Zobrazeno 1 - 10
of 445
pro vyhledávání: '"Subglacial stream"'
Autor:
Park, Chris, Allaby, Michael
Publikováno v:
A Dictionary of Environment and Conservation, 3 ed., 2017.
Externí odkaz:
http://www.oxfordreference.com/view/10.1093/acref/9780191826320.001.0001/acref-9780191826320-e-7903
Autor:
Park, Chris, Allaby, Michael
Publikováno v:
A Dictionary of Environment and Conservation, 2 ed., 2013.
Externí odkaz:
http://www.oxfordreference.com/view/10.1093/acref/9780199641666.001.0001/acref-9780199641666-e-7903
Autor:
Park, Chris
Publikováno v:
A Dictionary of Environment and Conservation, 1 ed., 2007.
Externí odkaz:
http://www.oxfordreference.com/view/10.1093/acref/9780198609957.001.0001/acref-9780198609957-e-7903
Publikováno v:
Hydrological Processes. 31:4719-4733
The thermal regimes of alpine streams remain understudied and have important implications for cold-water fish habitat which is expected to decline due to climatic warming. Previous research has focused on the effects of distributed energy fluxes and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5dcf1b49af11220507fcf0d63998779e
https://doi.org/10.1002/hyp.11391
https://doi.org/10.1002/hyp.11391
Autor:
Chris R. Stokes
Publikováno v:
Earth Surface Processes and Landforms. 43:85-123
Ice streams are integral components of an ice sheet's mass balance and directly impact on sea level. Their flow is governed by processes at the ice-bed interface which create landforms that, in turn, modulate ice stream dynamics through their influen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3770051b6cbac38093a7f61b36486549
https://doi.org/10.1002/esp.4259
https://doi.org/10.1002/esp.4259
Autor:
Emily L. Shroyer, David A. Sutherland, Leigh A. Stearns, Jonathan D. Nash, Ginny A. Catania, Dustin Carroll
Publikováno v:
Journal of Geophysical Research: Oceans. 122:6611-6629
The classic model of fjord renewal is complicated by tidewater glacier fjords, where submarine melt and subglacial discharge provide substantial buoyancy forcing at depth. Here we use a suite of idealized, high-resolution numerical ocean simulations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e313c120e41c5d562f835284ebf9d96c
https://doi.org/10.1002/2017jc012962
https://doi.org/10.1002/2017jc012962
Autor:
Sebastian Beyer, Karin Andreassen, Angelika Humbert, Eythor Gudlaugsson, Thomas Kleiner, Caroline Clason
Publikováno v:
EPIC3Journal of Glaciology, Cambridge University Press, 63(239), pp. 556-564, ISSN: 0022-1430
Ice-stream dynamics are strongly controlled by processes taking place at the ice/bed interface where subglacial water both lubricates the base and saturates any existing, underlying sediment. Large parts of the former Eurasian ice sheet were underlai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a1cd5a73e9b5036b1374eedf32f0b39
https://doi.org/10.1017/jog.2017.21
https://doi.org/10.1017/jog.2017.21
Autor:
Riccardo Vassallo, Hervé Guillon, Jean-Louis Mugnier, Jean-François Buoncristiani, Peter van der Beek, Julien Carcaillet, Charlotte Prud'homme, Cécile Godon
Publikováno v:
Earth Surface Processes and Landforms. 40:1202-1215
Deciphering the complex interplays between climate, uplift and erosion is not straightforward and estimating present-day erosion rates can provide useful insights. Glaciers are thought to be powerful erosional agents, but most published ‘glacial’
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::719f84c3669096236990feaed14377a0
https://doi.org/10.1002/esp.3713
https://doi.org/10.1002/esp.3713
Publikováno v:
Geochimica et Cosmochimica Acta
In this study, we present the first measurements of iron (Fe) stable isotopic composition (δ 56 Fe) of subglacial streams draining the Greenland Ice Sheet (GIS). We measure the δ 56 Fe values [(δ 56 Fe, ‰ = ( 56 Fe/ 54 Fe) sample /( 56 Fe/ 54 Fe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::713f9a87a8c069fa87668da2f9f205e1
http://eprints.esc.cam.ac.uk/4006/1/1-s2.0-S0016703717303502-main.pdf
http://eprints.esc.cam.ac.uk/4006/1/1-s2.0-S0016703717303502-main.pdf
Publikováno v:
The Cryosphere, Vol 10, Iss 6, Pp 2971-2980 (2016)
We identify two previously unknown subglacial lakes beneath the stagnated trunk of the Kamb Ice Stream (KIS). Rapid fill-drain hydrologic events over several months are inferred from surface height changes measured by CryoSat-2 altimetry and indicate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ce9f88b48e1a95b166d8f0a291e35237
http://www.the-cryosphere.net/10/2971/2016/tc-10-2971-2016.pdf
http://www.the-cryosphere.net/10/2971/2016/tc-10-2971-2016.pdf