Diurnal Warming Observations with ASIP in the subtropical Northern Atlantic

European Geosciences Union General Assembly 2015 (EGU2015), 12-17 April 2015, Vienna, Austria.-- 1 page Quantification of air-sea exchange fluxes of energy, moisture, momentum and gases require in situ-measurements of the near-surface layer of the ocean. In the framework of the Salinity Processes in...

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Main Authors: ten Doeschate, A., Ward, Brian, Sutherland, G., Font, Jordi, Reverdin, Gilles
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Language:unknown
Published: European Geosciences Union 2015
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Online Access:http://hdl.handle.net/10261/140955
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spelling ftcsic:oai:digital.csic.es:10261/140955 2024-02-11T10:06:35+01:00 Diurnal Warming Observations with ASIP in the subtropical Northern Atlantic ten Doeschate, A. Ward, Brian Sutherland, G. Font, Jordi Reverdin, Gilles 2015-04-16 http://hdl.handle.net/10261/140955 unknown European Geosciences Union Publisher's version http://meetingorganizer.copernicus.org/EGU2015/posters/17339 Sí issn: 1607-7962 Geophysical Research Abstracts 17: EGU2015-7098 (2015) http://hdl.handle.net/10261/140955 open póster de congreso http://purl.org/coar/resource_type/c_6670 2015 ftcsic 2024-01-16T10:19:04Z European Geosciences Union General Assembly 2015 (EGU2015), 12-17 April 2015, Vienna, Austria.-- 1 page Quantification of air-sea exchange fluxes of energy, moisture, momentum and gases require in situ-measurements of the near-surface layer of the ocean. In the framework of the Salinity Processes in the Upper Ocean Regional Study (SPURS) project, we participated in two cruises to the North Atlantic Salinity Maximum (NASM) region. Observations in the upper ocean are obtained with the Air Sea Interaction Profiler (ASIP), which is an upwardly-rising microstructure instrument designed to study processes in the mixing layer of the ocean. ASIP operates autonomously for up to two days, obtaining undisturbed profiles within the water column from depth to the immediate surface. During the SPURS experiment, ASIP was deployed on several occasions, resulting in a total of over 1000 profiles of the ocean surface boundary layer. ASIP is equipped with microstructure sensors for temperature (FP07), conductivity (SBE07), shear, accurate C-T sensors, a PAR and an oxygen sensor. The high resolution temperature profiles obtained, combined with information on local meteorological variables, allow for an accurate study of the temporal and vertical variability of diurnal warming of the upper ocean boundary layer. Characteristics of the measured diurnal warming at the ocean surface and at specific depth levels are compared to physics-based models of near-surface warming. Mixing rates in the upper ocean are determined from the turbulent dissipation rate, calculated from profiles of the turbulent shear. This information is used to quantify variability between the modeled and observed diurnal warming signal Peer Reviewed Still Image North Atlantic Digital.CSIC (Spanish National Research Council)
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language unknown
description European Geosciences Union General Assembly 2015 (EGU2015), 12-17 April 2015, Vienna, Austria.-- 1 page Quantification of air-sea exchange fluxes of energy, moisture, momentum and gases require in situ-measurements of the near-surface layer of the ocean. In the framework of the Salinity Processes in the Upper Ocean Regional Study (SPURS) project, we participated in two cruises to the North Atlantic Salinity Maximum (NASM) region. Observations in the upper ocean are obtained with the Air Sea Interaction Profiler (ASIP), which is an upwardly-rising microstructure instrument designed to study processes in the mixing layer of the ocean. ASIP operates autonomously for up to two days, obtaining undisturbed profiles within the water column from depth to the immediate surface. During the SPURS experiment, ASIP was deployed on several occasions, resulting in a total of over 1000 profiles of the ocean surface boundary layer. ASIP is equipped with microstructure sensors for temperature (FP07), conductivity (SBE07), shear, accurate C-T sensors, a PAR and an oxygen sensor. The high resolution temperature profiles obtained, combined with information on local meteorological variables, allow for an accurate study of the temporal and vertical variability of diurnal warming of the upper ocean boundary layer. Characteristics of the measured diurnal warming at the ocean surface and at specific depth levels are compared to physics-based models of near-surface warming. Mixing rates in the upper ocean are determined from the turbulent dissipation rate, calculated from profiles of the turbulent shear. This information is used to quantify variability between the modeled and observed diurnal warming signal Peer Reviewed
format Still Image
author ten Doeschate, A.
Ward, Brian
Sutherland, G.
Font, Jordi
Reverdin, Gilles
spellingShingle ten Doeschate, A.
Ward, Brian
Sutherland, G.
Font, Jordi
Reverdin, Gilles
Diurnal Warming Observations with ASIP in the subtropical Northern Atlantic
author_facet ten Doeschate, A.
Ward, Brian
Sutherland, G.
Font, Jordi
Reverdin, Gilles
author_sort ten Doeschate, A.
title Diurnal Warming Observations with ASIP in the subtropical Northern Atlantic
title_short Diurnal Warming Observations with ASIP in the subtropical Northern Atlantic
title_full Diurnal Warming Observations with ASIP in the subtropical Northern Atlantic
title_fullStr Diurnal Warming Observations with ASIP in the subtropical Northern Atlantic
title_full_unstemmed Diurnal Warming Observations with ASIP in the subtropical Northern Atlantic
title_sort diurnal warming observations with asip in the subtropical northern atlantic
publisher European Geosciences Union
publishDate 2015
url http://hdl.handle.net/10261/140955
genre North Atlantic
genre_facet North Atlantic
op_relation Publisher's version
http://meetingorganizer.copernicus.org/EGU2015/posters/17339

issn: 1607-7962
Geophysical Research Abstracts 17: EGU2015-7098 (2015)
http://hdl.handle.net/10261/140955
op_rights open
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