ICEX buoy drift data 1976-1979

A Norwegian Ice Drift Experiment (ICEX) started in 1976 as part of a national contribution to the polar programmes under the Global Atmospheric Research Programme (GARP). The main aim of the experiment is to obtain information on an important climatic parameter: the export of ice from the Arctic Oce...

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Bibliographic Details
Main Authors: Vinje, Torgny, Finnekåsa, Øyvind, Helgeland, Conrad
Format: Dataset
Language:unknown
Published: Norwegian Polar Institute 2016
Subjects:
Online Access:http://data.npolar.no/dataset/dbf2b6b1-3cbf-444d-b363-eadbe1e938c0
id npolardata:oai:npolar.no:dataset/dbf2b6b1-3cbf-444d-b363-eadbe1e938c0
record_format openpolar
institution Open Polar
collection Norwegian Polar Data Centre
op_collection_id npolardata
language unknown
topic OCEANS
Trajectory
oceanography
EARTH SCIENCE
ATMOSPHERE
ATMOSPHERIC PRESSURE
ATMOSPHERIC PRESSURE MEASUREMENTS
ATMOSPHERIC TEMPERATURE
AIR TEMPERATURE
SALINITY/DENSITY
spellingShingle OCEANS
Trajectory
oceanography
EARTH SCIENCE
ATMOSPHERE
ATMOSPHERIC PRESSURE
ATMOSPHERIC PRESSURE MEASUREMENTS
ATMOSPHERIC TEMPERATURE
AIR TEMPERATURE
SALINITY/DENSITY
Vinje, Torgny
Finnekåsa, Øyvind
Helgeland, Conrad
ICEX buoy drift data 1976-1979
topic_facet OCEANS
Trajectory
oceanography
EARTH SCIENCE
ATMOSPHERE
ATMOSPHERIC PRESSURE
ATMOSPHERIC PRESSURE MEASUREMENTS
ATMOSPHERIC TEMPERATURE
AIR TEMPERATURE
SALINITY/DENSITY
description A Norwegian Ice Drift Experiment (ICEX) started in 1976 as part of a national contribution to the polar programmes under the Global Atmospheric Research Programme (GARP). The main aim of the experiment is to obtain information on an important climatic parameter: the export of ice from the Arctic Ocean through the Fram Strait. The project was reorganized in 1981, and became a joint programme between Norsk Polarinstitutt and Det norske meteorologiske institutt, also involving cooperation with the University of Washington's Arctic Ocean Buoy Program. An ICEX measuring capsule has been developed in cooperation with Chr. Michelsens Institutt, Bergen, (Vinje & Steinbakke 1976, Nergaard et al. 1985). The capsule operates effectively in the marginal sea ice areas where it may be subject to frequent ridging and sporadic drift in water. The buoys were deployed from a boat in a pilot project in 1975, from a Cessna 185 aircraft landing on the ice in 1976 and 1977, and they have been air-dropped by the Norwegian Air Force from 1978 onwards. Since 1981 data from the Norwegian buoys have been included in the Arctic Ocean Buoy Program data reports edited by the Polar Science Center, University of Washington. The present data report contains drift tracks and daily values of positions, air pressure (P) mb, air temperatures (TA) about 80 cm above the ice surface, and temperatures (TB) at the bottom of the ICEX capsule. The latter information indicates if the measuring capsule is on the ice or in the water. When free floating, (TB) gives the temperature about 40 cm below the sea surface. During the first five years of the experiment, the air pressure sensors were built at the Norwegian Meteorological Institute, based on an aneroid and a displacement transducer. Another Norwegian pressure transducer has been produced by Aanderaa Instruments. This is based on a silicon chip as sensing element. The Digiquarts pressure sensor from the US firm Paro Scientific has also been used since 1981. The sensor resolution is hetter than 0.1 mb, while the system resolution is 0.4 mb within the normal variation range of the meteorological variables. Series of comparisons in the field showed that the mean difference between the data obtained via Nimbus-6 and the readings on a test set was less than 0.1 mb (Vinje 1978). Later comparisons showed differences of about 1 mb (Vinje 1981). This was, however, well inside the FGGE requirements. The temperature is measured with a radiation shielded termistor. Fenwal UUA 3213. The system resolution is 0.2°C. The ventilation of the sensor is dependent upon the wind speed, and the sensor signal is also dependent upon the heating of the capsule. A series of comparisons in the field showed that the temperatures were correct within ±0.1 °C during conditions with normal ventilation (Vinje 1981). A comparison on Fram Ill (Thorndike et al. 1982) during part of April 1981 indicated temperatures as much as 1 °C - 2°C too high during the warmest part of each day. Otherwise the daily cycle was well resolved and the temperature readings from the ICEX buoy agreed well with the met observer's data. References ========= Nergaard, N., Vinje, T. & Finnekåsa, Ø. 1985: Report on ice buoys in theArctic and the Antarctic. Report No. 851129-1 from Chr. Michelsens institutt, Bergen. Thorndike, A. S., Colony, R. & Munoz, E. A. 1982: [Arctic Ocean Buoy Program. Data Report 1 January 1981 - 31 December 1981](http://iabp.apl.washington.edu/pdfs/AOBP1981Thorndike.pdf). Polar Science Center, University of Washington, Seattle. Vinje, T. E. 1978: Weather and tide observations at Bouvetøya. Norsk Polarinstitutt [Skrifter 169](http://hdl.handle.net/11250/173571). Vinje, T. E. 1981: Meteorological observations from Bouvetøya. Norsk Polarinstitutt [Skrifter 175](http://hdl.handle.net/11250/173651). Vinje, T. E. & Steinbakke, P. 1976: Nimbus-6 located automatic stations in the Svalbard waters in 1975. [Norsk Polarinstitutt Årbok 1975](http://hdl.handle.net/11250/172804).
format Dataset
author Vinje, Torgny
Finnekåsa, Øyvind
Helgeland, Conrad
author_facet Vinje, Torgny
Finnekåsa, Øyvind
Helgeland, Conrad
author_sort Vinje, Torgny
title ICEX buoy drift data 1976-1979
title_short ICEX buoy drift data 1976-1979
title_full ICEX buoy drift data 1976-1979
title_fullStr ICEX buoy drift data 1976-1979
title_full_unstemmed ICEX buoy drift data 1976-1979
title_sort icex buoy drift data 1976-1979
publisher Norwegian Polar Institute
publishDate 2016
url http://data.npolar.no/dataset/dbf2b6b1-3cbf-444d-b363-eadbe1e938c0
op_coverage BEGINDATE: 1976-01-01 ENDDATE: 1979-12-01
ENVELOPE(-26.28,52.12,83.86,70.61)
long_lat ENVELOPE(3.358,3.358,-54.422,-54.422)
ENVELOPE(14.450,14.450,68.620,68.620)
ENVELOPE(-26.28,52.12,83.86,70.61)
geographic Antarctic
Arctic
Arctic Ocean
Bergen
Bouvetøya
Svalbard
The Antarctic
Vinje
geographic_facet Antarctic
Arctic
Arctic Ocean
Bergen
Bouvetøya
Svalbard
The Antarctic
Vinje
genre Antarc*
Antarctic
Arctic
Arctic Ocean
Bouvetøya
Fram Strait
Norsk Polarinstitutt
Polar Science Center
Polar Science Center, University of Washington
Sea ice
Svalbard
genre_facet Antarc*
Antarctic
Arctic
Arctic Ocean
Bouvetøya
Fram Strait
Norsk Polarinstitutt
Polar Science Center
Polar Science Center, University of Washington
Sea ice
Svalbard
_version_ 1792545109048295424
spelling npolardata:oai:npolar.no:dataset/dbf2b6b1-3cbf-444d-b363-eadbe1e938c0 2024-03-03T22:15:36+00:00 ICEX buoy drift data 1976-1979 Vinje, Torgny Finnekåsa, Øyvind Helgeland, Conrad BEGINDATE: 1976-01-01 ENDDATE: 1979-12-01 ENVELOPE(-26.28,52.12,83.86,70.61) 2016-11-07 application/pdf application/zip http://data.npolar.no/dataset/dbf2b6b1-3cbf-444d-b363-eadbe1e938c0 unknown Norwegian Polar Institute OCEANS Trajectory oceanography EARTH SCIENCE ATMOSPHERE ATMOSPHERIC PRESSURE ATMOSPHERIC PRESSURE MEASUREMENTS ATMOSPHERIC TEMPERATURE AIR TEMPERATURE SALINITY/DENSITY Dataset 2016 npolardata 2023-07-25T13:05:10Z A Norwegian Ice Drift Experiment (ICEX) started in 1976 as part of a national contribution to the polar programmes under the Global Atmospheric Research Programme (GARP). The main aim of the experiment is to obtain information on an important climatic parameter: the export of ice from the Arctic Ocean through the Fram Strait. The project was reorganized in 1981, and became a joint programme between Norsk Polarinstitutt and Det norske meteorologiske institutt, also involving cooperation with the University of Washington's Arctic Ocean Buoy Program. An ICEX measuring capsule has been developed in cooperation with Chr. Michelsens Institutt, Bergen, (Vinje & Steinbakke 1976, Nergaard et al. 1985). The capsule operates effectively in the marginal sea ice areas where it may be subject to frequent ridging and sporadic drift in water. The buoys were deployed from a boat in a pilot project in 1975, from a Cessna 185 aircraft landing on the ice in 1976 and 1977, and they have been air-dropped by the Norwegian Air Force from 1978 onwards. Since 1981 data from the Norwegian buoys have been included in the Arctic Ocean Buoy Program data reports edited by the Polar Science Center, University of Washington. The present data report contains drift tracks and daily values of positions, air pressure (P) mb, air temperatures (TA) about 80 cm above the ice surface, and temperatures (TB) at the bottom of the ICEX capsule. The latter information indicates if the measuring capsule is on the ice or in the water. When free floating, (TB) gives the temperature about 40 cm below the sea surface. During the first five years of the experiment, the air pressure sensors were built at the Norwegian Meteorological Institute, based on an aneroid and a displacement transducer. Another Norwegian pressure transducer has been produced by Aanderaa Instruments. This is based on a silicon chip as sensing element. The Digiquarts pressure sensor from the US firm Paro Scientific has also been used since 1981. The sensor resolution is hetter than 0.1 mb, while the system resolution is 0.4 mb within the normal variation range of the meteorological variables. Series of comparisons in the field showed that the mean difference between the data obtained via Nimbus-6 and the readings on a test set was less than 0.1 mb (Vinje 1978). Later comparisons showed differences of about 1 mb (Vinje 1981). This was, however, well inside the FGGE requirements. The temperature is measured with a radiation shielded termistor. Fenwal UUA 3213. The system resolution is 0.2°C. The ventilation of the sensor is dependent upon the wind speed, and the sensor signal is also dependent upon the heating of the capsule. A series of comparisons in the field showed that the temperatures were correct within ±0.1 °C during conditions with normal ventilation (Vinje 1981). A comparison on Fram Ill (Thorndike et al. 1982) during part of April 1981 indicated temperatures as much as 1 °C - 2°C too high during the warmest part of each day. Otherwise the daily cycle was well resolved and the temperature readings from the ICEX buoy agreed well with the met observer's data. References ========= Nergaard, N., Vinje, T. & Finnekåsa, Ø. 1985: Report on ice buoys in theArctic and the Antarctic. Report No. 851129-1 from Chr. Michelsens institutt, Bergen. Thorndike, A. S., Colony, R. & Munoz, E. A. 1982: [Arctic Ocean Buoy Program. Data Report 1 January 1981 - 31 December 1981](http://iabp.apl.washington.edu/pdfs/AOBP1981Thorndike.pdf). Polar Science Center, University of Washington, Seattle. Vinje, T. E. 1978: Weather and tide observations at Bouvetøya. Norsk Polarinstitutt [Skrifter 169](http://hdl.handle.net/11250/173571). Vinje, T. E. 1981: Meteorological observations from Bouvetøya. Norsk Polarinstitutt [Skrifter 175](http://hdl.handle.net/11250/173651). Vinje, T. E. & Steinbakke, P. 1976: Nimbus-6 located automatic stations in the Svalbard waters in 1975. [Norsk Polarinstitutt Årbok 1975](http://hdl.handle.net/11250/172804). Dataset Antarc* Antarctic Arctic Arctic Ocean Bouvetøya Fram Strait Norsk Polarinstitutt Polar Science Center Polar Science Center, University of Washington Sea ice Svalbard Norwegian Polar Data Centre Antarctic Arctic Arctic Ocean Bergen Bouvetøya ENVELOPE(3.358,3.358,-54.422,-54.422) Svalbard The Antarctic Vinje ENVELOPE(14.450,14.450,68.620,68.620) ENVELOPE(-26.28,52.12,83.86,70.61)