THE USE OF SATELLITE DERIVED UPPER OCEAN HEAT CONTENT TO THE STUDY OF CLIMATE VARIABILITY IN THE SOUTH ATLANTIC

The lack of continuous long-term hydrographic observations, especially in the South Atlantic Ocean, makes satellite-derived data a key tool to investigate time and spatial variability on a basin scale. Altimeter data, which is not affected by cloud coverage as infrared-derived data, provides extreme...

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Main Authors: Edmo J. D. Campos, Carlos A. D. Lentini, Wilton Z. Arruda
Format: Article
Language:English
Published: Universidade Federal de Uberlândia 2005-08-01
Series:Revista Brasileira de Cartografia
Subjects:
Online Access:http://www.rbc.ufrj.br/_pdf_57_2005/57_2_04.pdf
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author Edmo J. D. Campos
Carlos A. D. Lentini
Wilton Z. Arruda
author_facet Edmo J. D. Campos
Carlos A. D. Lentini
Wilton Z. Arruda
author_sort Edmo J. D. Campos
collection DOAJ
description The lack of continuous long-term hydrographic observations, especially in the South Atlantic Ocean, makes satellite-derived data a key tool to investigate time and spatial variability on a basin scale. Altimeter data, which is not affected by cloud coverage as infrared-derived data, provides extremely useful information on the vertical thermal and dynamical structure of the upper ocean when combined with climatological hydrographic data through a diagnostic model. We present a semi-dynamic model that combines sea surface height anomalies from TOPEX/POSEIDON, infrared satellite-derived sea surface temperature from NOAA/AVHRR, and World Ocean Atlas 2001 hydrographic data to generate maps of the Upper Ocean Heat Content Anomaly which are suitable for climate variability studies.
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spelling doaj.art-8a46c22ca21245fba49afb116e29acdb2022-12-21T18:18:38ZengUniversidade Federal de UberlândiaRevista Brasileira de Cartografia0560-46131808-09362005-08-015728792THE USE OF SATELLITE DERIVED UPPER OCEAN HEAT CONTENT TO THE STUDY OF CLIMATE VARIABILITY IN THE SOUTH ATLANTICEdmo J. D. CamposCarlos A. D. LentiniWilton Z. ArrudaThe lack of continuous long-term hydrographic observations, especially in the South Atlantic Ocean, makes satellite-derived data a key tool to investigate time and spatial variability on a basin scale. Altimeter data, which is not affected by cloud coverage as infrared-derived data, provides extremely useful information on the vertical thermal and dynamical structure of the upper ocean when combined with climatological hydrographic data through a diagnostic model. We present a semi-dynamic model that combines sea surface height anomalies from TOPEX/POSEIDON, infrared satellite-derived sea surface temperature from NOAA/AVHRR, and World Ocean Atlas 2001 hydrographic data to generate maps of the Upper Ocean Heat Content Anomaly which are suitable for climate variability studies.http://www.rbc.ufrj.br/_pdf_57_2005/57_2_04.pdfAltimeter dataSHASouth Atlantic Thermocline Watersupper layer thicknesstwo-layer model.
spellingShingle Edmo J. D. Campos
Carlos A. D. Lentini
Wilton Z. Arruda
THE USE OF SATELLITE DERIVED UPPER OCEAN HEAT CONTENT TO THE STUDY OF CLIMATE VARIABILITY IN THE SOUTH ATLANTIC
Revista Brasileira de Cartografia
Altimeter data
SHA
South Atlantic Thermocline Waters
upper layer thickness
two-layer model.
title THE USE OF SATELLITE DERIVED UPPER OCEAN HEAT CONTENT TO THE STUDY OF CLIMATE VARIABILITY IN THE SOUTH ATLANTIC
title_full THE USE OF SATELLITE DERIVED UPPER OCEAN HEAT CONTENT TO THE STUDY OF CLIMATE VARIABILITY IN THE SOUTH ATLANTIC
title_fullStr THE USE OF SATELLITE DERIVED UPPER OCEAN HEAT CONTENT TO THE STUDY OF CLIMATE VARIABILITY IN THE SOUTH ATLANTIC
title_full_unstemmed THE USE OF SATELLITE DERIVED UPPER OCEAN HEAT CONTENT TO THE STUDY OF CLIMATE VARIABILITY IN THE SOUTH ATLANTIC
title_short THE USE OF SATELLITE DERIVED UPPER OCEAN HEAT CONTENT TO THE STUDY OF CLIMATE VARIABILITY IN THE SOUTH ATLANTIC
title_sort use of satellite derived upper ocean heat content to the study of climate variability in the south atlantic
topic Altimeter data
SHA
South Atlantic Thermocline Waters
upper layer thickness
two-layer model.
url http://www.rbc.ufrj.br/_pdf_57_2005/57_2_04.pdf
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