Zobrazeno 1 - 10
of 43
pro vyhledávání: '"W. L. Quinton"'
Autor:
C. M. DeBeer, H. S. Wheater, J. W. Pomeroy, A. G. Barr, J. L. Baltzer, J. F. Johnstone, M. R. Turetsky, R. E. Stewart, M. Hayashi, G. van der Kamp, S. Marshall, E. Campbell, P. Marsh, S. K. Carey, W. L. Quinton, Y. Li, S. Razavi, A. Berg, J. J. McDonnell, C. Spence, W. D. Helgason, A. M. Ireson, T. A. Black, M. Elshamy, F. Yassin, B. Davison, A. Howard, J. M. Thériault, K. Shook, M. N. Demuth, A. Pietroniro
Publikováno v:
Hydrology and Earth System Sciences, Vol 25, Pp 1849-1882 (2021)
The interior of western Canada, like many similar cold mid- to high-latitude regions worldwide, is undergoing extensive and rapid climate and environmental change, which may accelerate in the coming decades. Understanding and predicting changes in co
Externí odkaz:
https://doaj.org/article/946be1658aca485c8322d6862b85c1ab
Publikováno v:
Hydrology and Earth System Sciences, Vol 22, Pp 4455-4472 (2018)
Boreal peatlands are major catchment sources of dissolved organic carbon (DOC) and nutrients and thus strongly regulate the landscape carbon balance, aquatic food webs, and downstream water quality. Climate change is likely to influence catchment
Externí odkaz:
https://doaj.org/article/e64424c1bce94f2d93f7e9fa41694769
Publikováno v:
Hydrology and Earth System Sciences, Vol 16, Iss 2, Pp 501-515 (2012)
There are not many studies that report water movement in freezing peat. Soil column studies under controlled laboratory settings can help isolate and understand the effects of different factors controlling freezing of the active layer in organic cove
Externí odkaz:
https://doaj.org/article/685d8fb0f20548e9b52a2a986b863ccf
Publikováno v:
Hydrology and Earth System Sciences, Vol 14, Iss 5, Pp 729-750 (2010)
Infiltration into frozen and unfrozen soils is critical in hydrology, controlling active layer soil water dynamics and influencing runoff. Few Land Surface Models (LSMs) and Hydrological Models (HMs) have been developed, adapted or tested for frozen
Externí odkaz:
https://doaj.org/article/ef5a6b0f85f24a4bab0f2268c7aeb1c1
Publikováno v:
Hydrology and Earth System Sciences, Vol 13, Iss 10, Pp 1993-2002 (2009)
The hydraulic conductivity of unsaturated peat soil is controlled by the air-filled porosity, pore size and geometric distribution as well as other physical properties of peat materials. This study investigates how the size and shape of pores affects
Externí odkaz:
https://doaj.org/article/8493d8f24c6547dd8db744512bec5eaf
Publikováno v:
Hydrology and Earth System Sciences, Vol 8, Iss 5, Pp 877-890 (2004)
In northern alpine tundra, large slope gradients, late-lying snow drifts and shallow soils overlying impermeable substrates all contribute to large hillslope runoff volumes during the spring freshet. Understanding the processes and pathways of hillsl
Externí odkaz:
https://doaj.org/article/25e8ae1b693f46808406d17e8d3207da
Autor:
W. L. Quinton, Nicole Dion, David Olefeldt, Stefan Goodman, Christopher Spence, N. Hedstrom, Suzanne E. Tank
Publikováno v:
Hydrological Processes. 34:4940-4958
Forest fires are becoming more frequent and larger in the subarctic Canadian Shield, so understanding the effect of fire on catchment scale water budgets is becoming increasingly important. The objective of this study was to determine the water budge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cca344c1436765d16af61a2dd7817113
https://doi.org/10.1002/hyp.13915
https://doi.org/10.1002/hyp.13915
Autor:
Philippe Van Cappellen, W. L. Quinton, Jonathan S. Price, Fereidoun Rezanezhad, T. Milojevic, Bernd Lennartz
Publikováno v:
Chemical Geology. 429:75-84
Global peatlands are a valuable but vulnerable resource. They represent a significant carbon and energy reservoir and play major roles in water and biogeochemical cycles. Peat soils are highly complex porous media with distinct characteristic physica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bf8f6b28b4cb74e114c6c4219c68d131
https://doi.org/10.1016/j.chemgeo.2016.03.010
https://doi.org/10.1016/j.chemgeo.2016.03.010
In the arctic tundra the ground is normally composed by a relatively thin organic soil layer, overlying mineral sediment. Subsurface water drainage generally occurs in the organic layer for its high hydraulic conductivity. However, the organic layer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::02207d1055dbb2f82d9e0569dbbfa070
https://www.the-cryosphere-discuss.net/tc-2011-3/
https://www.the-cryosphere-discuss.net/tc-2011-3/
Changing hydrologic connectivity due to permafrost thaw in the lower Liard River valley, NWT, Canada
Publikováno v:
Hydrological Processes. 28:4163-4178
Flows from river basins in northwestern Canada have been rising in the last two decades as a result of climate warming. In the wetland-dominated basins that characterise the southern margin of permafrost, permafrost thaw and disappearance, and result
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c7967f8734f886e3bcbfdd788b99a7ea
https://doi.org/10.1002/hyp.10206
https://doi.org/10.1002/hyp.10206