Chemical evidence of the changes of the Antarctic Bottom Water ventilation in the western Ross Sea between 1997 and 2003

Data from three Italian CLIMA project cruises between 1997 and 2003 were used to obtain sections of the hydrographic and chemical properties of the main water masses across the shelf break off Cape Adare (western Ross Sea, Antarctica). Dissolved oxygen, nitrate and phosphate data were combined on th...

Full description

Bibliographic Details
Published in:Deep Sea Research Part I: Oceanographic Research Papers
Main Authors: RIVARO P, MASSOLO S, BERGAMASCO A, CASTAGNO P, BUDILLON G
Other Authors: Rivaro, P, Massolo, S, Bergamasco, A, Castagno, P, Budillon, G
Format: Article in Journal/Newspaper
Language:English
Published: 2010
Subjects:
CO2
Online Access:http://hdl.handle.net/11367/27453
https://doi.org/10.1016/j.dsr.2010.03.005
id ftuninapoliparth:oai:ricerca.uniparthenope.it:11367/27453
record_format openpolar
spelling ftuninapoliparth:oai:ricerca.uniparthenope.it:11367/27453 2023-11-12T04:03:38+01:00 Chemical evidence of the changes of the Antarctic Bottom Water ventilation in the western Ross Sea between 1997 and 2003 RIVARO P MASSOLO S BERGAMASCO A CASTAGNO P BUDILLON G Rivaro, P Massolo, S Bergamasco, A Castagno, P Budillon, G 2010 http://hdl.handle.net/11367/27453 https://doi.org/10.1016/j.dsr.2010.03.005 eng eng volume:57 issue:5 firstpage:639 lastpage:652 numberofpages:14 journal:DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS http://hdl.handle.net/11367/27453 doi:10.1016/j.dsr.2010.03.005 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-77951173210 CO2 Ross Sea water masses info:eu-repo/semantics/article 2010 ftuninapoliparth https://doi.org/10.1016/j.dsr.2010.03.005 2023-10-17T21:03:19Z Data from three Italian CLIMA project cruises between 1997 and 2003 were used to obtain sections of the hydrographic and chemical properties of the main water masses across the shelf break off Cape Adare (western Ross Sea, Antarctica). Dissolved oxygen, nitrate and phosphate data were combined on the basis of the Redfield ratio to obtain the quasi-conservative tracers NO (9[NO3]+[O2]), PO (135[PO4]+[O2]) and phosphate star PO4 * (PO4 * = [PO4] + [O2]/175 – 1.95). In 1997 and 2003 the presence of the High Salinity Shelf Water at the bottom depth near the sill was traced by both physical and chemical measurements. In 2001 the Modified Shelf Water, characterized by warmer temperature and by a lower dissolved oxygen content than High Salinity Shelf Water, was observed at the shelf edge. The distribution of the chemical tracers together with the hydrographic observations showed recently formed Antarctic Bottom Water on the continental slope during all of the cruises. These observations were confirmed by the extended Optimum MultiParameter analysis. The calculated thickness of the new Antarctic Bottom Water, as well as the tracer content, were variable in time and in space. The estimated volume of the new Antarctic Bottom Water and the export of dissolved oxygen and nutrient associated with the overflowing water were different over the examined period. In particular, a lower (~ 55%) export was evidenced in 2001 compared to 1997. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ross Sea Università degli Studi di Napoli "Parthenope": CINECA IRIS Adare ENVELOPE(170.233,170.233,-71.283,-71.283) Antarctic Cape Adare ENVELOPE(175.000,175.000,-71.000,-71.000) Ross Sea The Antarctic Deep Sea Research Part I: Oceanographic Research Papers 57 5 639 652
institution Open Polar
collection Università degli Studi di Napoli "Parthenope": CINECA IRIS
op_collection_id ftuninapoliparth
language English
topic CO2
Ross Sea
water masses
spellingShingle CO2
Ross Sea
water masses
RIVARO P
MASSOLO S
BERGAMASCO A
CASTAGNO P
BUDILLON G
Chemical evidence of the changes of the Antarctic Bottom Water ventilation in the western Ross Sea between 1997 and 2003
topic_facet CO2
Ross Sea
water masses
description Data from three Italian CLIMA project cruises between 1997 and 2003 were used to obtain sections of the hydrographic and chemical properties of the main water masses across the shelf break off Cape Adare (western Ross Sea, Antarctica). Dissolved oxygen, nitrate and phosphate data were combined on the basis of the Redfield ratio to obtain the quasi-conservative tracers NO (9[NO3]+[O2]), PO (135[PO4]+[O2]) and phosphate star PO4 * (PO4 * = [PO4] + [O2]/175 – 1.95). In 1997 and 2003 the presence of the High Salinity Shelf Water at the bottom depth near the sill was traced by both physical and chemical measurements. In 2001 the Modified Shelf Water, characterized by warmer temperature and by a lower dissolved oxygen content than High Salinity Shelf Water, was observed at the shelf edge. The distribution of the chemical tracers together with the hydrographic observations showed recently formed Antarctic Bottom Water on the continental slope during all of the cruises. These observations were confirmed by the extended Optimum MultiParameter analysis. The calculated thickness of the new Antarctic Bottom Water, as well as the tracer content, were variable in time and in space. The estimated volume of the new Antarctic Bottom Water and the export of dissolved oxygen and nutrient associated with the overflowing water were different over the examined period. In particular, a lower (~ 55%) export was evidenced in 2001 compared to 1997.
author2 Rivaro, P
Massolo, S
Bergamasco, A
Castagno, P
Budillon, G
format Article in Journal/Newspaper
author RIVARO P
MASSOLO S
BERGAMASCO A
CASTAGNO P
BUDILLON G
author_facet RIVARO P
MASSOLO S
BERGAMASCO A
CASTAGNO P
BUDILLON G
author_sort RIVARO P
title Chemical evidence of the changes of the Antarctic Bottom Water ventilation in the western Ross Sea between 1997 and 2003
title_short Chemical evidence of the changes of the Antarctic Bottom Water ventilation in the western Ross Sea between 1997 and 2003
title_full Chemical evidence of the changes of the Antarctic Bottom Water ventilation in the western Ross Sea between 1997 and 2003
title_fullStr Chemical evidence of the changes of the Antarctic Bottom Water ventilation in the western Ross Sea between 1997 and 2003
title_full_unstemmed Chemical evidence of the changes of the Antarctic Bottom Water ventilation in the western Ross Sea between 1997 and 2003
title_sort chemical evidence of the changes of the antarctic bottom water ventilation in the western ross sea between 1997 and 2003
publishDate 2010
url http://hdl.handle.net/11367/27453
https://doi.org/10.1016/j.dsr.2010.03.005
long_lat ENVELOPE(170.233,170.233,-71.283,-71.283)
ENVELOPE(175.000,175.000,-71.000,-71.000)
geographic Adare
Antarctic
Cape Adare
Ross Sea
The Antarctic
geographic_facet Adare
Antarctic
Cape Adare
Ross Sea
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ross Sea
genre_facet Antarc*
Antarctic
Antarctica
Ross Sea
op_relation volume:57
issue:5
firstpage:639
lastpage:652
numberofpages:14
journal:DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
http://hdl.handle.net/11367/27453
doi:10.1016/j.dsr.2010.03.005
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-77951173210
op_doi https://doi.org/10.1016/j.dsr.2010.03.005
container_title Deep Sea Research Part I: Oceanographic Research Papers
container_volume 57
container_issue 5
container_start_page 639
op_container_end_page 652
_version_ 1782338204429451264