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A proxy for snow cover and winter ground surface cooling: mapping Usnea sp. communities using high resolution remote sensing imagery (Maritime Antarctica)
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Orientador(es)
Resumo(s)
Usnea sp. formations show a spatial distribution coinciding with wind-exposed locations on rock knobs or sedimentary bodies, while they are commonly absent from concave sites. Field collection of georeferenced ground truthing data in the Meseta Norte (Fildes Peninsula, Maritime Antarctica) and the application of supervised classification techniques over a summer high resolution QuickBird satellite scene showed excellent classification accuracy for the different landcover types. The results show that Usnea formation distribution maps are a viable proxy for areas with less snow during the cold season. Such an approach provides input for permafrost and active layer modelling since snow acts as a critical control on ground surface heat balance. Since snow mapping is extremely difficult in Maritime Antarctica our tested approach provides important added-value for empirical–statistical modelling of permafrost distribution.
Descrição
Palavras-chave
Permafrost Bioindicators Snow cover Ground surface cooling Fildes Peninsula Antarctica
Contexto Educativo
Citação
Vieira, Goncalo, Mora, Carla, Pina, Pedro & Schaefer, Carlos E.R. (2014). A proxy for snow cover and winter ground surface cooling: mapping Usnea sp. communities using high resolution remote sensing imagery (Maritime Antarctica). Geomorphology, 225, 69-75. https://doi.org/10.1016/j.geomorph.2014.03.049. ISSN: 0169-555X
Editora
Elsevier