Holocene climatic optimum

GPTKB entity

Statements (29)
Predicate Object
gptkbp:instanceOf climate period
gptkbp:affectedArea gptkb:Africa
gptkb:Asia
gptkb:Europe
gptkb:Northern_Hemisphere
gptkb:Arctic
gptkbp:alsoKnownAs gptkb:Altithermal
gptkb:Holocene_Thermal_Maximum
gptkb:Hypsithermal
gptkbp:causedBy orbital forcing
gptkbp:characterizedBy expansion of forests in northern latitudes
increased precipitation in some regions
warmer temperatures than present
gptkbp:endDate circa 5,000 years BP
gptkbp:followedBy gptkb:Neoglaciation
https://www.w3.org/2000/01/rdf-schema#label Holocene climatic optimum
gptkbp:notableEvent Sahara was greener and wetter
expansion of boreal forests
higher lake levels in Africa
reduction of Arctic sea ice
retreat of glaciers
gptkbp:partOf gptkb:Holocene_epoch
gptkbp:precededBy gptkb:Younger_Dryas
gptkbp:relatedTo archaeology
climate change research
paleoclimatology
gptkbp:startDate circa 9,000 years BP
gptkbp:bfsParent gptkb:Quaternary_period
gptkbp:bfsLayer 6