The temporal variation of accumulation and temperature in the Siberian Altai were
investigated using a 86 m long ice core from Belukha glacier (49° 48′ 26 ″N, 86° 34′ 43 …

During summer 2001, a 140 m long ice core was recovered from the Belukha glacier (49°
48′ 26 ″N, 86° 34′ 43 ″E, 4062 m asl) in the Siberian Altai. The englacial temperature …

For the first time we present a multi-proxy data set for the Russian Altai, consisting of
Siberian larch tree-ring width (TRW), latewood density (MXD), δ 13 C and δ 18 O in …

A 20 km wide zone of fast ice, reaching offshore to the 20 m isobath and sealing off coastal
embay ments along the Taymyr Peninsula, survived until at least 23 November 1 993 …

In the summers of 2001 and 2002, glacio-climatological research was performed at 4110–
4120 m asl on the Belukha snow/firn plateau, Siberian Altai. Hundreds of samples from …

A multiple parameter dating technique was used to establish a depth/age scale for a 171.3
m (145.87 m we) surface to bedrock ice core (Bl2003) recovered from the cold …

In July 2001, a 140 m long ice core was recovered from the Belukha glacier (49° 48′ 26
″N, 86° 34′ 43 ″E, 4062 m asl) in the Siberian Altai. The ion chemistry of the upper 86 m …

Abstract The Little Ice Age (LIA) is known as one of the coldest stages of the Holocene. Most
records from the Northern Hemisphere show evidence of significantly colder conditions …

Palaeoenvironmental reconstructions with temporal coverages extending beyond Marine
Isotope Stage (MIS) three are scarce within the data sparse region of Chukotka, Far East …

Palaeotemperature reconstruction for the period of 20− 18 ka BP in S iberia is here based
on δ18 O analysis and 14 C dating of large syngenetic ice wedges. Dozens of yedoma …