Past temperatures directly from the greenland ice sheet
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Summary
A Monte Carlo inverse method has been used on the temperature profiles measured down through the Greenland Ice Core Project (GRIP) borehole, at the summit of the Greenland ice Sheet, and the Dye 3 borehole 865 kilometers farther south, resulting in a 50, 000-year-long temperature history at GRIP and a 7000-year history at Dye3.
- Type
- article
- Published
- 1998-10-09
- Cited by
- 1,058
- References
- 24
- OpenAlex
- https://openalex.org/W2014688144
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:30298901
Keywords
Greenland ice sheet, Geology, Ice core, Ice sheet, Groenlandia
References
- Bore-Hole Survey at Dye 3, South Greenland
- Resolving the Younger Dryas event through borehole thermometry
- A new high-precision borehole-temperature logging system used at GISP2, Greenland, and Taylor Dome, Antarctica
- A search in north Greenland for a new ice-core drill site
- Heat flow from the Earth's interior: Analysis of the global data set
- HEAT FLOW AND SURFACE RADIOACTIVITY AT TWO SITES IN SOUTH GREENLAND.
- Palaeotemperatures still exist in the Greenland ice sheet
- Bore-hole survey at dome GRIP 1991
- Resolution analysis of general inverse problems through inverse Monte Carlo sampling
- Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition
- Aspects of climate variability in the North Atlantic sector: Discussion and relation to the Greenland Ice Sheet Project 2 high‐resolution isotopic signal
- Large Arctic Temperature Change at the Wisconsin-Holocene Glacial Transition
- Greenland Ice Sheet History Since the Last Glaciation
- The climate signal in the stable isotopes of snow from Summit, Greenland: Results of comparisons with modern climate observations
- Monte Carlo sampling of solutions to inverse problems
- Arctic Environmental Change of the Last Four Centuries
- Greenland palaeotemperatures derived from GRIP bore hole temperature and ice core isotope profiles
- Decadal Trends in the North Atlantic Oscillation: Regional Temperatures and Precipitation
- The extent of temporal smearing in surface-temperature histories derived from borehole temperature measurements
- ATMOSPHERE WEATHER & CLIMATE
Cited by
- Holocene glacial history of Renland Ice Cap, East Greenland, reconstructed from lake sediments
- VARIABILITÉ CLIMATIQUE RAPIDE EN ATLANTIQUE NORD : L'APPORT DES ISOTOPES DE L'AIR PIÉGÉ DANS LA GLACE DU GROENLAND
- Late Quaternary ice-ocean interactions in central West Greenland
- Gulf Stream density structure and transport during the past millennium
- Reconciling glacial Antarctic water stable isotopes with ice sheet topography and the isotopic paleothermometer
- ‘Dark Age Economics’ revisited: the English fish bone evidence AD 600-1600
- Paleontology in Ecology and Conservation
- Using sea-level data to constrain the contribution of the Greenland ice sheet to contemporary and recent sea-level change
- Paleoclimatic reconstructions based on borehole temperature measurements in ice sheets : possibilities and limitations
- Simulating the evolution of the Arctic climate during the last millenium.
- A Holocene palaeoceanographic multi-proxy study on the variability of Atlantic water inflow and sea ice distribution along the pathway of Atlantic water
- Long Term Climate Records from Polar Ice
- The postglacial environmental development of Raffles Sø, East Greenland: inferences from a 10,000 year diatom record
- Lake Diatoms as a Proxy for Holocene Environmental Change, West Greenland
- Climate change and the Viking-age fjord environment of the Eastern Settlement, South Greenland
- Principles of Glacier Mechanics
- К обоснованию понятия «личностно значимый выбор»
- Contraintes chronologiques et biogéochimiques grâce au méthane dans la glace naturelle : une application aux forages du projet EPICA
- Ice-atmosphere interactions in the Canadian high Arctic: implications for the thermo-mechanical evolution of terrestrial ice masses
- Paleoclimate on the Kola Peninsula (Russia) From Inversion of Subsurface Temperatures: Role of Weichselian Glaciation
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