Abstract
We present a method to estimate the glacier contribution to sea-level rise from glacier
length records. These records form the only direct evidence of glacier changes prior
to 1946, when the first systematic mass-balance observations began. A globally rep-
resentative length signal is calculated from 197 length records from all continents by
normalisation and averaging of 14 different regions. Next, the resulting signal is calibrated
with mass-balance observations for the period 1961–2000. We find that the
glacier contribution to sea level rise was 5.5±1.0 cm during the period 1850–2000 and
4.5±0.7 cm during the period 1900–2000.
Original language | Undefined/Unknown |
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Pages (from-to) | 77-97 |
Number of pages | 23 |
Journal | Cryosphere Discussions |
Volume | 1 |
Publication status | Published - 2007 |