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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... -
GIS mapping of the moraines of the Mont-Blanc and Aiguilles Rouges massifs
This dataset is a shapefile (polyline) of the moraine ridges of the Mont-Blanc and Aiguilles-Rouges massifs (French, Italian and Swiss Alps) intended to be as exhaustive as... -
Vector dataset of manually mapped retrogressive thaw slumps from very high-re...
We present a comprehensive inventory of retrogressive thaw slumps (RTS) for six study sites in the Russian High Arctic covering an area of more than 600 km². The sites are... -
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... -
The GeoMAP (v.2022-08) continent-wide detailed geological dataset of Antarctica
A dataset describing exposed bedrock and surficial geology of Antarctica constructed by the GeoMAP Action Group of SCAR (The Scientific Committee on Antarctic Research) and GNS... -
Known mapped areas of seagrass (Zostera marina & Zostera noltii) meadows arou...
Since 1998, approximately 148,134,806 m2 (14,813.5 Ha) of seagrass habitat has been mapped across the United Kingdom coastline. This was calculated from a total of 1,872... -
(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).