A Rosette for Sampling Ice-Covered Water

The Arctic Ocean is changing rapidly as Earth's climate warms. To document and understand these changing ocean conditions, we developed a rosette that collects high-quality oceanographic data and is deployed from an aircraft through a 30.5 cm diameter hole drilled in the ice (Figure 1). The ros...

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Bibliographic Details
Main Authors: William M. Smethie Jr., Dale Chayes, Richard Perry, Peter Schlosser, Ronny Friedrich
Format: Article in Journal/Newspaper
Language:English
Published: The Oceanography Society 2011
Subjects:
IPY
Online Access:https://doaj.org/article/37607e6f4fc94a3995d6ef80eaa00df5
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spelling ftdoajarticles:oai:doaj.org/article:37607e6f4fc94a3995d6ef80eaa00df5 2023-05-15T15:00:52+02:00 A Rosette for Sampling Ice-Covered Water William M. Smethie Jr. Dale Chayes Richard Perry Peter Schlosser Ronny Friedrich 2011-09-01T00:00:00Z https://doaj.org/article/37607e6f4fc94a3995d6ef80eaa00df5 EN eng The Oceanography Society http://tos.org/oceanography/archive/24-3_smethie.pdf https://doaj.org/toc/1042-8275 1042-8275 https://doaj.org/article/37607e6f4fc94a3995d6ef80eaa00df5 Oceanography, Vol 24, Iss 3, Pp 160-161 (2011) Arctic Ocean International Polar Year IPY rosette Oceanography GC1-1581 article 2011 ftdoajarticles 2022-12-31T02:13:19Z The Arctic Ocean is changing rapidly as Earth's climate warms. To document and understand these changing ocean conditions, we developed a rosette that collects high-quality oceanographic data and is deployed from an aircraft through a 30.5 cm diameter hole drilled in the ice (Figure 1). The rosette is modular, with the modules attached vertically on a conducting hydrowire to achieve a small diameter. Typically, three modules with four 4-liter bottles each are positioned above the conductivity-temperature-depth (CTD) module (Figure 2). The rosette package is lowered through the ice and retrieved at speeds up to 40 meters per minute using a small winch mounted in the aircraft. The hydrowire leads from the aircraft to a sheave hung from a tripod on the ice above the hole inside a tent that is heated to prevent water samples and sensors from freezing (Figure 3). The CTD data are acquired and displayed in real time on a laptop computer, and bottles are closed at desired depths electronically. Upon recovery, each water-bottle module is immediately placed in a cooler with bags of snow, which provide thermal stability within ± 2°C of the in situ temperature. The modules are returned to a base camp where they can be sampled and the samples processed under controlled conditions. A wide variety of water samples can be collected. Thus far, we have collected samples for salinity, dissolved oxygen, nutrients, helium isotopes, oxygen isotopes, chlorofluorocarbons, SF6, tritium, CO2, barium, and 129I. The quality of all samples has been excellent. Smethie et al. (2011) provide a detailed description of the rosette and its performance. Article in Journal/Newspaper Arctic Arctic Ocean International Polar Year IPY Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic Ocean
International Polar Year
IPY
rosette
Oceanography
GC1-1581
spellingShingle Arctic Ocean
International Polar Year
IPY
rosette
Oceanography
GC1-1581
William M. Smethie Jr.
Dale Chayes
Richard Perry
Peter Schlosser
Ronny Friedrich
A Rosette for Sampling Ice-Covered Water
topic_facet Arctic Ocean
International Polar Year
IPY
rosette
Oceanography
GC1-1581
description The Arctic Ocean is changing rapidly as Earth's climate warms. To document and understand these changing ocean conditions, we developed a rosette that collects high-quality oceanographic data and is deployed from an aircraft through a 30.5 cm diameter hole drilled in the ice (Figure 1). The rosette is modular, with the modules attached vertically on a conducting hydrowire to achieve a small diameter. Typically, three modules with four 4-liter bottles each are positioned above the conductivity-temperature-depth (CTD) module (Figure 2). The rosette package is lowered through the ice and retrieved at speeds up to 40 meters per minute using a small winch mounted in the aircraft. The hydrowire leads from the aircraft to a sheave hung from a tripod on the ice above the hole inside a tent that is heated to prevent water samples and sensors from freezing (Figure 3). The CTD data are acquired and displayed in real time on a laptop computer, and bottles are closed at desired depths electronically. Upon recovery, each water-bottle module is immediately placed in a cooler with bags of snow, which provide thermal stability within ± 2°C of the in situ temperature. The modules are returned to a base camp where they can be sampled and the samples processed under controlled conditions. A wide variety of water samples can be collected. Thus far, we have collected samples for salinity, dissolved oxygen, nutrients, helium isotopes, oxygen isotopes, chlorofluorocarbons, SF6, tritium, CO2, barium, and 129I. The quality of all samples has been excellent. Smethie et al. (2011) provide a detailed description of the rosette and its performance.
format Article in Journal/Newspaper
author William M. Smethie Jr.
Dale Chayes
Richard Perry
Peter Schlosser
Ronny Friedrich
author_facet William M. Smethie Jr.
Dale Chayes
Richard Perry
Peter Schlosser
Ronny Friedrich
author_sort William M. Smethie Jr.
title A Rosette for Sampling Ice-Covered Water
title_short A Rosette for Sampling Ice-Covered Water
title_full A Rosette for Sampling Ice-Covered Water
title_fullStr A Rosette for Sampling Ice-Covered Water
title_full_unstemmed A Rosette for Sampling Ice-Covered Water
title_sort rosette for sampling ice-covered water
publisher The Oceanography Society
publishDate 2011
url https://doaj.org/article/37607e6f4fc94a3995d6ef80eaa00df5
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
International Polar Year
IPY
genre_facet Arctic
Arctic Ocean
International Polar Year
IPY
op_source Oceanography, Vol 24, Iss 3, Pp 160-161 (2011)
op_relation http://tos.org/oceanography/archive/24-3_smethie.pdf
https://doaj.org/toc/1042-8275
1042-8275
https://doaj.org/article/37607e6f4fc94a3995d6ef80eaa00df5
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