English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

To date, most mass balance studies in Iceland have concentrated on the three largest ice caps. This study turns the focus toward smaller Icelandic glaciers, presenting geodetic mass-balance estimates for 14 of them (total area 1,005 km2 in 2017) from 1945 to 2017, in decadal time spans. These glaciers, distributed over the country, are subject to different climatic forcing. The mass balance, derived from airborne and spaceborne stereo imagery and airborne lidar, is correlated with precipitation and air temperature by a first-order equation including a reference-surface correction term. This permits statistical modeling of annual mass balance, used to temporally homogenize the mass balance for a region-wide mass balance assessment for the periods 1945–1960, 1960–1980, 1980–1994, 1994–2004, 2004–2010, and 2010–2017. The 14 glaciers were close to equilibrium during 1960–1994, with an area-weighted mass balance of 0.07 ± 0.07 m w.e. a−1. The most negative mass balance occurred in 1994–2010, accounting for −1.20 ± 0.09 m w.e. a−1, or 21.4 ± 1.6 Gt (1.3 ± 0.1 Gt a−1) of mass loss. Glaciers located along the south and west coasts show higher decadal mass-balance variability and static mass-balance sensitivities to summer temperature and winter precipitation, −2.21 ± 0.25 m w.e. a−1 K−1 and 0.22 ± 0.11 m w.e. a−1(10%)−1, respectively, while glaciers located inland, north and northwest, have corresponding mass-balance sensitivities of −0.72 ± 0.10 m w.e. a−1 K−1 and 0.13 ± 0.07 m w.e. a−1(10%)−1. These patterns are likely due to the proximity to warm (south and west) vs. cold (northwest) oceanic currents.

Mass Balance of 14 Icelandic Glaciers, 1945–2017: Spatial Variations and Links With Climate