Satellite Derived Bathymetry Crete - Greece
Data provides bathymetric information based on Landsat 8 satellite at 15 m resolution.
Data were processed by the Modular and Inversion System (MIP) by EOMAP GmbH Co.KG. MIP is designed for the physically based assessment of hydro-biological parameters from multi- and hyperspectral remote sensing data.
Supplemental_Information:
EOMAPs Satellite Derived Bathymetry (SDB) method relies on the reflected light energy which is measured at the satellite sensor in space. In order to measure the water column thickness, the sea bottom reflection must be separated from all other simultaneously measured portions of light. Other contributors of light scattered to the sensor are atmospheric molecules and aerosols, adjacent scattering from land, the water surface reflection, and light scattered and absorbed due to particular properties of water constituents and the pure water itself. The pure water itself also absorbs light in a spectrally specific manner and therefore leaves unique signatures in the signal while the light passes through the water column and returns after reflection at the sea bottom. This property is relevant to estimate water depth from optical satellite imagery. As many properties can vary over space and time, effective correction, regularization and retrieval algorithms must be applied to avoid instable results. EOMAP developed and maintains these unique algorithm and its workflows for almost 2 decades. The maximum depth the system is able to sense is related to the complex interaction of radiance of bottom material, incident sun angle and intensity, and the type and quantity of organics or sediments in the water column. As a rule-of-thumb, satellite derived bathymetry should be capable of sensing bottom to depths equal to one to one point five times the Secchi depth.
no-data-value optically deep water: -9999
What
Metadata details
- File identifier
- SDN_CPRD_4667_greece1001
- Catalogue type
-
Composite Product Record
-
Project name
-
-
EMODNet Bathymetry
-
- Dissemination level
-
public
- Metadata language
- English
- Date stamp
- 2019-12-18T10:16:47
Identification
- Dataset name
-
Satellite Derived Bathymetry Crete - Greece
- Short name of dataset (SDN Local Product-ID)
-
greece1001
-
Parameter Discovery Vocabulary (P02)
-
-
Bathymetry and Elevation
-
-
SeaDataNet device categories
-
-
cameras
-
Geometry
- Spatial representation type
- Grid
- Number of columns
- 18965
- Number of lines
- 7441
- Pixel size
- 15
- Maximum scale of use
- 10000
Abstract
- Dataset description abstract
-
Data provides bathymetric information based on Landsat 8 satellite at 15 m resolution.
Data were processed by the Modular and Inversion System (MIP) by EOMAP GmbH Co.KG. MIP is designed for the physically based assessment of hydro-biological parameters from multi- and hyperspectral remote sensing data.
Supplemental_Information:
EOMAPs Satellite Derived Bathymetry (SDB) method relies on the reflected light energy which is measured at the satellite sensor in space. In order to measure the water column thickness, the sea bottom reflection must be separated from all other simultaneously measured portions of light. Other contributors of light scattered to the sensor are atmospheric molecules and aerosols, adjacent scattering from land, the water surface reflection, and light scattered and absorbed due to particular properties of water constituents and the pure water itself. The pure water itself also absorbs light in a spectrally specific manner and therefore leaves unique signatures in the signal while the light passes through the water column and returns after reflection at the sea bottom. This property is relevant to estimate water depth from optical satellite imagery. As many properties can vary over space and time, effective correction, regularization and retrieval algorithms must be applied to avoid instable results. EOMAP developed and maintains these unique algorithm and its workflows for almost 2 decades. The maximum depth the system is able to sense is related to the complex interaction of radiance of bottom material, incident sun angle and intensity, and the type and quantity of organics or sediments in the water column. As a rule-of-thumb, satellite derived bathymetry should be capable of sensing bottom to depths equal to one to one point five times the Secchi depth.
no-data-value optically deep water: -9999
- Description of data processing
-
Data were processed by the Modular and Inversion System (MIP) by EOMAP GmbH Co.KG.
MIP is designed for the physically based assessment of hydro-biological parameters from multi- and hyperspectral remote sensing data.
Correction modules applied:
Corrected for Satellite sensor noise: Yes
Corrected for atmospheric effects: Yes
Corrected for the effect of adjacent land reflectance: Yes
Corrected for effects of turbidity: Yes
Corrected for water refraction effect: No
Ground-control points accessed to improve horizontal accuracy: No
Local in-situ data accessed for calibration and validation purposes: No
Description of in-situ data used: None
Corrected for tidal influence: Yes (using predicted tidal station(s))
Quality
Accuracy / Calibration
Hor. accuracy
- Measure description
-
Based on global ground control points. Evaluation done by US Government.
- Value
- 15m
- Evaluation method description
-
LE95
Vert. accuracy
- Measure description
-
General description of the vertical accuracies is given based on worldwide validation with acoustic and Lidar data and comparisons with nautical charts. For this area an on site validation was not possible because of the absence of modern surveyed data using acoustic or lidar technology.
- Evaluation method description
-
CE90
Suitability
- Suitability, Expected type of users / uses and limitations
-
Reconnaissance survey, hydrodynamic modelling, pre-planning, coastal zone management
Quality Indicators
- Horizontal Quality Indicator
- 3 - < 20 m
- Vertical Quality Indicator
- 1 - SBES low frequency, SDB (similar than 2+5%d)
- Purpose Quality Indicator
- 2 - Bathymetric/morphologic survey
Where
- Min. depth in meters (>0 below Sea Level)
- 1
- Max. depth in meters (>0 below Sea Level)
- -20
Projection
- code
-
WGS 84 (EPSG:4326)
- Version or custom projection details
-
8.6
- code
-
WGS 84 (EPSG:4326)
- Version or custom projection details
-
7.4
- Vertical Datum
-
-
Lowest Astronomical Tide
-
When
- Date (Creation)
- 2017-10-12
Temporal extent*
- Begin
- 2013-08-01
Who
Originator
Data Holding Center
Collating Centre = Metadata author
Access
Distributor
Data formats*
- Format
-
GeoTIFF
- Version
-
1.0
- Format
-
KML
- Format
-
XYZ Ascii
- Format
-
ESRI Shapefile
- Version
-
1.0
- Transfer size (in MB)
- 20
Intellectual property
- Use limitation
-
see EOMAP EULA: EOMAP_Product_EULA2014Oct19.pdf
- Access constraints
- by negotiation
- Use constraints
- Copyright