Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Madeleine C. Garibaldi"'
Publikováno v:
Arctic Science (2024)
A scenario-based approach was used to test air and ground response to warming with and without changes to inverted surface lapse rates in four Yukon valleys. Generally, climate warming coupled with weakening of temperature inversions resulted in the
Externí odkaz:
https://doaj.org/article/8853fd7c0559419a840b4160c2ef5c54
Publikováno v:
Arctic Science (2024)
Spatial maps of the air and ground thermal regime were generated for four Yukon valleys. The aim was to model air, ground surface, and ground temperature (at fine spatial resolution) using locally measured inverted surface lapse rates (SLR) to better
Externí odkaz:
https://doaj.org/article/3af44c0c40ad4829aea414197879f28d
Autor:
Nick C. Noad, Philip P. Bonnaventure, Gaëlle F. Gilson, Hester Jiskoot, Madeleine C. Garibaldi
Publikováno v:
Arctic Science, Vol 9, Iss 3, Pp 545-563 (2023)
Assumptions of linear lapse rates in regions prone to surface-based inversions (SBIs) can generate biases in the prediction of surface air temperature. Although studies of Arctic inversions are common, few regional studies of their characteristics ex
Externí odkaz:
https://doaj.org/article/9848081be2ae4bfd99b6dcc6114dc872
Publikováno v:
Arctic, Antarctic, and Alpine Research, Vol 54, Iss 1, Pp 274-293 (2022)
Active layer thicknesses (ALTs) from sites along a transect through the Mackenzie Valley, Northwest Territories, Canada, were analyzed to explore variation in thickness within and between ecoregions. At an ecoregional scale the relation between ALT,
Externí odkaz:
https://doaj.org/article/d9598ae2fbea4e82be99a74a304573cb
Publikováno v:
Permafrost and Periglacial Processes. 32:19-34
Autor:
Yifeng Wang, Mishélle A. E. Wehbe, Jake R. Burton, Robert G. Way, Caitlin M. Lapalme, Philip P. Bonnaventure, Alexandre R. Bevington, Emma Davis, Rosamond Tutton, Madeleine C. Garibaldi
Publikováno v:
Permafrost 2021.
The Torngat Mountains of northern Labrador are an Arctic cordilleran mountain range located at the southern limit of the Canadian Arctic. Sparse observations of periglacial landforms including rock glaciers and ice-cored moraines imply that permafros