[https://books.google.com/books?id=8OKPBAAAQBAJ |
*[https://books.google.com/books?id=8OKPBAAAQBAJ&dq=abbassia+gravel&pg=PA59 ''The Geological Evolution of the River Nile'', by Rushdi Said] |
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[[Category:Climate]] |
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[[Category:Climatology]] |
[[Category:Climatology]] |
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[[Category:History of climate variability and change]] |
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[[Category:Prehistoric Africa]] |
[[Category:Prehistoric Africa]] |
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{{Geology-stub}} |
{{Geology-stub}} |
Latest revision as of 03:17, 19 April 2024
You can help expand this article with text translated from the corresponding article in German. (May 2014) Click [show] for important translation instructions.
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In geology and climatology, a pluvial is either a modern climate characterized by relatively high precipitation or an interval of time of variable length, decades to thousands of years, during which a climate is characterized by relatively high precipitation or humidity. Subdivisions of a pluvial, which are characterized by relatively high precipitation, are known as a subpluvials. Formally, pluvials were equated with glacial stages of the Quaternary. However, pluvials, as in equatorial regions, can also occur during interglacial stages. No lower latitudes have experienced major pluvials in early to mid-Holocene times.
In geomorphology, a pluvial refers to a geologic episode, change, process, deposit, or feature that is the result of the action or effects of rain. Sometimes, it also refers to the fluvial action of rainwater flowing in a stream channel, including a flood, known as a pluvial flood, that is the direct result of excessive precipitation.[1][2]
See also
[edit]- African pluvial periods
- Abbassia Pluvial
- Carnian Pluvial Event
- Mousterian Pluvial
- Neolithic Subpluvial
- Pluvial lake
References
[edit]- ^ Bradley, R.S. (2015) Paleoclimatology: reconstructing climates of the Quaternary. (3r ed.). Boston, Massachusetts, Academic Press 696 pp. ISBN 978-0-12-386913-5
- ^ Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) Glossary of Geology (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. ISBN 0-922152-76-4
External links
[edit]