Zobrazeno 1 - 10
of 95
pro vyhledávání: '"Barret L Kurylyk"'
Storm surge, seawater flooding, and sea-level rise paradoxically drive fresh surface water expansion
Autor:
Julia A Cantelon, Barret L Kurylyk
Publikováno v:
Environmental Research Letters, Vol 19, Iss 12, p 124038 (2024)
Coastal storms and sea-level rise (SLR) are expected to increase seawater flooding in low-elevation coastal zones. High sea levels and seawater flooding can drive groundwater table rise via ocean-aquifer connections. These dynamics are often overlook
Externí odkaz:
https://doaj.org/article/4b79a22cb8724a8887b64aecd0495bad
Autor:
Julia A Guimond, Cansu Demir, Barret L Kurylyk, Michelle A Walvoord, James W McClelland, M Bayani Cardenas
Publikováno v:
Environmental Research Letters, Vol 18, Iss 9, p 094042 (2023)
Groundwater discharge transports dissolved constituents to the ocean, affecting coastal carbon budgets and water quality. However, the magnitude and mechanisms of groundwater exchange along rapidly transitioning Arctic coastlines are largely unknown
Externí odkaz:
https://doaj.org/article/a9ea9680bf904304bda30a44453d3b70
Autor:
Barret L Kurylyk, Kathryn A Smith
Publikováno v:
Environmental Research Letters, Vol 18, Iss 6, p 061003 (2023)
Externí odkaz:
https://doaj.org/article/be2ea7dfcbba418a82284272dac14c3e
Autor:
Aaron A Mohammed, Julia A Guimond, Victor F Bense, Rob C Jamieson, Jeffrey M McKenzie, Barret L Kurylyk
Publikováno v:
Environmental Research Letters, Vol 17, Iss 12, p 124036 (2022)
Permafrost thaw leads to an increase in groundwater circulation and potential mobilization of organic carbon sequestered in deep Arctic sediments (e.g. 3–25 m below surface). Upon thaw, a portion of this carbon may be transported along new groundwa
Externí odkaz:
https://doaj.org/article/dde8ea021dc14d7685630f04c1437715
Publikováno v:
Environmental Research Letters, Vol 17, Iss 4, p 045027 (2022)
Groundwater discharge is an important mechanism through which fresh water and associated solutes are delivered to the ocean. Permafrost environments have traditionally been considered hydrogeologically inactive, yet with accelerated climate change an
Externí odkaz:
https://doaj.org/article/77dda524b8864395a2157d293b745d83
Publikováno v:
Environmental Research Letters, Vol 13, Iss 8, p 084017 (2018)
Permafrost thaw due to climate warming modifies hydrological processes by increasing hydrological connectivity between aquifers and surface water bodies and increasing groundwater storage. While previous studies have documented arctic river baseflow
Externí odkaz:
https://doaj.org/article/fc811406cdff4c5bb57bca0a0f800fdb
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-11 (2022)
Using shallow geothermal energy systems to recycle the heat accumulating in the subsurface due to climate change and urbanization is a feasible, sustainable, and opportunistic alternative to conventional space heating in the face of climate change
Externí odkaz:
https://doaj.org/article/40d48272e2254d888160f61a9484da6d
Autor:
Raymond D. Craddock, Gavin W. Kennedy, Rob C. Jamieson, Jonathan Keizer, Aaron A. Mohammed, Barret L. Kurylyk
Publikováno v:
Journal of Hydrology: Regional Studies, Vol 44, Iss , Pp 101205- (2022)
Study region: Mabou Harbour located in Cape Breton Island, Nova Scotia, Canada, is representative of the many natural harbours throughout the Maritime region of Canada as the surrounding landscape is overlain by glacial deposits, predominantly compos
Externí odkaz:
https://doaj.org/article/fe9e2311ac474d9593bd6b8adb121571
Publikováno v:
Hydrogeology Journal. 30:1551-1567
Autor:
Peter Bayer, Guillaume Attard, Philipp Blum, Hannes Hemmerle, Barret L. Kurylyk, Kathrin Menberg, Maximilian Noethen, Susanne Benz
Heat loss from buildings, infrastructure and enhanced heat flow from sealed surfaces increase the temperatures of shallow groundwater often more than global warming. A worldwide analysis of thousands of wells reveals that the temperature at every sec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b645219256c51d6c9e9958695634bf14
https://doi.org/10.5194/egusphere-egu23-1781
https://doi.org/10.5194/egusphere-egu23-1781