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Hydrochemistry of meltwaters draining a polythermal-based, high-Arctic glacier, south Svalbard: II. Winter and early Spring

โœ Scribed by J. L. Wadham; M. Tranter; J. A. Dowdeswell


Publisher
John Wiley and Sons
Year
2000
Tongue
English
Weight
237 KB
Volume
14
Category
Article
ISSN
0885-6087

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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