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Remote sensing of alpine glaciers in visible and infrared wavelengths: a survey of advances and prospects
Department of Environmental Science, Sharda University.ORCID-id: 0000-0002-2502-6384
Space Applications Centre, ISRO, Ahmedabad, Atmospheric and Oceanic Sciences Group, Space Applications Centre, Indian Space Research Organisation, Ahmedabad, Department of Natural Resources, TERI University, New Delhi.
Department of Environmental Science, Sharda University.
Snow and Avalanche Study Establishment, Defence Research and Development Organization (DRDO), Him Parisar, Sector-37A, Chandigarh.
2016 (Engelska)Ingår i: Geocarto International, ISSN 1010-6049, E-ISSN 1752-0762, Vol. 31, nr 5, s. 557-574Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

Remote sensing is an efficient tool for temporal monitoring of inaccessible alpine glacial terrain. This study discusses the methods of remote sensing in visible and infrared (IR) wavelengths, which are helpful in providing important information about alpine glaciers. The scope of this study covers recent advances and prospects in optical and thermal remote sensing of glacier facies, glacier velocity, mass balance, glacial hazards and automated mapping techniques. The technology is ever evolving with the advent of new remote sensors capturing data in visible/IR wavelengths and better digital computing technology. An extensive list of significant studies further helps the reader to explore a particular topic of interest. We survey recent advances in this field and additionally highlight the emerging prospects

Ort, förlag, år, upplaga, sidor
2016. Vol. 31, nr 5, s. 557-574
Nationell ämneskategori
Rymd- och flygteknik
Forskningsämne
Atmosfärsvetenskap
Identifikatorer
URN: urn:nbn:se:ltu:diva-7173DOI: 10.1080/10106049.2015.1059903Lokalt ID: 57f6bfd3-d493-4128-a074-1b4ea7ae44b2OAI: oai:DiVA.org:ltu-7173DiVA, id: diva2:980061
Anmärkning
Upprättat; 2016; 20160627 (andbra)Tillgänglig från: 2016-09-29 Skapad: 2016-09-29 Senast uppdaterad: 2017-11-24Bibliografiskt granskad

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