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Multibeam echosounder data used for Seasonal Change of Multifrequency Backsca...
Multibeam snippet raw data were recorded using a Norbit STX WBMS multibeam echosounder mounted to the side of the 6.5 m-long aluminum catamaran KLAASHAHN. Data were recorded... -
Five Radiometric Landscape of Kerguelen Islands
Landscape mapping is crucial for monitoring and understanding a wide range of ecological and social processes, as well as for addressing major issues such as land use... -
Manually mapped retrogressive thaw slumps in West Siberia, version 0.1
This dataset presents a comprehensive update to the inventory of retrogressive thaw slumps (RTS) in northern West Siberia, achieved through meticulous manual mapping. RTS sites... -
Habitat suitability maps for vulnerable and foundation cold-water coral taxa ...
We developed habitat suitability models for 14 vulnerable and foundation cold-water coral (CWC) taxa of the Azores (NE Atlantic) using GAM and MAXENT models. The modelled taxa... -
Multibeam bathymetry raw data (Norbit STX WBMS entire dataset) of KLAASHAHN d...
Multibeam snippet raw data were recorded using a Norbit STX WBMS multibeam echosounder mounted to the side of the 6.5 m-long aluminum catamaran KLAASHAHN. Data were recorded... -
Multibeam bathymetry raw data (Norbit STX WBMS entire dataset) of KLAASHAHN d...
Multibeam snippet raw data were recorded using a Norbit STX WBMS multibeam echosounder mounted to the side of the 6.5 m-long aluminum catamaran KLAASHAHN. Data were recorded... -
Multibeam bathymetry raw data (Norbit STX WBMS entire dataset) of KLAASHAHN d...
Multibeam snippet raw data were recorded using a Norbit STX WBMS multibeam echosounder mounted to the side of the 6.5 m-long aluminum catamaran KLAASHAHN. Data were recorded... -
Glacial landforms in the region formerly occupied by the Haslach glacier, sou...
This dataset contains ESRI shapefiles of mapped glacial landforms, i.e., initial cirques, cirques, moraines, and moraine crests in the region formerly occupied by the former... -
(Figure 10b, 11) Benthic electromagnetic profile of GeoB130106 on the northwe...
Porosity is derived from Archie's law with constants m = 1.6, a = 1 and 14.4% offset (susceptibility with 37.7 offset; based on Figure 9). -
(Figure 10a, 11, 12) Benthic electromagnetic profile of GeoB130124 on the nor...
Porosity is derived from Archie's law with constants m = 1.6, a = 1 and 14.4% offset (susceptibility with 37.7 offset; based on Figure 9). -
(Figure 9b) Correlation of EM and sediment core susceptibility
This dataset has no description
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(Figure 9a) Correlation of EM and sediment core porosity
EM Porosity is derived from Archie's law with constants m = 1.6 and a = 1. -
(Figure 7b) Apparent susceptibility profiles by various available sensor size...
Assumption: magnetite dissolution sets in at depths of 0.2-0.8 m and is completed 0.2 m deeper. -
(Figure 7a) Simulations of apparent susceptibility and conductivity profiles ...
This dataset has no description
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(Figure 6b) Horizontal footprint diameter (90% of the total signal) and half-...
This dataset has no description
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(Figure 6a) Lateral response of GEM-3 sensor (96 cm coil) for susceptibility ...
This dataset has no description
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(Figure 5c) In-phase and quadrature responses of GEM-3 sensor at various oper...
The models are based on 0.1% perturbations of an homogenous seafloor model with seawater (and sediment) conductivities/susceptibilities of 3 S/m and -9 x 10-6 (1 S/m and 100 x... -
(Figure 5b) Vertical sensor characteristics of GEM-3 (96 cm coil) for quadrat...
The models are based on 0.1% perturbations of an homogenous seafloor model with seawater (and sediment) conductivities/susceptibilities of 3 S/m and -9 x 10-6 (1 S/m and 100 x... -
(Figure 4a) Relative contribution of the magnetic response to total in-phase ...
This dataset has no description
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(Figure 3) Modeled GEM-3 susceptibility and conductivity response under decre...
This model result assumes that the sensor emerges from an infinite seawater half-space (kappa w = -9 x 10**-6 and Sigma w = 3 S/m; susceptibility in SI-units).
