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Circulation and fronts in continental shelf seas - Slope turbulence, internal waves and phytoplankto...

Circulation and fronts in continental shelf seas - Slope turbulence, internal waves and phytoplankto...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_istex_primary_ark_67375_V84_63GZPGQK_3

Circulation and fronts in continental shelf seas - Slope turbulence, internal waves and phytoplankton growth at the Celtic Sea shelf-break

About this item

Full title

Circulation and fronts in continental shelf seas - Slope turbulence, internal waves and phytoplankton growth at the Celtic Sea shelf-break

Publisher

London: The Royal Society

Journal title

Philosophical transactions of the Royal Society of London. Series A: Mathematical and physical sciences, 1981-09, Vol.302 (1472), p.663-682

Language

English

Formats

Publication information

Publisher

London: The Royal Society

More information

Scope and Contents

Contents

The edge of the Celtic Sea shelf is characterized during the summer by a band of cold water (ca. 100 km broad), which is generally conspicuous in high resolution infrared images from satellites, particularly under high pressure atmospheric conditions with clear skies. Preliminary studies of mixing in this region were made in 1972, 1973 and 1974 and...

Alternative Titles

Full title

Circulation and fronts in continental shelf seas - Slope turbulence, internal waves and phytoplankton growth at the Celtic Sea shelf-break

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_istex_primary_ark_67375_V84_63GZPGQK_3

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_istex_primary_ark_67375_V84_63GZPGQK_3

Other Identifiers

ISSN

0080-4614

E-ISSN

2054-0272

DOI

10.1098/rsta.1981.0191

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