The North Pole to Greenland: A Scientific Transect

In April 2012 a team of four set out south from the North Pole, their destination: Greenland, over 700 km away; their aim: the intimate collection of never-before obtained data from beneath the ice; data that could verify the role that a changing Arctic may play in the greater Atlantic circulation,...

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Bibliographic Details
Main Author: McCallum, A B
Format: Conference Object
Language:English
Published: University of the Sunshine Coast 2012
Subjects:
Ice
Online Access:http://www.usc.edu.au/research/university-research-week
id ftunivscoast:usc:17989
record_format openpolar
spelling ftunivscoast:usc:17989 2023-05-15T14:43:19+02:00 The North Pole to Greenland: A Scientific Transect McCallum, A B 2012 http://www.usc.edu.au/research/university-research-week eng eng University of the Sunshine Coast usc:17989 FoR 0406 (Physical Geography and Environmental Geoscience) Greenland Conference Presentation 2012 ftunivscoast 2019-07-01T22:29:57Z In April 2012 a team of four set out south from the North Pole, their destination: Greenland, over 700 km away; their aim: the intimate collection of never-before obtained data from beneath the ice; data that could verify the role that a changing Arctic may play in the greater Atlantic circulation, with implications for the climate of Europe and beyond. That was the 2011 Catlin Arctic Survey, and I was one of that team. The aim of the 2011 Catlin Arctic Survey was to investigate how changes in the Arctic Ocean may impact the Atlantic thermohaline circulation; a global ocean circulation system that affects climate and weather patterns worldwide, driven by buoyancy differences because of changes in water temperature and salinity. Diminished extent and thickness of sea ice, thawing permafrost and increased rainfall and runoff from glaciers and rivers is increasing the amount of freshwater entering the Arctic Ocean; temperatures are rising and these processes may interrupt the driving and sinking mechanisms of Atlantic surface water. The expedition phase of the Survey consisted of a six-week overland traverse from the vicinity of the North Pole towards Greenland. The scientific routine included observations of sea ice morphology, measurement of ocean temperature and salinity to hundreds of metres beneath the ice and three-dimensional profiling of currents to a depth of 100 m. Measurements were obtained daily after manually drilling through the sea ice, sometimes in temperatures less than -50oC. Although preliminary analysis has occurred, the wealth of data obtained throughout this innovative survey are still undergoing scrutiny. The 2011 Catlin Arctic Survey was an audacious privately-funded research expedition, the results of which may shed new light on evolving climates within a changing world. Conference Object Arctic Arctic Ocean Greenland Ice North Pole permafrost Sea ice University of the Sunshine Coast, Queensland, Australia: COAST Research Database Arctic Arctic Ocean Greenland North Pole
institution Open Polar
collection University of the Sunshine Coast, Queensland, Australia: COAST Research Database
op_collection_id ftunivscoast
language English
topic FoR 0406 (Physical Geography and Environmental Geoscience)
Greenland
spellingShingle FoR 0406 (Physical Geography and Environmental Geoscience)
Greenland
McCallum, A B
The North Pole to Greenland: A Scientific Transect
topic_facet FoR 0406 (Physical Geography and Environmental Geoscience)
Greenland
description In April 2012 a team of four set out south from the North Pole, their destination: Greenland, over 700 km away; their aim: the intimate collection of never-before obtained data from beneath the ice; data that could verify the role that a changing Arctic may play in the greater Atlantic circulation, with implications for the climate of Europe and beyond. That was the 2011 Catlin Arctic Survey, and I was one of that team. The aim of the 2011 Catlin Arctic Survey was to investigate how changes in the Arctic Ocean may impact the Atlantic thermohaline circulation; a global ocean circulation system that affects climate and weather patterns worldwide, driven by buoyancy differences because of changes in water temperature and salinity. Diminished extent and thickness of sea ice, thawing permafrost and increased rainfall and runoff from glaciers and rivers is increasing the amount of freshwater entering the Arctic Ocean; temperatures are rising and these processes may interrupt the driving and sinking mechanisms of Atlantic surface water. The expedition phase of the Survey consisted of a six-week overland traverse from the vicinity of the North Pole towards Greenland. The scientific routine included observations of sea ice morphology, measurement of ocean temperature and salinity to hundreds of metres beneath the ice and three-dimensional profiling of currents to a depth of 100 m. Measurements were obtained daily after manually drilling through the sea ice, sometimes in temperatures less than -50oC. Although preliminary analysis has occurred, the wealth of data obtained throughout this innovative survey are still undergoing scrutiny. The 2011 Catlin Arctic Survey was an audacious privately-funded research expedition, the results of which may shed new light on evolving climates within a changing world.
format Conference Object
author McCallum, A B
author_facet McCallum, A B
author_sort McCallum, A B
title The North Pole to Greenland: A Scientific Transect
title_short The North Pole to Greenland: A Scientific Transect
title_full The North Pole to Greenland: A Scientific Transect
title_fullStr The North Pole to Greenland: A Scientific Transect
title_full_unstemmed The North Pole to Greenland: A Scientific Transect
title_sort north pole to greenland: a scientific transect
publisher University of the Sunshine Coast
publishDate 2012
url http://www.usc.edu.au/research/university-research-week
geographic Arctic
Arctic Ocean
Greenland
North Pole
geographic_facet Arctic
Arctic Ocean
Greenland
North Pole
genre Arctic
Arctic Ocean
Greenland
Ice
North Pole
permafrost
Sea ice
genre_facet Arctic
Arctic Ocean
Greenland
Ice
North Pole
permafrost
Sea ice
op_relation usc:17989
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