Results 41 to 50 of about 815,112 (296)
Response of a marine-terminating Greenland outlet glacier to abrupt cooling 8200 and 9300 years ago [PDF]
Long-term records of Greenland outlet-glacier change extending beyond the satellite era can inform future predictions of Greenland Ice Sheet behavior. Of particular relevance is elucidating the Greenland Ice Sheet's response to decadal- and centennial ...
Greg S. Babonis +13 more
core +1 more source
Improved direct-count method by fluorescence microscope for low-biomass ice core
Ice cores recovered from ice sheets contain microorganisms that were transported to the surface of the ice sheet along with airborne dust. The abundance of microorganisms in ice cores, as measured by direct cell count under a fluorescence microscope, is ...
Jun Uetake +2 more
doaj +1 more source
The physical and geochemical characteristics of shallow ice cores drilled in the accumulation area (Western Cwm) of Khumbu Glacier in the Nepal Himalayas in 1980 were analyzed.
Nozomu Takeuchi +4 more
doaj +1 more source
Greenland Summit Ice Cores CD-ROM as zip-archive
Greenland Summit Ice Cores CD-ROM as zip ...
GRIP/GISP +3 more
core +1 more source
Shallow firn cores, in addition to a near-basal ice core, were recovered in 2018 from the Quelccaya ice cap (5470 m a.s.l) in the Cordillera Vilcanota, Peru, and in 2017 from the Nevado Illimani glacier (6350 m a.s.l) in the Cordillera Real, Bolivia. The
Heather M. Clifford +24 more
doaj +1 more source
Seasonal Variations in Hydrogen Peroxide in Polar Ice Cores [PDF]
Hydrogen peroxide is present in polar snow and ice in remarkably high concentrations. With values up to 300 ppb, H2O2 is one of the most concentrated impurities in polar ice.
Sigg, Andreas +3 more
core +1 more source
210Pb-Dating of Cold Alpine Firn/Ice Cores From Colle Gnifetti, Switzerland [PDF]
The 210Pb(210Po) method has for the first time been successfully applied for dating cold alpine firn/ice cores. The mean accumulation rate on Grenzgletscher near Colle Gnifetti (Switzerland, altitude 4 450 m) is found to be 37 cm year−1 and 32 cm year−1 ...
H. R. von Gunten +9 more
core +1 more source
Novel approach to estimate the water isotope diffusion length in deep ice cores with an application to Marine Isotope Stage 19 in the Dome C ice core [PDF]
Accurate estimates of water isotope diffusion lengths are crucial when reconstructing and interpreting water isotope records from ice cores. This is especially true in the deepest, oldest sections of deep ice cores, where thermally enhanced diffusive ...
F. Shaw +5 more
doaj +1 more source
The Shewanella oneidensis Fic enzyme SoFic targets the switch‐I region of EF‐Tu for AMPylation
Fic enzymes mediate diverse post‐translational modifications across all domains of life, including AMPylation. Prokaryotic EF‐Tu can be AMPylated and deAMPylated by the conserved Fic enzyme SoFic. Structural and biochemical approaches were used to characterize the effect of AMPylation on EF‐Tu, SoFic's enzymatic activities, and the enzyme‐target ...
Svenja Runge +6 more
wiley +1 more source
(Table 3) Ion concentration of the GRIP and Dome Fuji ice cores, Greenland and Antarctica
(Table 3) Ion concentration of the GRIP and Dome Fuji ice cores, Greenland and ...
Yoshinori Iizuka (8008220) +13 more
core +1 more source

