Hypsithermal period: Difference between revisions
From Glossary of Meteorology
imported>Perlwikibot (Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == hypsithermal period == </div> <div class="definition"><div class="short_definition">The per...") |
imported>Perlwikibot No edit summary |
||
| Line 9: | Line 9: | ||
</div> | </div> | ||
<div class="definition"><div class="short_definition">The period from about 7000 to 500 B.C., proposed by E. S. Deevey and R. F. Flint (1957), during which global [[climate]] was thought to be warmer than today.</div><br/> <div class="paragraph">Spanning the [[Boreal]] through [[SubBoreal]] periods of the Blytt–Sernander sequence of inferred climates in northern Europe, it includes both wet and dry periods. It is followed by the general expansion of [[glaciers]] known as the [[Neoglacial]].</div><br/> </div><div class="reference">Deevey, E. S., and R. F. Flint 1957. Postglacial hypsithermal interval. Science. 125. 183–184. </div><br/> <div class="reference">Sernander, R. 1908. On the evidence of postglacial changes of climate furnished by the peat-mosses of northern Europe. Geol. F& | <div class="definition"><div class="short_definition">The period from about 7000 to 500 B.C., proposed by E. S. Deevey and R. F. Flint (1957), during which global [[climate]] was thought to be warmer than today.</div><br/> <div class="paragraph">Spanning the [[Boreal]] through [[SubBoreal]] periods of the Blytt–Sernander sequence of inferred climates in northern Europe, it includes both wet and dry periods. It is followed by the general expansion of [[glaciers]] known as the [[Neoglacial]].</div><br/> </div><div class="reference">Deevey, E. S., and R. F. Flint 1957. Postglacial hypsithermal interval. Science. 125. 183–184. </div><br/> <div class="reference">Sernander, R. 1908. On the evidence of postglacial changes of climate furnished by the peat-mosses of northern Europe. Geol. Fören. Förh.. 30. 456–478. </div><br/> | ||
</div> | </div> | ||
Latest revision as of 15:26, 20 February 2012
hypsithermal period
The period from about 7000 to 500 B.C., proposed by E. S. Deevey and R. F. Flint (1957), during which global climate was thought to be warmer than today.
Spanning the Boreal through SubBoreal periods of the Blytt–Sernander sequence of inferred climates in northern Europe, it includes both wet and dry periods. It is followed by the general expansion of glaciers known as the Neoglacial.
Deevey, E. S., and R. F. Flint 1957. Postglacial hypsithermal interval. Science. 125. 183–184.
Sernander, R. 1908. On the evidence of postglacial changes of climate furnished by the peat-mosses of northern Europe. Geol. Fören. Förh.. 30. 456–478.
