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IBCSO IBCSO - Discovering Antarctica’s present-day bathymetry

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IBCSO

Project website: www.ibcso.org contact: Jan.Erik.Arndt@awi.de

IBCSO - Discovering Antarctica’s present-day bathymetry

Jan Erik Arndt

1

, Fernando Bohoyo

2

, Boris Dorschel

1

, and the IBCSO Editorial Board

1) Alfred Wegener Institute, 2) Instituto Geológico y Minero de España

Figure 1: IBCSO Version 1.0 printable chart;

original size 1 x 1.2 m; scale 1 : 7,000,000

Figure 2: Comparison of (1) IBCSO Version 1.0 to (2) GEBCO_08 (from Arndt et al. 2013)

Figure 3: Different types of IBCSO Version 1.0; all types are available as NetCDF - GMT, sd - Fleder- maus, or GeoTIFF - ArcGIS file; the Source Identifier Grid (SID) shows the origin of the base data

The IBCSO project

The aim of the International Bathymetric Chart of the Southern Ocean (IBCSO) project is to create high resolu- tion bathymetric compilations for the Southern Ocean to support scientific activieties and investigations in Antarctic waters. Due to its huge size, the area’s remoteness and harsh ice conditions, the project is strongly relying on inter- national collaboration. IBCSO was inaugurated as a SCAR expert group in 2004. IBCSO is also a regional mapping project of the General Bathymetric Chart of the Ocean (GEBCO) under the joint auspices of the Intergovernmen- tal Oceanographic Commission (IOC) (of UNESCO) and the International Hydrographic Organization (IHO). In 2013, the first version of IBCSO was published in the Jour- nal Geophysical Research Letters (Arndt et al., 2013).

IBCSO Version 1.0

The first version of IBCSO is a prime example for an international collaboration in Antarctic Science. Over 30 institutions from 15 countries contributed data and shared their expertise to generate the, so far, largest database of bathy- metric data of the Southern Ocean. From this database, a digital bathymetric model (DBM) was produced with state of the art gridding algo- rithms. The DBM covers the entire Antarctic Treaty area south of 60° S with a resolution of 500 x 500 m. The DBM significantly improves our knowledge of the seafloor (Fig. 2). Three types of DBM are available in several formats and projections (Fig. 3). In addition, a new print- able chart of the Southern Ocean and Antarcti- ca has been created from this data (Fig. 1).

Both, the DBMs and the chart, can be down- loaded free of charge from the IBCSO website (www.ibcso.org).

Data Access: www.ibcso.org

Reference: Arndt et al. 2013 "The International Bathymetric Chart of the Southern Ocean (IBCSO) Version 1.0 - A new bathymetric compilation covering circum-Antarctic waters", Geophysical Research Letters, doi:

10.1002/grl.50413

Editorial Board:

Hans-Werner Schenke (Chair/Alfred Wegener Institute) Jan Erik Arndt (Editor/Alfred Wegener Institute)

Martin Jakobsson (Stockholm University)

Frank Nitsche (Lamont-Doherty Earth Observatory) Gwen Buys (British Antarctic Survey)

Bruce Goleby (Geoscience Australia)

Michele Rebesco (Istituto Nazionale di Oceanografia e di Geofisica Sperimentale) Fernando Bohoyo (Instituto Geológico y Minero de España)

Jon Kuk Hong (Korean Polar Research Institute)

Jenny Black (Institute of Geological and Nuclear Sciences) Rudolf Greku (Institute of Geological Sciences)

Gleb Udintsev (Vernadsky Institute of Geochemistry and Analytical Chemistry) Felipe Barrios (Servicio Hidrográfico y Oceanográfico)

Walter Reynoso-Peralta (Servicio de Hidrografía Naval) Taisei Morishita (Japan Coast Guard)

Rochelle Wigley (University of New Hampshire)

Contributing organisations:

IBCSO Version 1.0

The future of IBCSO ► Version 2.0

In IBCSO Version 1.0, about 83 % of the modelled grid cells are not directly constraint by measurements. In the aftermath of the production and release of Version 1.0, additional bathymetric data have been collected and more institutes offered to contribute their data. This data will im- prove an upcoming 2nd version, especially in the so far sparsely mapped waters offshore East Antarctica. In a working meeting of IBCSO Editorial Board members during the XXXIII SCAR meeting in Auckland, NZ, we fur- thermore agreed that a new version should have an in- creased extent to cover the area south of 50°S to include all ocean pathways of the Antarctic Circumpolar Current (ACC). This nearly doubles the modelled area. As the quality and reliability of the bathymetric compilation is highly depending on data contributions we would like to ask you:

If you have additional bathymetric data south of 50°S ↓ please contact us! ↓

General Bathym etric Ch

arGEBCOt of t h e Oc eans

SCRIPPSINSTIT UT I ON O F OCEAN OGRA

PHY

U C S D

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