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Full text: The European harmonised bathymetry grid EMODnet Bathymetry

Neb Map Service 
era: 
sün 
=ig. 6: German research chmın 
orocessed bathymetry in the Black See 
v(MARUM ancı e. ( 
Jr 
1b, 
nNerge all data sets covering this area provided by 
“he data providers. 
The German marine geoscience research com- 
Munity acquired numerous hydroacoustic data 
within the European seas. Raw data sets are be 
ng archived by the BSH (www.bsh.de/EN/DATA, 
Iceanographic_Data_Center/Surveying_data/ 
surveying_data_node.html). Within the EMOD 
1et Bathymetry project the University of Bremen 
and MARUM have processed (full hydrographic 
oarocessing including tidal, sound velocity cor 
‚ection, manual soundings editing and draft cor- 
‚ections), prepared metadata and sampled some 
af these data sets. More specifically, benefiting 
‘rom two decades of strong interest in the Black 
ea region, MARUM has shared their processed 
oathymetric data for the area (14 out of 16 survey 
zruises, see Fig. 6). Moreover, German bathymetric 
zontribution has generated a number of scien- 
tific peer-reviewed papers such as Gutscher et al. 
2017) in the lonian Sea (Fig..Z) Loher et al. (2018) 
or the Calabrian Arc or the Gibraltar/Alboran Sea 
Wienbera et al. 2013). The German research com 
000 
‚500 
2a. ; : High-resolution bathvmetry contribution af the German research commMmUNÄIN 
N the lonian Sea 
munity has also been largely contributing to the 
Arctic area as part of a tight collaboration between 
EMODnet Bathymetry and the IBCAO community 
(Jakobsson et al. 2020). 
Contribution to global bathymetric 
grids and regional programmes 
As outlined above, since early years of the EMOD 
net Bathymetry programme, collaboration has 
aeen key factor for its development and success. 
Beyond the strong internal collaboration between 
contributors of the EMODnet consortium, as de- 
scribed earlier, EMODnet Bathymetry has also 
elaborated strong relations with several interna- 
tional actors. 
The EMODnet DTM along with the description 
of the source bathymetric data enable contribut- 
ng partners to fulfil their obligations against the 
NSPIRE Directive. Moreover, because the EMOD- 
ı1et DTM extends over national borders and that 
netadata are uniformly describing the data sourc 
es in a unique portal, user groups of similar inter- 
est have been selecting the EMODnet products as 
their main source of information. For example, both 
the North Sea Hydrographic Commission and the 
3altic Sea Hydrographic Commission are using the 
aathymetric information originating from EMOD- 
1et as part of their Marine Spatial Data Infrastruc 
‚ure, This is also the case for the Baltic Environmen 
)rotection Commission (Jakobsson et al. 2019). 
zMODnet Bathymetry also shares mutual com 
olementary benefits with the International Hy- 
drographic Organization (IHO) as a number of 
:MODnet contributors are themselves Hydro- 
graphic Offices and as the IHO sees the EMODnet 
3Zathymetry products (DTM and data Inventory) 
as an authoritative best estimate, trans-nationa! 
digital bathymetric grid vital to the development 
of economic, scientihc and environmental activi- 
ties. This collaboration is embodied as part of the 
Memorandum of Understanding signed betweer 
the IHO and the European Commission in 2012. It is 
naterialised through the full integration of the CDI/ 
CPRD metadata inventory services in the IHO DCDB 
(Data Centre for Digital Bathymetry) viewer (https:/ 
Naps.ngdc.noaa.gov/viewers/iho_dcdb) through 
OGC services, giving the possibility for any user to 
‚etrieve metadata information from European data 
1olders and to be redirected to the EMODnet Ba- 
thymetry portal for further exploration. 
Additionally, GEBCO and EMODnet communities 
Nutually integrate their bathymetric grids (respec 
üvely at 115 and approximately 500 m horizonta 
esolution). Fig. 8 shows the geographical distri- 
aution of measured data sources composing the 
'ecent 2019 GEBCO release. Note that darker areas 
ndicate regions without direct measurement. In 
these areas, the bathymetry is predicted from sat 
ellite altimetry (Smith and Sandwell 1994). One can 
see in Fig. 8 that the European seas have largely 
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