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Lowered ADCP current measurements during RV MARIA S. MERIAN cruise MSM107
Ocean velocity profiles were collected using an ADCP (300 kHz Teledyne RD Instruments Workhorse Sentinel ADCP) mounted on the CTD-Rosette during the Maria S. Merian cruise... -
Shipboard Acoustic Doppler Current Profiler measurements during R/V Littorina...
Vessel-mounted Acoustic Doppler Current Profiler (ADCP) measurements were carried out to acquire velocity profiles at two sites north (start: latitude & longitude:... -
Table 2: Firn temperature, ram resistance, mass balance and submergence velo ...
Distributional patterns of glaciological parameters at the Colle Gnifetti core drilling site are described and their interrelationships are brietly discussed. Observations... -
Passive surface drifter data in the bay of Sept-Îles in 2017-2018
Lagrangian drift data were gathered in the Bay of Sept-Îles during the Spring and Summer in 2017 and 2018, as part of the Canadian Healthy Oceans Network (CHONe II) program. The... -
Passive surface drifter data in the bay of Sept-Îles in 2003
Lagrangian drift data were gathered by Denis Lefaivre in the Bay of Sept-Îles in 2003 as part of work for the Department of Fisheries and Oceans, Canada (DFO). The drifters were... -
(Table 2) Picked maximum velocities from 3 radars (RAY, SHK, and SUM), showin...
We used a novel system of three continuous wave Doppler radars to successfully record the directivity of i) Strombolian explosions from the active lava lake of Erebus volcano,... -
Seagrass blue carbon stocks in the German Baltic Sea
A total of 169 sediment cores (30 cm length; 5.5 cm inner diameter) were sampled in seagrass meadows (n = 110 cores) and nearby unvegetated sediments (n = 59 cores). Nine cores... -
Current velocity magnitude data obtained by an ADCP (acoustic doppler current...
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Flow velocity magnitude from ADV 0.12 m above seabed at station HE441/07-1 fr...
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(Table 2) Surface height and flow velocities of Jakobshavn Isbræ, West Greenl...
Flow velocities were originally given in m/day and were recalculated to m/year by multiplying by 365. -
(Table 3) Spatial extent and length of main glacial channels for tributary gl...
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(Table 4) Seasonal variation of ice surface velocities of Vestfonna ice cap a...
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(Table 3) Geodetic and satellite derived ice surface velocities of Vestfonna ...
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(Table 2) Ice surface velocities of Vestfonna ice cap 2007-2010
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Summary of water depth, velocity magnitude and direction, shear velocity and ...
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(Table 5) Annual flow velocities at Nordenskiöldbreen glacier
GPS positions only approximate. Vav (m/yr) is calculated using Eq. (1), with np = nv = 240. A velocity year runs from day 91 to day 90 of the following year. Period refers to... -
(Table 4) GPS measured ice velocities at Nordenskiöldbreen glacier
GPS positions only approximate. Comparison between GPS and DGPS determined velocities of Nordenskioldbreen. Vav is calculated using Eq. (1), with np = nv = 240. Vbe is based on... -
(Table 2) Horizontal ice flow velocities, azimuths (relative to true north), ...
In the austral summer seasons 2001/02 and 2002/03, Global Positioning System (GPS) data were collected in the vicinity of Vostok Station to determine ice flow velocities over... -
Table 1: Discharge, mass flux, maximum velocity and ice thickness of glaciers...
Mass transport and mass flux values for the different types of glaciers in the Sør-Rondane are calculated from computer models, based upon gravity data and geodetic stake... -
Measured ice surface velocities on the King George Island ice cap with DGPS
King George Island is located at the northern tip of the Antarctic Peninsula, which is influenced by maritime climate conditions. The observed mean annual air temperature at sea...
