Matches in SemOpenAlex for { <https://semopenalex.org/work/W300463197> ?p ?o ?g. }
- W300463197 endingPage "36" @default.
- W300463197 startingPage "19" @default.
- W300463197 abstract "While several studies explore cave climate and thermal regimes, little is known about the controls on cave drip water temperature. Yet water temperature significantly influences biogeochemical processes associated with cave drips. To identify the processes that control the cave drip water temperature, we measured the temperatures at multiple locations along a speleothem flow path and drip sources (stalactites) concurrently with the drip rates in Cathedral Cave, Wellington, Australia. We monitored long-term drip water temperature, drip rates, surface and cave climate and in-cave evaporation rates and conducted 3 infiltration experiments with different flow, temperature and isotopic conditions. Our results show that the drip water temperature is controlled by multiple superimposed heat transport mechanisms that act upon the infiltrating water in the epikarst, the water film after it enters the cave and before it becomes a drip. The two main heat sources/sinks for drip water are the cave air and the surrounding rock. The subsurface temperature is coupled to the surface temperature by conduction through the soil and rock mass, but the cave climate is also coupled to the surface climate by venting. On a regional scale, drip temperatures are mainly driven by the annual ground surface temperature signal but damped with depth and shifted in time compared to the surface. On a local scale, the drip water temperature can differ significantly from cave air and speleothem temperature due to the latent heat exchange of evaporation and localised water film convection. The main controls are ground surface temperature, subsurface depth, air density induced ventilation, distance from entry and drip rate. We present a conceptual model that explains drip water temperature signals and provide signal driven guidance on best type and location for speleothem sampling. We anticipate that our results will significantly improve the understanding of temperature-dependent paleoclimate signals from speleothem archives." @default.
- W300463197 created "2016-06-24" @default.
- W300463197 creator A5001806211 @default.
- W300463197 creator A5002080802 @default.
- W300463197 creator A5004054166 @default.
- W300463197 creator A5005344720 @default.
- W300463197 creator A5024368072 @default.
- W300463197 creator A5024549797 @default.
- W300463197 creator A5042689834 @default.
- W300463197 creator A5058239798 @default.
- W300463197 creator A5059602657 @default.
- W300463197 creator A5086165069 @default.
- W300463197 date "2015-11-01" @default.
- W300463197 modified "2023-10-18" @default.
- W300463197 title "Controls on cave drip water temperature and implications for speleothem-based paleoclimate reconstructions" @default.
- W300463197 cites W1530742546 @default.
- W300463197 cites W1557491957 @default.
- W300463197 cites W1660454357 @default.
- W300463197 cites W1964060420 @default.
- W300463197 cites W1964470428 @default.
- W300463197 cites W1971910917 @default.
- W300463197 cites W1983353374 @default.
- W300463197 cites W1983674049 @default.
- W300463197 cites W1984209532 @default.
- W300463197 cites W1988801873 @default.
- W300463197 cites W2001191033 @default.
- W300463197 cites W2001789335 @default.
- W300463197 cites W2004587064 @default.
- W300463197 cites W2005441843 @default.
- W300463197 cites W2005911067 @default.
- W300463197 cites W2006207974 @default.
- W300463197 cites W2010904233 @default.
- W300463197 cites W2016964152 @default.
- W300463197 cites W2017913935 @default.
- W300463197 cites W2020505016 @default.
- W300463197 cites W2023766611 @default.
- W300463197 cites W2025476990 @default.
- W300463197 cites W2025504179 @default.
- W300463197 cites W2029634609 @default.
- W300463197 cites W2034718423 @default.
- W300463197 cites W2041743483 @default.
- W300463197 cites W2046487099 @default.
- W300463197 cites W2051973454 @default.
- W300463197 cites W2056035882 @default.
- W300463197 cites W2061053358 @default.
- W300463197 cites W2063009391 @default.
- W300463197 cites W2068599282 @default.
- W300463197 cites W2069311181 @default.
- W300463197 cites W2072604141 @default.
- W300463197 cites W2074912297 @default.
- W300463197 cites W2078022896 @default.
- W300463197 cites W2081701626 @default.
- W300463197 cites W2083265220 @default.
- W300463197 cites W2083702468 @default.
- W300463197 cites W2088278431 @default.
- W300463197 cites W2090992138 @default.
- W300463197 cites W2091031409 @default.
- W300463197 cites W2102004532 @default.
- W300463197 cites W2129693144 @default.
- W300463197 cites W2132027636 @default.
- W300463197 cites W2133060148 @default.
- W300463197 cites W2139404099 @default.
- W300463197 cites W2147401205 @default.
- W300463197 cites W2147972288 @default.
- W300463197 cites W2152546202 @default.
- W300463197 cites W2153175030 @default.
- W300463197 cites W2156771808 @default.
- W300463197 cites W2165696439 @default.
- W300463197 cites W4233334897 @default.
- W300463197 doi "https://doi.org/10.1016/j.quascirev.2015.03.026" @default.
- W300463197 hasPublicationYear "2015" @default.
- W300463197 type Work @default.
- W300463197 sameAs 300463197 @default.
- W300463197 citedByCount "29" @default.
- W300463197 countsByYear W3004631972015 @default.
- W300463197 countsByYear W3004631972016 @default.
- W300463197 countsByYear W3004631972017 @default.
- W300463197 countsByYear W3004631972018 @default.
- W300463197 countsByYear W3004631972019 @default.
- W300463197 countsByYear W3004631972020 @default.
- W300463197 countsByYear W3004631972021 @default.
- W300463197 countsByYear W3004631972022 @default.
- W300463197 countsByYear W3004631972023 @default.
- W300463197 crossrefType "journal-article" @default.
- W300463197 hasAuthorship W300463197A5001806211 @default.
- W300463197 hasAuthorship W300463197A5002080802 @default.
- W300463197 hasAuthorship W300463197A5004054166 @default.
- W300463197 hasAuthorship W300463197A5005344720 @default.
- W300463197 hasAuthorship W300463197A5024368072 @default.
- W300463197 hasAuthorship W300463197A5024549797 @default.
- W300463197 hasAuthorship W300463197A5042689834 @default.
- W300463197 hasAuthorship W300463197A5058239798 @default.
- W300463197 hasAuthorship W300463197A5059602657 @default.
- W300463197 hasAuthorship W300463197A5086165069 @default.
- W300463197 hasBestOaLocation W3004631972 @default.
- W300463197 hasConcept C127313418 @default.
- W300463197 hasConcept C152453397 @default.
- W300463197 hasConcept C159390177 @default.