Climate oscillations as recorded in Svalbard ice core δO 18 records between AD 1200 and 1997
Arctic Region ; Climate ; Climate oscillation ; Climatic trend ; Cold area ; Ice core ; Isotope analysis ; Oxygen 18 ; Spitsbergen ; Svalbard ; Temperature
The AA. apply 2 different time series analytical tools to δ O 18 records from 2 Svalbard ice cores. One ice core is from Lomonosovfonna at 1250 m a.s.l. and the other from Austfonna at 750 m a.s.l. These cores are estimated to cover at least