Academic literature on the topic 'Winter-Weddell-Sea Project 1986'

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Journal articles on the topic "Winter-Weddell-Sea Project 1986"

1

Hempel, G. "Antarctic marine research in winter: the Winter Weddell Sea Project 1986." Polar Record 24, no. 148 (1988): 43–48. http://dx.doi.org/10.1017/s0032247400022336.

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AbstractFrom austral autumn to spring 1986 the West German research ship RV Polarstern made three consecutive cruises to Antarctica in 1986; of these the second and third (27 June–14 December) made up the Winter Weddell Sea Projet, the first detailed winter survey of the pack ice, oceanography and biota of the offshore and eastern coastal Weddell Sea south to 76°S. This article briefly describes the ship and outlines the scientific programme, which involved 137 scientists and technicians from 12 German and 16 non-German institutions. In the cruise of 27 June–17 September research was centred o
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2

Wadhams, P., C. B. Sear, D. R. Crane, M. A. Rowe, S. J. Morrison, and D. W. S. Limbert. "Basin-Scale Ice Motion and Deformation in the Weddell Sea During Winter." Annals of Glaciology 12 (1989): 178–86. http://dx.doi.org/10.3189/s0260305500007163.

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Ice motion in the Weddell Sea is examined for the period 19 August (Day 232) to 12 October (Day 286) 1986 using the tracks of four Argos buoys deployed during the Winter Weddell Sea Project 1986 (WWSP 86). Two were SPRI/BAS buoys, launched in December 1985 and March 1986 in the south-east and north-west Weddell Sea. The others were part of a mesoscale array deployed in the Maud Rise area by H. Hoeber of the Meteorologisches Institut der Universität Hamburg, during the WWSP 86 cruise of FS Polarstern. The four buoys operated together for 44 d, comprising a basin-scale quadrilateral from which t
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3

Wadhams, P., C. B. Sear, D. R. Crane, M. A. Rowe, S. J. Morrison, and D. W. S. Limbert. "Basin-Scale Ice Motion and Deformation in the Weddell Sea During Winter." Annals of Glaciology 12 (1989): 178–86. http://dx.doi.org/10.1017/s0260305500007163.

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Abstract:
Ice motion in the Weddell Sea is examined for the period 19 August (Day 232) to 12 October (Day 286) 1986 using the tracks of four Argos buoys deployed during the Winter Weddell Sea Project 1986 (WWSP 86). Two were SPRI/BAS buoys, launched in December 1985 and March 1986 in the south-east and north-west Weddell Sea. The others were part of a mesoscale array deployed in the Maud Rise area by H. Hoeber of the Meteorologisches Institut der Universität Hamburg, during the WWSP 86 cruise of FS Polarstern. The four buoys operated together for 44 d, comprising a basin-scale quadrilateral from which t
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4

Limbert, D. W. S., S. J. Morrison, C. B. Sear, P. Wadhams, and M. A. Rowe. "Pack-Ice Motion in the Weddell Sea in Relation to Weather Systems and Determination of a Weddell Sea Sea-Ice Budget." Annals of Glaciology 12 (1989): 104–12. http://dx.doi.org/10.3189/s0260305500007047.

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As part of the Winter Weddell Sea Project 1986 (WWSP 86), a buoy, transmitting via TIROS-N satellites to Service Argos, was inserted into an ice floe in the southern Weddell Sea. Operational U.K. Meteorological Office numerical surface-pressure analyses, which utilized the buoy’s measured values of air pressure and temperature, are used to assess the impact of weather systems on pack-ice movement. The motion of the buoy is shown to be related closely to the position of the circumpolar trough and to the tracks of depressions crossing the area. The tracks of this and other buoys deployed during
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5

Limbert, D. W. S., S. J. Morrison, C. B. Sear, P. Wadhams, and M. A. Rowe. "Pack-Ice Motion in the Weddell Sea in Relation to Weather Systems and Determination of a Weddell Sea Sea-Ice Budget." Annals of Glaciology 12 (1989): 104–12. http://dx.doi.org/10.1017/s0260305500007047.

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Abstract:
As part of the Winter Weddell Sea Project 1986 (WWSP 86), a buoy, transmitting via TIROS-N satellites to Service Argos, was inserted into an ice floe in the southern Weddell Sea. Operational U.K. Meteorological Office numerical surface-pressure analyses, which utilized the buoy’s measured values of air pressure and temperature, are used to assess the impact of weather systems on pack-ice movement. The motion of the buoy is shown to be related closely to the position of the circumpolar trough and to the tracks of depressions crossing the area. The tracks of this and other buoys deployed during
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6

Lange, M. A., S. F. Ackley, P. Wadhams, G. S. Dieckmann, and H. Eicken. "Development of Sea Ice in the Weddell Sea." Annals of Glaciology 12 (1989): 92–96. http://dx.doi.org/10.3189/s0260305500007023.

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We report on the development and physical properties of sea ice in the central and eastern Weddell Sea. The investigations were part of the Winter Weddell Sea Project 1986, which extended over the months of July through December. Major elements of the glaciological part of this study included continuous shipborne observations of sea-ice conditions and occasional helicopter reconnaissance flights, extensive measurements of snow and ice thicknesses at daily ice stations, and detailed analyses of sampled ice cores from each ice station. Textural investigations of the sampled ice revealed the domi
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7

Lange, M. A., S. F. Ackley, P. Wadhams, G. S. Dieckmann, and H. Eicken. "Development of Sea Ice in the Weddell Sea." Annals of Glaciology 12 (1989): 92–96. http://dx.doi.org/10.1017/s0260305500007023.

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Abstract:
We report on the development and physical properties of sea ice in the central and eastern Weddell Sea. The investigations were part of the Winter Weddell Sea Project 1986, which extended over the months of July through December. Major elements of the glaciological part of this study included continuous shipborne observations of sea-ice conditions and occasional helicopter reconnaissance flights, extensive measurements of snow and ice thicknesses at daily ice stations, and detailed analyses of sampled ice cores from each ice station. Textural investigations of the sampled ice revealed the domi
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8

Lange, Μ. A., P. Schlosser, S. F. Ackley, P. Wadhams, and G. S. Dieckmann. "18O Concentrations In Sea Ice Of The Weddell Sea, Antarctica." Journal of Glaciology 36, no. 124 (1990): 315–23. http://dx.doi.org/10.3189/002214390793701291.

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AbstractWe present data on ice texture, salinity, and δ18O obtained from identical sections of ice cores during the Winter Weddell Sea Project 1986 on RV Polarstern from July through August 1986, in the longitude range between 5°W. and 7°E. We find no uniquely definable relationship between δ18O values and ice texture in a particular section. However, most of the snow ice as well as some sections of frazil ice are found to have negative δ18O concentrations. This is due to varying degrees of admixtures of meteoric ice (snow) and sea-water during formation of snow ice. In contrast to common assu
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9

Squire, Vernon A. "Super-Critical Reflection of Ocean Waves; A New Factor in Ice-Edge Dynamics?" Annals of Glaciology 12 (1989): 157–61. http://dx.doi.org/10.3189/s0260305500007138.

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Movement of the sea-ice edge on short time-scales (<1 d) is due to a balance of forces between several mechanisms (wind stress, sea-surface tilt, internal ice stress, and Coriolis force) which are often comparable in magnitude. Other factors such as the force induced by partial reflection of short seas, internal gravity waves in the pycnocline, etc., may also contribute. Through the momentum equation, these mechanisms affect the dynamics of the ice edge. In this paper we suggest another mechanism which may have importance, namely, a radiation-stress contribution which derives from obliquely
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10

Squire, Vernon A. "Super-Critical Reflection of Ocean Waves; A New Factor in Ice-Edge Dynamics?" Annals of Glaciology 12 (1989): 157–61. http://dx.doi.org/10.1017/s0260305500007138.

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Abstract:
Movement of the sea-ice edge on short time-scales (<1 d) is due to a balance of forces between several mechanisms (wind stress, sea-surface tilt, internal ice stress, and Coriolis force) which are often comparable in magnitude. Other factors such as the force induced by partial reflection of short seas, internal gravity waves in the pycnocline, etc., may also contribute. Through the momentum equation, these mechanisms affect the dynamics of the ice edge. In this paper we suggest another mechanism which may have importance, namely, a radiation-stress contribution which derives from obliq
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Books on the topic "Winter-Weddell-Sea Project 1986"

1

Hoeber, Heinrich. The eastern Weddell Sea drifting buoy data set of the Winter Weddell Sea Project (WWSP) 1986. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1987.

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2

Rabe, Werner. Weather and synoptic situation during Winter Weddell Sea Project 1986 (ANT V/2), July 16-September 10, 1986. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1987.

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3

Eberhard, Fahrbach, ed. Meteorological and oceanographic data of the Winter-Weddell-Sea Project 1986 (ANT V/3). Alfred Wegener Institute for Polar and Marine Research, 1988.

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4

Meteorological and oceanographic data of the Winter-Weddell-Sea Project 1986 (ANT V/3). Alfred-Wegener-Institut für Polar- und Meeresforschung, 1988.

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