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

Area and volume changes and the average geodetic mass balance of thenon-surging outlet glaciers of the southeast Vatnajökull ice cap, Iceland,during different time periods between ~ 1890 and 2010, are derived froma multi-temporal glacier inventory. A series of digital elevation models(DEMs) (~ 1890, 1904, 1936, 1945, 1989, 2002, 2010) are compiled fromglacial geomorphological features, historical photographs, maps, aerialimages, DGPS measurements and a lidar survey. Given the mapped basaltopography, we estimate volume changes since the end of the Little Ice Age(LIA) ~ 1890. The variable volume loss of the outlets to similarclimate forcing is related to their different hypsometry, basal topography,and the presence of proglacial lakes. In the post-LIA period, the glacierizedarea decreased by 164 km2 (or from 1014 to 851 km2) and theglaciers had lost 10–30 % of their ~ 1890 area by 2010 (anywherefrom 3 to 36 km2). The glacier surface lowered by 150–270 m near theterminus and the outlet glaciers collectively lost 60 ± 8 km3 ofice, which is equivalent to 0.15 ± 0.02 mm of sea-level rise. Thevolume loss of individual glaciers was in the range of 15–50%,corresponding to a geodetic mass balance between −0.70 and−0.32 m w.e. a−1. The annual rate of mass change during thepost-LIA period was most negative in 2002–2010, on average−1.34 ± 0.12 m w.e. a−1, which is among the most negativemass balance values recorded worldwide in the early 21st century

Changes in the southeast Vatnajökull ice cap, Iceland, between ~ 1890 and 2010