658,300 Works

Physical properties of sediment core PS55/096-2

Michael Pirrung

PKDB150132

A A Huaraz & S Hastenrath

Snowline in 1990 on Pico de Teide (PKDB149242), supplement to: Becht, M; Trimborn, Peter (1992): Isotopenhydrologische Untersuchungen der Schneedecke am Pico de Teide (Teneriffa). Zeitschrift für Gletscherkunde und Glazialgeologie, 28, 151-163

M Becht & Peter Trimborn
Meteorologische Messungen am Pico de Teide (Teneriffa) ergaben für die Hochlagen (> 2800 m ü. d. M.) ein Dampfdruckgefälle von der Schneedeckenoberfläche zur Atmosphäre. Damit sind Voraussetzungen für den Abbau der Schneedecke auch durch Verdunstung und Sublimation gegeben. Isotopenhydrologische Untersuchungen der Schneedecke bestätigen diese Energie- und Massenumsätze. 2H und 180 zeigen eine deutliche Anreicherung an der Oberfläche während des gesamten Meßzeitraumes. In tiefen Lagen um 2400 m ü. d. M. alternieren Verdunstung, Kondensation und Schmelze,...

Volume susceptibility on ODP Hole 114-701B

Paul F Ciesielski &

Volume susceptibility on ODP Hole 114-703A

Paul F Ciesielski &

Volume susceptibility on ODP Hole 114-704B

Paul F Ciesielski &

PKDB161354

S Jianzhong

Hydrochemistry measured on water bottle samples at station A4/93_62 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station A4/93_64 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station A8/93_156 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station A8/93_158 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station A8/93_159 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station B10/93_820 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station B13/93_994 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station B14/93_1001 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station B1/94_1 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station B2/93_142 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station B5/93_186 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station B8/93_548 during the Irminger Sea seasonal study

Jón Ólafsson

Hydrochemistry measured on water bottle samples at station A2/90_88 during the MRI-LDEO cooperative study

Jón Ólafsson & Taro Takahashi
For pCO2 measurements were about 0.5 liter of air equilibrated with sample. Sample volume 4. Nutrient samples are collected in 250 ml soft low density polyethylene acid washed bottles. They are kept refrigerated until analysis if it was not carried out soon after sampling. Otherwisee samples are stored at -20°C.

Hydrochemistry measured on water bottle samples at station A3/88_120 during the MRI-LDEO cooperative study

Jón Ólafsson & Taro Takahashi
For pCO2 measurements were about 0.5 liter of air equilibrated with sample. Sample volume 4. Nutrient samples are collected in 250 ml soft low density polyethylene acid washed bottles. They are kept refrigerated until analysis if it was not carried out soon after sampling. Otherwisee samples are stored at -20°C.

Hydrochemistry measured on water bottle samples at station A3/88_62 during the MRI-LDEO cooperative study

Jón Ólafsson & Taro Takahashi
For pCO2 measurements were about 0.5 liter of air equilibrated with sample. Sample volume 4. Nutrient samples are collected in 250 ml soft low density polyethylene acid washed bottles. They are kept refrigerated until analysis if it was not carried out soon after sampling. Otherwisee samples are stored at -20°C.

Hydrochemistry measured on water bottle samples at station B12/83_1054 during the MRI-LDEO cooperative study

Jón Ólafsson & Taro Takahashi
For pCO2 measurements were about 0.5 liter of air equilibrated with sample. Sample volume 4. Nutrient samples are collected in 250 ml soft low density polyethylene acid washed bottles. They are kept refrigerated until analysis if it was not carried out soon after sampling. Otherwisee samples are stored at -20°C.

Hydrochemistry measured on water bottle samples at station B7/84_707 during the MRI-LDEO cooperative study

Jón Ólafsson & Taro Takahashi
For pCO2 measurements were about 0.5 liter of air equilibrated with sample. Sample volume 4. Nutrient samples are collected in 250 ml soft low density polyethylene acid washed bottles. They are kept refrigerated until analysis if it was not carried out soon after sampling. Otherwisee samples are stored at -20°C.

(Table 3) Sedimentation rates of stage 1 and last glacial maximum from different Holes during cruises of RRS Discovery in 1984-1985 and 1987-1988, and RRS James Clark Ross in 1992-1993

Carol J Pudsey & John Howe
Within the Scotia Sea, the axis of the Antarctic Circumpolar Current (ACC) is geographically confined, and sediments therefore contain a record of palaeo-flow speed uncomplicated by ACC axis migration. We outline Holocene and Last Glacial Maximum (LGM) current-controlled sedimentation using data from 3.5-kHz profiles, cores and current meter moorings. Geophysical surveys show areas of erosion and deposition controlled by Neogene basement topography. Deposition occurs in mounded sediment drifts or flatter areas, where 500-1000 m of...

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