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pro vyhledávání: '"Murray D. Mackay"'
Autor:
Habiba Kallel, Daniel F. Nadeau, Benjamin Bouchard, Antoine Thiboult, Murray D. Mackay, François Anctil
Publikováno v:
Frontiers in Environmental Science, Vol 12 (2024)
At high latitudes, lake-atmosphere interactions are disrupted for several months of the year by the presence of an ice cover. By isolating the water column from the atmosphere, ice, typically topped by snow, drastically alters albedo, surface roughne
Externí odkaz:
https://doaj.org/article/8419cb61c49f431ead1fee6439123935
Autor:
Murray D. MacKay
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 12, Pp n/a-n/a (2023)
Abstract If lake ice is assumed to deform and fail as a linear viscoelastic material under the action of wind stress, then a simple ice concentration scaling law can be constructed suitable for one‐dimensional lake models embedded within environmen
Externí odkaz:
https://doaj.org/article/3a130f6f902a4a5885072558e81a929c
Publikováno v:
Atmosphere-Ocean. 61:1-11
The files provided here include the source code of the CanadianLand Surface Scheme Including biogeochemical Cycles (CLASSIC;https://cccma.gitlab.io/classic_pages/)v1.1, initialization files and meteorological measurementsused to forceCLASSIC at five
Publikováno v:
Journal of Hydrometeorology.
Accurately modeling the interactions between inland water bodies and the atmosphere in meteorological and climate models is crucial, given the marked differences with surrounding landmasses. Modeling surface heat fluxes remains a challenge because di
Autor:
Murray D. MacKay
Publikováno v:
Geoscientific Model Development, Vol 12, Pp 3045-3054 (2019)
Lake models are increasingly being incorporated into global and regional climate and numerical weather prediction systems. Lakes interact with their surroundings through flux exchange at their bottom sediments and with the atmosphere at the surface,
Autor:
Murray D. MacKay
Publikováno v:
Journal of the Atmospheric Sciences. 55:2261-2269
Unbalanced frontogenesis studies frequently employ a mathematical model known as the two-dimensional primitive equations, a reduction of the full three-dimensional primitive equations made by ignoring variations in the meridional direction. Such a mo
Autor:
G. W. Kent Moore, Murray D. MacKay
Publikováno v:
Journal of the Atmospheric Sciences. 52:3879-3884
Piecewise linear flow profiles are commonly used in quasigeostrophic (QG) stability analyses as idealizations of the smooth profiles found in nature. In such studies the QG potential vorticity (PV) equation is generally solved in layers of uniform PV