Date (Creation)

2015-01-11T00:00:00

Temporal resolution

P0Y0M1DT0H0M0S

Topic category

• Oceans

Maintenance and update frequency

Not planned

Global Change Master Directory (GCMD) Earth Science Keywords Version 8.0

• EARTH SCIENCE | OCEANS | OCEAN TEMPERATURE
• EARTH SCIENCE | OCEANS | OCEAN TEMPERATURE | SEA SURFACE TEMPERATURE
• EARTH SCIENCE | CLIMATE INDICATORS | ATMOSPHERIC/OCEAN INDICATORS | SURFACE SALINITY
• EARTH SCIENCE | OCEANS | OCEAN CIRCULATION | OCEAN CURRENTS
• EARTH SCIENCE | OCEANS | SALINITY/DENSITY | DENSITY
• EARTH SCIENCE | OCEANS | SALINITY/DENSITY | SALINITY
• EARTH SCIENCE SERVICES | MODELS | OCEAN GENERAL CIRCULATION MODELS (OGCM)/REGIONAL OCEAN MODELS
• EARTH SCIENCE | OCEANS | COASTAL PROCESSES
• EARTH SCIENCE | OCEANS | COASTAL PROCESSES | SEA SURFACE HEIGHT

Australian and New Zealand Standard Research Classification (ANZSRC): Fields of Research

• Physical Oceanography
• Climatology (excl. Climate Change Processes)

Keywords (Theme)

• Z coordinate at grid layer faces
• Latitude at cell centre
• Longitude at cell centre
• Time
• Surface Elevation
• Eastward component of current
• Northward component of current
• K component of current at cell centre and Z grid
• Eastward component of bottom current deviation
• Northward component of bottom current deviation
• Temperature

AODN Discovery Parameter Vocabulary

• Density of the water body
• Practical salinity of the water body

Language

English

Character encoding

UTF8

Supplemental Information

Oliver, E.C.J, M. Herzfeld and N.J. Holbrook, Modelling the shelf circulation off eastern Tasmania, submitted to Continental Shelf Research

Content type

Physical measurement

Name

Z coordinate at grid layer faces

Name

z_centre

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/ULAA

Name

Metres

Name

Latitude at cell centre

Name

y_centre

Name

degrees_north

Name

Longitude at cell centre

Name

x_centre

Name

degrees_east

Name

Time

Name

t

Name

days since 1990-01-01 00:00:00

Name

Surface Elevation

Name

eta

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/ULAA

Name

Metres

Name

Eastward component of current

Name

u

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/UVAA

Name

Metres per second

Name

Northward component of current

Name

v

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/UVAA

Name

Metres per second

Name

K component of current at cell centre and Z grid

Name

w

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/UVAA

Name

Metres per second

Name

dens

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/UKMC

Name

Kilograms per cubic metre

Name

Eastward component of bottom current deviation

Name

ubot

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/UVAA

Name

Metres per second

Name

Northward component of bottom current deviation

Name

vbot

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/UVAA

Name

Metres per second

Name

salt

Identifier

http://vocab.aodn.org.au/def/unitsofmeasure/entity/481

Name

Practical Salinity Unit

Name

Temperature

Name

temp

Identifier

http://vocab.nerc.ac.uk/collection/P06/current/UPAA

Name

Degrees Celsius

Distribution format

• NetCDF

OnLine resource

ETAS paper (.pdf) [direct download]

OnLine resource

ETAS paper supplement (.pdf) [direct download]

OnLine resource

THREDDS catalogue of data files

Statement

The Sparse Hydrodynamic Ocean Code (SHOC) developed at the CSIRO Marine Laboratories in Hobart (Australia) was used to dynamically simulate variability of the near-shore and continental shelf waters off eastern Tasmania for 1993-2014. SHOC is based on the nonlinear three-dimensional equations for momentum conservation, continuity, and the conservation of heat and salt. The model domain consists of the continental shelf and slope off eastern Tasmania. The domain was defined by a curvilinear horizontal grid with three open boundaries and the fourth side bounded by the Tasmanian coast. The seaward boundary ran parallel to the continental shelf break roughly following the 2500 m isobath. The two cross-shelf boundaries ran perpendicular to the shelf break and met the coast at South Cape in the south and just north of Eddystone Point in the north. The grid included two narrow spurs for the Derwent River and Huon River estuaries. River runoff was included by specifying the flow rate and temperature of freshwater input (zero salinity) every six hours at source points. The model boundary forcing consisted of daily fields of three-dimensional velocities, sea level, temperature and salinity from the 1/10-degree Bluelink ReANalysis (BRAN, version 3, 1/1/1993-31/7/2012) and OceanMAPS analysis (versions 2.0--2.2.1, 1/8/2012-31/12/2014). The model surface boundary forcing consisted of 6-hourly atmospheric fields provided by the National Centers for Environmental Prediction (NCEP) Climate Forecast System Reanalysis (CFSR, 1993-2010) and Climate Forecast System Version 2 analysis (CSFv2, 2011-2014). Daily fields of sea surface height and three-dimensional fields of velocity, temperature, and salinity, were output every day. Hourly time series were output at specific points of interest.

Hierarchy level

Dataset

Resource scope

Dataset

Title

ISO 19115-3:2018