Influence of Salinity and Temperature Gradients on the Variability of the North Brazil Undercurrent
The North Brazil Undercurrent (NBUC) is a narrow (<1°) northward western boundary current in the tropical South Atlantic Ocean. It carries a large volume of water (>16 Sv) and plays an important role in the Atlantic Meridional Overturning Circulation and the South Atlantic Subtropical...
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doaj-1635d9ccf6144c9f99b90626a0307fff2021-09-20T04:45:55ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452021-09-01810.3389/fmars.2021.744833744833Influence of Salinity and Temperature Gradients on the Variability of the North Brazil UndercurrentHao Liu0Hao Liu1Hao Liu2Zexun Wei3Zexun Wei4Zexun Wei5Ingo Richter6Xunwei Nie7Xunwei Nie8Xunwei Nie9Chuanshun Li10First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modelling, Pilot National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modelling, Qingdao, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modelling, Pilot National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modelling, Qingdao, ChinaApplication Laboratory, Research Institute for Value-Added-Information Generation, Japan Agency for Marine-Earth Science and Technology, Yokohama, JapanFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modelling, Pilot National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modelling, Qingdao, ChinaFirst Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaThe North Brazil Undercurrent (NBUC) is a narrow (<1°) northward western boundary current in the tropical South Atlantic Ocean. It carries a large volume of water (>16 Sv) and plays an important role in the Atlantic Meridional Overturning Circulation and the South Atlantic Subtropical Cell. Strong salinity and temperature fronts occur over the NBUC region. The role of temperature and salinity gradients on the genesis of NBUC variability has never been explored. This study uses three high-resolution (≤0.1°) and one low-resolution (=0.25°) model outputs to explore the linear trend of NBUC transport and its variability on annual and interannual time scales. We find that the linear trend and interannual variability of the geostrophic NBUC transport show large discrepancies among the datasets. Thus, the linear trend and variability of the geostrophic NBUC are associated with model configuration. We also find that the relative contributions of salinity and temperature gradients to the geostrophic shear of the NBUC are not model dependent. Salinity-based and temperature-based geostrophic NBUC transports tend to be opposite-signed on all time scales. Despite the limited salinity and temperature profiles, the model results are consistent with the in-situ observations on the annual cycle and interannual time scales. This study shows the relationship of salinity-based and temperature-based geostrophic NBUC variations in the annual and interannual variability and trend among different models and highlights the equal important roles of temperature and salinity in driving the variability of NBUC transport.https://www.frontiersin.org/articles/10.3389/fmars.2021.744833/fullNorth Brazil Undercurrentsalinity-based geostrophic velocitytemperature-based geostrophic velocitytemporal variabilityHYCOMOFES2 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Hao Liu Hao Liu Hao Liu Zexun Wei Zexun Wei Zexun Wei Ingo Richter Xunwei Nie Xunwei Nie Xunwei Nie Chuanshun Li |
spellingShingle |
Hao Liu Hao Liu Hao Liu Zexun Wei Zexun Wei Zexun Wei Ingo Richter Xunwei Nie Xunwei Nie Xunwei Nie Chuanshun Li Influence of Salinity and Temperature Gradients on the Variability of the North Brazil Undercurrent Frontiers in Marine Science North Brazil Undercurrent salinity-based geostrophic velocity temperature-based geostrophic velocity temporal variability HYCOM OFES2 |
author_facet |
Hao Liu Hao Liu Hao Liu Zexun Wei Zexun Wei Zexun Wei Ingo Richter Xunwei Nie Xunwei Nie Xunwei Nie Chuanshun Li |
author_sort |
Hao Liu |
title |
Influence of Salinity and Temperature Gradients on the Variability of the North Brazil Undercurrent |
title_short |
Influence of Salinity and Temperature Gradients on the Variability of the North Brazil Undercurrent |
title_full |
Influence of Salinity and Temperature Gradients on the Variability of the North Brazil Undercurrent |
title_fullStr |
Influence of Salinity and Temperature Gradients on the Variability of the North Brazil Undercurrent |
title_full_unstemmed |
Influence of Salinity and Temperature Gradients on the Variability of the North Brazil Undercurrent |
title_sort |
influence of salinity and temperature gradients on the variability of the north brazil undercurrent |
publisher |
Frontiers Media S.A. |
series |
Frontiers in Marine Science |
issn |
2296-7745 |
publishDate |
2021-09-01 |
description |
The North Brazil Undercurrent (NBUC) is a narrow (<1°) northward western boundary current in the tropical South Atlantic Ocean. It carries a large volume of water (>16 Sv) and plays an important role in the Atlantic Meridional Overturning Circulation and the South Atlantic Subtropical Cell. Strong salinity and temperature fronts occur over the NBUC region. The role of temperature and salinity gradients on the genesis of NBUC variability has never been explored. This study uses three high-resolution (≤0.1°) and one low-resolution (=0.25°) model outputs to explore the linear trend of NBUC transport and its variability on annual and interannual time scales. We find that the linear trend and interannual variability of the geostrophic NBUC transport show large discrepancies among the datasets. Thus, the linear trend and variability of the geostrophic NBUC are associated with model configuration. We also find that the relative contributions of salinity and temperature gradients to the geostrophic shear of the NBUC are not model dependent. Salinity-based and temperature-based geostrophic NBUC transports tend to be opposite-signed on all time scales. Despite the limited salinity and temperature profiles, the model results are consistent with the in-situ observations on the annual cycle and interannual time scales. This study shows the relationship of salinity-based and temperature-based geostrophic NBUC variations in the annual and interannual variability and trend among different models and highlights the equal important roles of temperature and salinity in driving the variability of NBUC transport. |
topic |
North Brazil Undercurrent salinity-based geostrophic velocity temperature-based geostrophic velocity temporal variability HYCOM OFES2 |
url |
https://www.frontiersin.org/articles/10.3389/fmars.2021.744833/full |
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