Results 81 to 90 of about 28,822 (198)
Dating of ice cores from Vernagtferner (Austria) with fission products and lead-210 [PDF]
Fission product (90Sr_ 90y, I37CS, total beta) and 2tOPb_210pO activities were measured in core samples from the temperate vernagtferner (3150 m altitude, Oetztal Alps, Austria).
Gäggeler, Heinz +2 more
core
Refreezing is a critical component of the mass balance of glaciers in Svalbard, yet the processes and changes under a warming climate are not fully understood.
Satu Innanen +5 more
doaj +1 more source
Brief communication: Mapping Greenland's perennial firn aquifers using enhanced-resolution L-band brightness temperature image time series [PDF]
Julie Z. Miller +7 more
openalex +1 more source
Water movement in the firn of Storglaciären, Sweden [PDF]
AbstractThe hydraulic properties of the firn on Storglaciären, Sweden, were investigated in firn cores by water-table measurements and pumping tests. The mean density of the firn was 800 850 kg m3, giving an effective porosity of 0.073. The lower part of the firn layer was saturated with water, producing a maximum saturated layer of 5 m in late July ...
openaire +1 more source
First records of a new Europe’s southernmost glacier found in Southern Albania [PDF]
Several perennial snow and ice bodies have been recently studied and monitored in three mountain massifs across the Balkan Peninsula: Prokletije (Northern Albania), Durmitor (Montenegro) and Pirin (Bulgaria), the two glacierets in the Pirin Mountains ...
Emil Gachev +5 more
doaj +3 more sources
Eine wirkungsorientierte Finanzmarktstrategie zur Reduktion von Treibhausgasemissionen – Ergebnisse aus dem FIRN-Projekt [PDF]
Elsa Egerer
openalex +1 more source
A continuum mechanics perspective on the rheology of firn in the context of firn densification
While the complex nonlinear rheology of ice is well known and often discussed, for example in the context of large-scale ice sheet modeling, calving, and isotropy occurring at shear margins, the rheology of firn is often considered to be rather simple.
Timm Schultz +2 more
openaire +3 more sources
We present in situ firn temperatures from the extreme 2012 melt season in the southwestern lower accumulation area of the Greenland ice sheet. The upper 2.5 m of snow and firn was temperate during the melt season, when vertical meltwater percolation was ...
Charalampos Charalampidis +5 more
doaj +1 more source
Increasing surface runoff from Greenland’s firn areas
Andrew Tedstone, Horst Machguth
openalex +2 more sources

