Analysis of Megadune Fields in Antarctica

In this research, we present new and updated properties of the megadune fields, which are largely distributed on the Antarctic plateau. We used mainly Landsat 8 OLI imagery in order to characterize the megadune fields using visible and Near Infrared bands. Focusing on two areas where megadunes occur...

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Published in:2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS
Main Authors: Giacomo Traversa, Davide Fugazza, Massimo Frezzotti
Other Authors: G. Traversa, D. Fugazza, M. Frezzotti
Format: Book Part
Language:English
Published: IEEE 2021
Subjects:
Online Access:http://hdl.handle.net/2434/897972
https://doi.org/10.1109/igarss47720.2021.9554827
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spelling ftunivmilanoair:oai:air.unimi.it:2434/897972 2024-04-21T07:51:13+00:00 Analysis of Megadune Fields in Antarctica Giacomo Traversa Davide Fugazza Massimo Frezzotti G. Traversa D. Fugazza M. Frezzotti 2021 http://hdl.handle.net/2434/897972 https://doi.org/10.1109/igarss47720.2021.9554827 eng eng IEEE info:eu-repo/semantics/altIdentifier/isbn/978-1-6654-4762-1 ispartofbook:2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS IGARSS firstpage:5513 lastpage:5516 numberofpages:4 serie:IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM PROCEEDINGS http://hdl.handle.net/2434/897972 doi:10.1109/igarss47720.2021.9554827 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85129785976 info:eu-repo/semantics/closedAccess Antarctica megadune remote-sensing Landsat surface mass balance Settore GEO/04 - Geografia Fisica e Geomorfologia info:eu-repo/semantics/bookPart 2021 ftunivmilanoair https://doi.org/10.1109/igarss47720.2021.9554827 2024-03-27T02:08:15Z In this research, we present new and updated properties of the megadune fields, which are largely distributed on the Antarctic plateau. We used mainly Landsat 8 OLI imagery in order to characterize the megadune fields using visible and Near Infrared bands. Focusing on two areas where megadunes occur, we provide detailed albedo measurements, both broadband and near-infrared, differentiating their upwind and downwind parts. In addition, we calculated their brightness temperature. Using the wind surface morphology obtained from Landsat 8 OLI images and the REMA DTM, we also calculated the Slope in the Prevailing Wind Direction at about ten meters scale, which provided information about the formation of snow glazed surfaces. Finally, we studied the upwind migration of the megadunes and compared these results with other remote-sensing products and in-situ measurements. Book Part Antarc* Antarctic Antarctica The University of Milan: Archivio Istituzionale della Ricerca (AIR) 2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS 5513 5516
institution Open Polar
collection The University of Milan: Archivio Istituzionale della Ricerca (AIR)
op_collection_id ftunivmilanoair
language English
topic Antarctica
megadune
remote-sensing
Landsat
surface mass balance
Settore GEO/04 - Geografia Fisica e Geomorfologia
spellingShingle Antarctica
megadune
remote-sensing
Landsat
surface mass balance
Settore GEO/04 - Geografia Fisica e Geomorfologia
Giacomo Traversa
Davide Fugazza
Massimo Frezzotti
Analysis of Megadune Fields in Antarctica
topic_facet Antarctica
megadune
remote-sensing
Landsat
surface mass balance
Settore GEO/04 - Geografia Fisica e Geomorfologia
description In this research, we present new and updated properties of the megadune fields, which are largely distributed on the Antarctic plateau. We used mainly Landsat 8 OLI imagery in order to characterize the megadune fields using visible and Near Infrared bands. Focusing on two areas where megadunes occur, we provide detailed albedo measurements, both broadband and near-infrared, differentiating their upwind and downwind parts. In addition, we calculated their brightness temperature. Using the wind surface morphology obtained from Landsat 8 OLI images and the REMA DTM, we also calculated the Slope in the Prevailing Wind Direction at about ten meters scale, which provided information about the formation of snow glazed surfaces. Finally, we studied the upwind migration of the megadunes and compared these results with other remote-sensing products and in-situ measurements.
author2 G. Traversa
D. Fugazza
M. Frezzotti
format Book Part
author Giacomo Traversa
Davide Fugazza
Massimo Frezzotti
author_facet Giacomo Traversa
Davide Fugazza
Massimo Frezzotti
author_sort Giacomo Traversa
title Analysis of Megadune Fields in Antarctica
title_short Analysis of Megadune Fields in Antarctica
title_full Analysis of Megadune Fields in Antarctica
title_fullStr Analysis of Megadune Fields in Antarctica
title_full_unstemmed Analysis of Megadune Fields in Antarctica
title_sort analysis of megadune fields in antarctica
publisher IEEE
publishDate 2021
url http://hdl.handle.net/2434/897972
https://doi.org/10.1109/igarss47720.2021.9554827
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation info:eu-repo/semantics/altIdentifier/isbn/978-1-6654-4762-1
ispartofbook:2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS
IGARSS
firstpage:5513
lastpage:5516
numberofpages:4
serie:IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM PROCEEDINGS
http://hdl.handle.net/2434/897972
doi:10.1109/igarss47720.2021.9554827
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85129785976
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1109/igarss47720.2021.9554827
container_title 2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS
container_start_page 5513
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