Atmospheric temperature
; Caves
; Evaporation
; Heat transfer
; Process control
; Surface properties
; Temperature
; Biogeochemical process
; Drip waters
; Ground surface temperature
; Heat transport
; Paleoclimate reconstruction
; Paleoclimates
; Speleometeorology
; Subsurface temperature
; Infiltration
; biogeochemical cycle
; evaporation
; heat transfer
; infiltration
; latent heat flux
; paleoclimate
; speleology
; speleothem
; stalactite
; surface temperature
; thermal regime
; water temperature
; Australia
; New South Wales
; Wellington [New South Wales]
Connected Waters Initiative Research Centre, UNSW Australia, 110 King Street, Manly Vale, Australia; Connected Waters Initiative Research Centre, UNSW Australia, Sydney, NSW, Australia; School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, United Kingdom; Mark Wainwright Analytical Centre, UNSW Australia, Sydney, NSW, Australia; Australian Nuclear Science and Technology Organisation, Lucas HeightsNSW, Australia; SGA Environmental, Suite 8, 599 Pacific Highway, St Leonards, NSW, Australia
Recommended Citation:
Rau G.C.,Cuthbert M.O.,Andersen M.S.,et al. Controls on cave drip water temperature and implications for speleothem-based paleoclimate reconstructions[J]. Quaternary Science Reviews,2015-01-01,127