Structure of ocean circulation between the Galápagos Islands and Ecuador / (Registro nro. 13076)

Detalles MARC
000 -LEADER
fixed length control field 02341nab a22003137a 4500
003 - CONTROL NUMBER IDENTIFIER
control field EC-PaCDF
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20201006110803.0
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 170727t20132013xxu|||||||||||||||||eng||
040 ## - CATALOGING SOURCE
Original cataloging agency EC-PaCDF
Language of cataloging spa
Transcribing agency EC-PaCDF
041 ## - LANGUAGE CODE
Language code of text/sound track or separate title eng
082 04 - DEWEY DECIMAL CLASSIFICATION NUMBER
Edition number 23
Classification number 551.462
100 1# - MAIN ENTRY--PERSONAL NAME
Personal name Collins, C.
Relator term autor
245 10 - TITLE STATEMENT
Title Structure of ocean circulation between the Galápagos Islands and Ecuador /
Statement of responsibility, etc. C. Collins, A. Mascarenhas and R. Martinez.
260 3# - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Date of publication, distribution, etc. 2013.
300 ## - PHYSICAL DESCRIPTION
Extent : 3-12 p.
520 0# - SUMMARY, ETC.
Summary, etc. From 27 March to 5 April 2009, upper ocean velocities between the Galapagos Islands and Ecuador were measured using a vessel mounted ADCP. A region of posible strong cross-hemisphere exchange was observed immediately to the east of the Galapagos, where a shallow<br/>(200 m) 300 km wide northeastward surface flow transported 7–11 Sv. Underlying this strong northeastward surface current, a southward flowing undercurrent was observed which was at least 600 m thick, 100 km wide, and had an observed transport of 7–8 Sv. Next to the Ecuador coast, the shallow (<200 m) Ecuador Coastal Current was observed to extend offshore 100 km with strongest flow, 0.33 ms-1, near the surface. Immediately to the west of the Ecuador Coastal Current, flow was directed eastward and southward into the beginnings of the Peru-Chile Countercurrent. The integral of the surface currents between the Galapagos and Ecuador agreed well with observed sea level differences. Although the correlation of the sea level differences with<br/>large scale climate indices (Niño3 and the Southern Oscillation Index) was significant, more than half of the sea level variability was not explained. Seasonal variability of the sea level difference indicated that sea level was 2 cm higher at the Galapagos during late winter and early spring, which could be associated with the pattern of northward surface flows observed by R/V Knorr.<br/>
546 ## - LANGUAGE NOTE
Language note Inglés
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Structure
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Estructura
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Ocean circulation
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Circulación oceánica
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Galapagos Islands
653 ## - INDEX TERM--UNCONTROLLED
Uncontrolled term Islas Galápagos
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Mascarenhas, A.
Relator term autor
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Martinez, R.
Relator term autor
773 0# - HOST ITEM ENTRY
Related parts Vol. 33 (2013), p. 3-12
Title Advances in Geosciences.
856 ## - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier http://dx.doi.org/10.5194/adgeo-33-3-2013
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme Dewey Decimal Classification
Koha item type Artículo
Existencias
Withdrawn status Source of classification or shelving scheme Damaged status Not for loan Collection code Home library Current library Shelving location Date acquired Total Checkouts Full call number Barcode Date last seen Price effective from Koha item type
  Dewey Decimal Classification     Galápagos Corley Smith Library Corley Smith Library Artículos 27/07/2017   551.462 COL 2013 2020-0627 27/07/2017 27/07/2017 Artículo
  Dewey Decimal Classification     Galápagos Corley Smith Library Corley Smith Library Colección PDF 06/10/2020   551.462 COL 2013 2021-1314 06/10/2020 06/10/2020 Documento electrónico

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Digital