๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

The hydrology of the proglacial zone of a high-Arctic glacier (Finsterwalderbreen, Svalbard): Atmospheric and surface water fluxes

โœ Scribed by Richard Hodgkins; Richard Cooper; Jemma Wadham; Martyn Tranter


Book ID
113715878
Publisher
Elsevier Science
Year
2009
Tongue
English
Weight
1011 KB
Volume
378
Category
Article
ISSN
0022-1694

No coin nor oath required. For personal study only.


๐Ÿ“œ SIMILAR VOLUMES


Distribution of glaciofluvial sediment w
โœ Glasser, Neil F.; Bennett, Matthew R.; Huddart, David ๐Ÿ“‚ Article ๐Ÿ“… 1999 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 825 KB

Marthabreen is a 7ยด8 km long valley glacier in SW Spitsbergen. The glacier is partially covered by a layer of angular debris derived from rockfall in its accumulation area, pierced in places by pinnacles and ridges of glaciofluvial sediment. These concentrations of glaciofluvial sediment fall into t

The hydrochemistry of runoff from a โ€˜col
โœ R. Hodgkins; M. Tranter; J. A. Dowdeswell ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 362 KB ๐Ÿ‘ 1 views

There are still relatively few hydrochemical studies of glacial runo and meltwater routing from the high latitudes, where non-temperate glacier ice is frequently encountered. Representative samples of glacier meltwater were obtained from Scott Turnerbreen, a `cold-based' glacier at 788 N in the Norw

Impact of an extreme melt event on the r
โœ Sarah Boon; Martin Sharp; Peter Nienow ๐Ÿ“‚ Article ๐Ÿ“… 2003 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 951 KB

## Abstract On 28โ€“30 July 2000, an extreme melt event was observed at John Evans Glacier (JEG), Ellesmere Island (79ยฐ 40โ€ฒN, 74ยฐ 00โ€ฒW). Hourly melt rates during this event fell in the upper 4% of the distribution of melt rates observed at the site during the period 1996โ€“2000. Synoptic conditions dur

The hydrochemistry of meltwaters drainin
โœ J. L. Wadham; A. J. Hodson; M. Tranter; J. A. Dowdeswell ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 583 KB

Solute and runo time-series at Finsterwalderbreen, Svalbard, provide evidence for considerable basal routing of water and the existence of at least two contrasting subglacial chemical weathering environments. The hydrochemistry of a subglacial upwelling provides evidence for a snowmelt-fed subglacia