Results 111 to 120 of about 7,958 (231)
The role of near-surface snow processes for the formation of climate signals through densification into deep polar firn is still barely understood. To this end we have analyzed a shallow snow pit (0-3 meters) from EastGRIP (Greenland) and derived high ...
Maurine Montagnat +6 more
doaj +1 more source
Microwave emission from polar firn [PDF]
The microwave emission from a half-space medium, characterized by coordinate dependent scattering and absorbing centers, was calculated by numerically solving the radiative transfer equation by the method of invariant imbedding. Rayleigh scattering phase
Chang, A. T. C., Choudhury, B. J.
core +1 more source
Simulating ice core 10Be on the glacial–interglacial timescale [PDF]
10Be ice core measurements are an important tool for paleoclimate research, e.g., allowing for the reconstruction of past solar activity or changes in the geomagnetic dipole field.
Christl, Mark J +9 more
core +1 more source
Plant functional traits typically show strong covariation, e.g. as in the worldwide leaf economics spectrum (LES). Covariation is thought to arise from selective forces and physical constraints. However, processes shaping covariation at interspecific scales may differ from those at intraspecific scales.
Jolanta Rieksta +5 more
wiley +1 more source
Relationship between continuous aerosol measurements and firn core chemistry over a 10-year period at the South Pole [PDF]
Before ice core chemistry can be used to estimate past atmospheric chemistry it is necessary to establish an unambiguous link between concentrations of chemical species in the air and snow.
Bergin, M H +3 more
core +2 more sources
Diffusion of stable isotopes in polar firn and ice: the isotope effect in firn diffusion
International Symposium on Physics of Ice Core Records. Shikotsukohan, Hokkaido, Japan, September 14-17, 1998.
Johnsen, Sigfús. J. +6 more
openaire +2 more sources
Kinetic grain growth in firn induced by meltwater infiltration on the Greenland Ice Sheet [PDF]
The microstructure of polar firn governs its porosity, permeability, and compaction rate, and is thus critical to understanding surface elevation change, heat and gas exchange, and meltwater infiltration on ice sheets.
K. L. Gehl, J. T. Harper, N. F. Humphrey
doaj +1 more source
20th century trends and budget implications of chloroform and related tri-and dihalomethanes inferred from firn air [PDF]
Four trihalomethane (THM; CHCl3, CHBrCl2, CHBr2Cl and CHBr3) and two dihalomethane (DHM; CH2BrCl and CH2Br2) trace gases have been measured in air extracted from polar firn collected at the North Greenland Icecore Project (NGRIP) site.
D. R. Worton +5 more
doaj
Spatial distribution of vertical density and microstructure profiles in near-surface firn around Dome Fuji, Antarctica [PDF]
To better understand the near-surface evolution of polar firn in low-accumulation areas (<30 mm w.e. yr−1), we investigated the physical properties – density, microstructural anisotropy of ice matrix and pore space, and specific surface area (SSA ...
R. Inoue +13 more
doaj +1 more source

