Annual mass-balance series of a temperate glacier in the Caucasus, reconstructed from an ice core
Caucasus ; European part of Russia ; Geochemistry ; Geophysics ; Glacier ; Glacier mass balance ; Ice core ; Oxygen 18 ; Time series ; Twentieth Century
Identification of annual layers in a firn/ice core provides a possibility to reconstruct the mass-balance sequence for glaciers where no direct observations have been carried out. A number of cores is obtained from the boreholes drilled