Macrophysical properties and a climatology of Arctic coastal fog in East Greenland

Arctic summer fog is a major transportation hazard and has implications for the cryospheric energy balance. In this thesis, the climatology and macrophysical properties of fog along the coast of East Greenland are explored, and local to mesoscale environmental conditions studied to explain regional...

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Main Authors: Gilson, Gaëlle Florence, University of Lethbridge. Faculty of Arts and Science
Other Authors: Jiskoot, Hester
Format: Thesis
Language:English
Published: Lethbridge, Alta. : Universtiy of Lethbridge, Department of Geography 2018
Subjects:
Online Access:https://hdl.handle.net/10133/5038
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spelling ftunivlethb:oai:opus.uleth.ca:10133/5038 2023-05-15T14:32:35+02:00 Macrophysical properties and a climatology of Arctic coastal fog in East Greenland Gilson, Gaëlle Florence University of Lethbridge. Faculty of Arts and Science Jiskoot, Hester 2018 application/pdf https://hdl.handle.net/10133/5038 en_US eng Lethbridge, Alta. : Universtiy of Lethbridge, Department of Geography Arts and Science Department of Geography Thesis (University of Lethbridge. Faculty of Arts and Science) https://hdl.handle.net/10133/5038 Arctic summer fog Cryosphere Fog--Arctic regions Fog--Greenland Greenland--Climate liquid fog Coasts--Greenland Coasts--Arctic regions Arctic regions--Climate Climatic changes Temperature inversions--Greenland Thesis 2018 ftunivlethb 2021-06-27T07:20:04Z Arctic summer fog is a major transportation hazard and has implications for the cryospheric energy balance. In this thesis, the climatology and macrophysical properties of fog along the coast of East Greenland are explored, and local to mesoscale environmental conditions studied to explain regional differences. Using a combination of long-term synoptic weather observations and Integrated Global Radiosonde Archive data, novel automated methods were developed to classify liquid fog thermodynamic structure and calculate fog top elevation. Six fog types were identified; several of which could be associated with advection fog formation and dissipation processes. Temperature inversions during fog were deeper and stronger compared to non-fog conditions. At Low-Arctic locations fog was geometrically thin and occurred below the temperature inversion. Fog was thicker in the High-Arctic, often penetrating the inversion layer. The radiosonde data analysis and automated methods presented are applicable to any synoptic Arctic weather station with present weather codes. Natural Sciences and Engineering Research Council of Canada; Alberta Innovates Technology Futures. Thesis Arctic East Greenland Greenland University of Lethbridge Institutional Repository Arctic Canada Greenland
institution Open Polar
collection University of Lethbridge Institutional Repository
op_collection_id ftunivlethb
language English
topic Arctic summer fog
Cryosphere
Fog--Arctic regions
Fog--Greenland
Greenland--Climate
liquid fog
Coasts--Greenland
Coasts--Arctic regions
Arctic regions--Climate
Climatic changes
Temperature inversions--Greenland
spellingShingle Arctic summer fog
Cryosphere
Fog--Arctic regions
Fog--Greenland
Greenland--Climate
liquid fog
Coasts--Greenland
Coasts--Arctic regions
Arctic regions--Climate
Climatic changes
Temperature inversions--Greenland
Gilson, Gaëlle Florence
University of Lethbridge. Faculty of Arts and Science
Macrophysical properties and a climatology of Arctic coastal fog in East Greenland
topic_facet Arctic summer fog
Cryosphere
Fog--Arctic regions
Fog--Greenland
Greenland--Climate
liquid fog
Coasts--Greenland
Coasts--Arctic regions
Arctic regions--Climate
Climatic changes
Temperature inversions--Greenland
description Arctic summer fog is a major transportation hazard and has implications for the cryospheric energy balance. In this thesis, the climatology and macrophysical properties of fog along the coast of East Greenland are explored, and local to mesoscale environmental conditions studied to explain regional differences. Using a combination of long-term synoptic weather observations and Integrated Global Radiosonde Archive data, novel automated methods were developed to classify liquid fog thermodynamic structure and calculate fog top elevation. Six fog types were identified; several of which could be associated with advection fog formation and dissipation processes. Temperature inversions during fog were deeper and stronger compared to non-fog conditions. At Low-Arctic locations fog was geometrically thin and occurred below the temperature inversion. Fog was thicker in the High-Arctic, often penetrating the inversion layer. The radiosonde data analysis and automated methods presented are applicable to any synoptic Arctic weather station with present weather codes. Natural Sciences and Engineering Research Council of Canada; Alberta Innovates Technology Futures.
author2 Jiskoot, Hester
format Thesis
author Gilson, Gaëlle Florence
University of Lethbridge. Faculty of Arts and Science
author_facet Gilson, Gaëlle Florence
University of Lethbridge. Faculty of Arts and Science
author_sort Gilson, Gaëlle Florence
title Macrophysical properties and a climatology of Arctic coastal fog in East Greenland
title_short Macrophysical properties and a climatology of Arctic coastal fog in East Greenland
title_full Macrophysical properties and a climatology of Arctic coastal fog in East Greenland
title_fullStr Macrophysical properties and a climatology of Arctic coastal fog in East Greenland
title_full_unstemmed Macrophysical properties and a climatology of Arctic coastal fog in East Greenland
title_sort macrophysical properties and a climatology of arctic coastal fog in east greenland
publisher Lethbridge, Alta. : Universtiy of Lethbridge, Department of Geography
publishDate 2018
url https://hdl.handle.net/10133/5038
geographic Arctic
Canada
Greenland
geographic_facet Arctic
Canada
Greenland
genre Arctic
East Greenland
Greenland
genre_facet Arctic
East Greenland
Greenland
op_relation Thesis (University of Lethbridge. Faculty of Arts and Science)
https://hdl.handle.net/10133/5038
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